location	catalog #	site #	core/section/secondary location	latitude (decimal degrees)	longitude (decimal degrees)	depositional setting	physiographic setting	inundation distance (m)	inundation reference point	elevation(mamsl)	 barrier elevation (mamsl)	obsevational method/ sampling method	# cores/sampling localities	# events documented (tsunami + subsidence)	# tsunami events documented at site	subsidence present? (y/n or comment)	# subsidence events documented at site	# tsunami deposits at site associated with subsidence	# tsunami deposits at site not associated with subsidence	event #	tsunami event #	subsidence event #	amount of subsidence (m)	age (rcybp)	age range (cybp)	correlated date (in years A.D. unless otherwise noted)	age method/comments	thickness (cm)	maximum thickness (cm)	geometry	# layers 	layer thickness (cm)	layer characteristics	underlying material	overlying material	lower contact	upper contact	grain size range(phi)	grain size distribution	grain size description	horizontal textural gradient	grading	sorting	other sedimentary structures or properties	composition	inclusions	flow direction	microfossils	chemical evidence	comments/additional descriptions	reference	reference type	reference date	"map (USGS 7.5 minute quadrangle for U. S., NTS 1:50,000 for Canada)"
"Koprino Harbour, Vancouver Island, B.C."	1	1		50.5089	-127.8462	"marsh, tidal"	"Northern side of sound, 15 km from open ocean."					"Pits, gouge cores, outcrops"	Data points 5 m apart on gridded transects	2	2					1	1					1964	Correlation with Fair Harbor deposits	0.5		"Continuous only near axcial tidal channel, thins landward and away from tidal channels, pinches out near forest edge, only locally reachs it, rises 0.4 m from tidal channel to forest. "	May be locally stratified (2-3 sand/mud cuplets).		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		3.0 - 2.0		"Fine sand, moderately sorted silt"	Fines landward and away from tidal channels	Massive to normal			"Q,F,L"	"Sticks, cones, bark, shell fragments, forams, diatoms"		Marine microfossils		"Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago, based on Fair Harbor site)"	"Benson et al., 1997"	Journal	1997	"92 L/12,  92 L/5"
"Koprino Harbour, Vancouver Island, B.C."	2	1		50.5089	-127.8462	"marsh, tidal"	"Northern side of sound, 15 km from open ocean."					"Pits, gouge cores, outcrops"	Data points 5 m apart along 330 m transect and along seven shorter transects perpendicular to axial transect 	2	2					2	2			161±16	1670-1950	1700	"Radiocarbon from growth position triglochin in sand layer, correlation with Japanese historical records"	0.1-1.0	12.00	"Thins landward and away from tidal channels, discontinuous 15 m beyond axial tidal channel, rises10 cm toward forest. Possibly correlative discontinuous lenses up to 12 cm thick near forest edge."	May be locally stratified (2-3 sand/mud cuplets).		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		3.0 - -1.0		"Fine to very coarse sand, moderately sorted silt, some gravel present near tidal chanels."	Fines landward and away from tidal channels	Massive to normal			"Q,F,L"	"Sticks, cones, bark, shell fragments, forams, diatoms"		Marine microfossils		"Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago, based on Fair Harbor site)"	"Benson et al., 1997"	Journal	1997	"92 L/12,  92 L/5"
"Neroutsos Inlet, Vancouver Island, B.C."	3	2		50.4000	-127.5200	"marsh, tidal"	"Head of inlet, protected from open ocean by 50 km of narrow waterways and islands."			 		"Pits, gouge cores, outcrops"	Data points 5 m apart on 30x30m gridded transect	2	2					1	1					1964	Correlation with Fair Harbor deposits	0.5-2.0		"Thins landward and away from tidal channels, pinches out near forest edge, discontinuous near back of marsh to SE."	May be locally stratified (2-3 sand/mud cuplets).		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		 4.0 - 0.0		"Very fine to coarse sand, moderately sorted silt"	Fines landward and away from tidal channels	Massive			"Q,F,L"	"Sticks, cones, bark, shell fragments, forams, diatoms"		Marine microfossils		"Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago, based on Fair Harbor site)"	"Benson et al., 1997"	Journal	1997	"92 L/5, 92 L6"
"Neroutsos Inlet, Vancouver Island, B.C."	4	2		50.4000	-127.5200	"Marsh, tidal"	"head of inlet, protected from open ocean by 50 km of narrow waterways and islands"					"Pits, gouge cores, outcrops"	Data points 5 m apart on 30x30m gridded transect	2	2					2	2			230±50	1444-1950	1700	"Radiocarbon from bark fragment on sand layer, correlation with japanese historical record"	1.0-2.0		"Thins landward and away from tidal channels, pinches out near forest edge, discontinuous near back of marsh to SE."	May be locally stratified (2-3 sand/mud cuplets).		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		2.0 - -1.0		"Medium to very coarse sand, moderately sorted silt"	Fines landward and away from tidal channels	assive to normal			"Q,F,L"	"Growth position leaf bases of Triglochin maritimum, sticks, cones bark shell fragments, forams, diatoms"		Marine microfossils		"Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago, based on Fair Harbor site)"	"Benson et al., 1997"	Journal	1997	"92 L/5, 92 L6"
"Power Lake, Vancouver Island, B.C."	5	3		50.1925	-127.4617	Lake								2	2					1	1					1964																								Listed in table of marshes containing tsunami deposits	"Clague et al., 2000"	Journal	2000	92 L/3
"Power Lake, Vancouver Island, B.C."	6	3		50.1925	-127.4617	Lake								2	2					2	2					1700																								Listed in table of marshes containing tsunami deposits	"Clague et al., 2000"	Journal	2000	92 L/3
"Fair Harbour, Vancouver Island, B.C."	7	4		50.0700	-127.1500	"Marsh, tidal"	Head of inlet. Open ocean is 20 km away.					"Pits, gouge cores, outcrops"	"215 borings, data points 5 m apart on gridded transects"	2	2					1	1					1964	137Cs spike	0.5-1.0	2.00	"Thins landward and away from tidal channels, pinches out near forest edge."	3 (locally up to 3 couplets of clean coarse to fine sand overlain by muddy fine sand and siltÉ)		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		 3.0 - 1.0		"Fine to medium sand, moderately sorted silt"	Fines landward and away from tidal channels	Massive			"Q,F,L"	"Sticks, cones, bark, shell fragments, forams, diatoms, leaf bases of marsh plant Triglochin maritimum"		Marine microfossils		Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago)	"Benson et al., 1997"	Journal	1997	92 L/3
"Fair Harbour, Vancouver Island, B.C."	8	4		50.0700	-127.1500	"Marsh, tidal"	Head of inlet. Open ocean is 20 km away.					"Pits, gouge cores, outcrops"	"215 borings, data points 5 m apart on gridded transects"	2	2					2	2			270±80	1444-1950	1700	"Radiocarbon from stick 2-3 cm below sand layer, correlation with japanese historical record"	1.5-2.5	10.00	"Thins landward and away from tidal channels, pinches out near forest edge, rises topograsphically 1.4 m from open marsh to forest edge."	3 (locally up to 3 couplets of clean coarse to fine sand overlain by muddy fine sand and siltÉ)		"Normally graded, sharply based,fine to coarse sand abruptly overlain by sandy mud."	Peat	Peat	Mantled		3.0 - -1.0		"Fine to very coarse sand, moderately sorted silt, some gravel present near tidal chanels."	Fines landward and away from tidal channels	Massive or normal			"Q,F,L"	"Sticks, conifer cones, bark, leaf bases of marsh plants"		Marine diatoms (navicula marina)		Presence of only two tsunami deposits due to youthfulness of marshes (< 550 cal. yr. ago)	"Benson et al., 1997"	Journal	1997	92 L/3
"Zeballos, Vancouver Island, B.C."	9	5		49.9800	-126.8500	marsh	Marsh along coastal inlet																																												"Clague et al., 2000"	Journal	2000	92 E/15
"Zeballos, Vancouver Island, B.C."	10	5		49.9800	-126.8500	Marsh	Marsh along coastal inlet							1	1	y	1			1	1	1			<500	1700	Radiocarbon			Single widespread sand sheet.				Peaty soil		Sharp	Sharp			Sand and silty sand			Moderately sorted			Abundant wood and other plant detritus					"Bobrowski and Clague, 1995"	Abstract	1995	92 E/15
"Catala Lake, B.C."	11	6		49.8328	-127.0593	Lake	Coastal lake	500	Open coast	<1 m above high tide		Piston corer (lake)	"22, 7 in lake and 15 in marsh bordering lake"	2+	2+					1	1			170±40	0 - 343 	1700	"Radiocarbon (AMS) - youngest of 5 ages on plant detritus capping sand layer, most closely approximates age of deposit"	2		"Thins away from outlet, discontinuous at southernmost core site where it consists of fine sand a few mm thick."				Gyttja	Gyttja					"Sandy granule gravel, fines to fine sand."	Fines away from outlet		Poorly sorted	 Well-rounded stones	Sand and shell fragments	Coarse plant sdetritus		Marine shoreface and brackish diatom and foram assemblages			"Clague et al., 1999"	Journal	1999	92 E14
"Catala Lake, B.C."	12	6		49.8328	-127.0593	Lake	Coastal lake	500	Open coast	<1 m above high tide		Piston corer (lake)	"22, 7 in lake and 15 in marsh bordering lake"	2+	2+					2+	2+			1250±50	1000-1389		"Radiocarbon (AMS) - youngest of 5 ages for this layer, from spruce and fir needles"	0.5 -1.0						Gyttja	Gyttja					Sand and shell fragments		Masssive	Moderately sorted					Marine shoreface and brackish diatom and foram assemblages			"Clague et al., 1999"	Journal	1999	92 E14
"Catala Lake, B.C."	13	6		49.8328	-127.0593	Marsh	Coastal lake	500	Open coast	<1 m above high tide		"Gouge corer (marsh), push core (10 cm aluminum irrigation pipe - 1 marsh site)"	"22, 7 in lake and 15 in marsh bordering lake"	"1, possibly 2 in one core"	"1, possibly 2 in one core"					1	1			1000±60	790-1099		"Radiocarbon (AMS), obtained from bark"	0.5		"Present in most marsh cores, but often only as a trace. Thickest near lakeshore, rapidly pinches out upslope and away from lake."				Organic-rich mud	Organic-rich mud			4.0 - 2.0		Fine to very fine sand and silt											"Clague et al., 1999"	Journal	1999	92 E14
"Deserted Lake, B.C."	14	7	DL-2	49.7700	-126.5000	Lake	Coastal lake	500	Open coast		5 (maximum elevation)	Percussion corer	11	3	3	y	2	2		1	1	1	0.5-1.0	400±50	360-570	1700	Radiocarbon (AMS)Youngest of three age determinations on reworked material			"Cores collected close to stream outlet contain some, but not all of the deposits represented at Deserted Lake. Part of upper sequence may be eroded, possibly by a tsunami."	6		"5 thin (1-5 cm) layers of sand or muddy sand separated by thin layers of sandy, woody detritus. Uppermost thin sand layer overlain by thin mud layer overlain by 11 cm weakly graded clean fine sand layer topped by thin layer of plant detritus."	Gyttja	Gyttja	Sharp				Sand or muddy sand (lower layers) to clean fine sand (upper layer).			 			Capped by plant detritus		"Brackish and freshwater diatom assmblages, marine diatoms increase upward through unit."			"Hutchinson et al., 2000"	Journal	2000	92 E15
"Deserted Lake, B.C."	15	7	DL-2	49.7700	-126.5000	Lake	Coastal lake	500	Open coast		 	Percussion corer	11	3	3	y	2	2		2	2	2	"substantially less than the 0.5-0.7 m that occurred at Tofino, 80 km to the SE"	1750±60	1580-1870	"Event S (Atwater and Hemphill-Haley, 1997)"	Radiocarbon (AMS) on bark fragment			"Cores collected close to stream outlet contain some, but not all of the deposits represented at Deserted Lake. Part of upper sequence may be eroded, possibly by a tsunami."	3		2 thin sand layers separated by sandy gytja. Overlain by poorlystatified bed of sandy  mud containing woody detritus.	Gyttja	Gyttja	Sharp				Coarse-textured beds.			 			Woody detritus		Marine and brackish diatom and protazoan assemblages			"Hutchinson et al., 2000"	Journal	2000	92 E15
"Deserted Lake, B.C."	16	7	DL-2	49.7700	-126.5000	Lake	Coastal lake	500	Open coast		5 (maximum elevation)	Percussion corer	11	3	3		2			3	3			2630±60	2450-2900	"Event N (Atwater and Hemphill-Haley, 1997)"	Radiocarbon (AMS) on piece of wood	base of core		"Cores collected close to stream outlet contain some, but not all of the deposits represented at Deserted Lake. Part of upper sequence may be eroded, possibly by a tsunami."					Gyttja					Gravelly sand					Sand and shell fragments	"Mussel shells (shell hash), plant detritus"		"Planktonic, benthic, and brackish marine diatom and protazoan assemblages"			"Hutchinson et al., 2000"	Journal	2000	92 E15
"Deserted Lake, B.C."	17	7		49.7700	-126.5000	Lake	Coastal lake	500	Open coast		5	Percussion corer																																						Listed in table of lakes containing tsunami deposits	"Clague et al., 2000"	Journal	2000	92 E15
"Louie Bay, Vancouver Island, B.C"	18	8		49.7477	-126.9221	Marsh	marsh along coastal inlet																																											Shown on map (Figure 2) of sites presenting geologic evidence of tsunami deposits.	"Lopez and Bobrowski, 2001"	Proceedings	2001	92 E/10
"Louie Bay, Vancouver Island, B.C."	19	8		49.7477	-126.9221	Marsh	marsh along coastal inlet							2	2					1	1					1964																								Listed in table of known tsunami deposits	"Clague et al., 2000"	Journal	2000	92 E/10
"Louie Bay, Vancouver Island, B.C"	20	8		49.7477	-126.9221	Marsh	marsh along coastal inlet							2	2					2	2					1700																								Listed in table of known tsunami deposits	"Clague et al., 2000"	Journal	2000	92 E/10
"Channel Lagoon, Vancouver Island, B.C"	21	9		49.5810	-126.6788	Marsh	marsh along coastal inlet																																											Shown on map (Figure 2) of sites presenting geologic evidence of tsunami deposits.	"Lopez and Bobrowski, 2001"	Proceedings	2001	92 E/10
"Channel Lagoon, Vancouver Island, B.C"	22	9		49.5810	-126.6788	Marsh	marsh along coastal inlet																			Older than 1700																								Listed in table of known tsunami deposits	"Clague et al., 2000"	Journal	2000	92 E/10
"Kanim Lake, Vancouver Island, B.C."	23	10	6	49.4000	-126.3400	Lake	Lake in bedrock-rimmed basin	700	Open coast	6		Piston corer		1	1					1	1			2800±50	2780 - 3440 		AMS radiocarbon	9		Sand layer thicker to north near outlet stream(core 7)than in core 6. Disapears in cores farther south away from outlet.				Gyttja	Gyttja	Sharp	Gradional			Sand			 			"Plant detritus (branches, twigs, bryophyte fragments,conifer needles, seeds, and cones). Plant debris coarsens and increases in abundance downward."		"Marine diatoms (Plagiogramma staurophorum, Opephora pacifica, Opephora marina)"		"Distance inland based on tsunami entering lake from outlet stream, not over10m high rocky isthmus (probably 7.5 m  at time of tsunami). Outlet stream may also have been shorter at time of tsunami."	"Hutchinson et al., 1997"	Journal	1997	92 E/08
"Kanim Lake, Vancouver Island, B.C."	24	10	7	49.4000	-126.3400	Lake	Lake in bedrock-rimmed basin	700	Open coast	6		Piston corer		1	1					1	1			2700±50	2740-3000		AMS radiocarbon	20		Sand layer thicker to north near outlet stream (core 7) than in core 6. Disapears in cores farther south away from outlet.				Gyttja	Gyttja	Sharp	Gradional			Coarser sand		Plant debris coarsens downward				"Plant detritus (branches, twigs, bryophyte fragments,conifer needles, seeds, and cones). Plant debris coarsens and increases in abundance downward."		"Marine diatoms (Plagiogramma staurophorum, Opephora pacifica, Opephora marina)"		"Distance inland based on tsunami entering lake from outlet stream, not over10m high rocky isthmus (probably 7.5 m  at time of tsunami). Outlet stream may also have been shorter at time of tsunami."	"Hutchinson et al., 1997"	Journal	1997	92 E/08
"Kanim Lake, Vancouver Island, B.C."	25	10		49.4000	-126.3400	Lake	Lake in bedrock-silled basin	1000	Length of outlet stream	6		Cores		1	1					1	1																									Forest detritus		Marine-brackish planktonic and benthic diatoms			"Hutchinson et al., 1995"	Abstract	1995	92 E/08
"Kanim Lake, Vancouver Island, B.C."	26	10		49.4000	-126.3400	Lake																				Older than 1700																								Listed in table of lakes containing tsunami deposits	"Clague et al., 2000"	Journal	2000	92 E/08
"Hot Springs Cove, Vancouver Island, B.C."	27	11		49.3700	-126.2700	Marsh	Marsh along coastal inlet.																																											Shown on map (Figure 2) of sites presenting geologic evidence of tsunami deposits.	"Lopez and Bobrowski, 2001"	Proceedings	2001	92 E/08
"Port Alberni, Vancouver Island, B.C."	28	12		49.2500	-124.8300	Marsh	Marsh at head of coastal inlet.					"Pits, sonic corer , field exposures at banks of tidal channels."	50	3 (8 additionalsand layers in sonic drill hole)	3					1	1			< 360±50		1964	"High concentrations of137Cs, eye witness accounts of sand deposition, radiocarbon on twig 60 cm below sand sheet"	1-2 (average)	15.00	"Relatively uniform in thicknes, unusually thick (up to 15 cm) at some sites south of pipeline, north of pipeline, sand is thin and discontinuous."				"Peat (less rooty, more muddy)"	"Peat (rooty, dusky brown,minor mud)"		Sharp	3.0 - 1.0	5 - 30% silt	Fine to medium sand	Uniform in texture	Massive	Moderately well		"Q,F,L"	"Twigs, branches,logs bark seeds conifer cones and needles, also occur as a mat on top of sand sheet also includes rare tests of foraminifera"				"8 additional sand layers (11 total) were penetrated in the sonic drill hole, but not all of these are necessarilly tsunami deposits. Only top 3 sand layers are described."	"Clague and Bobrowski, 1994a"	Journal	1994	92 F2
"Port Alberni, Vancouver Island, B.C."	29	12		49.2500	-124.8300	Marsh	Marsh at head of coastal inlet.					"Pits, sonic corer , field exposures at banks of tidal channels."	50	3 (8 additionalsand layers in sonic drill hole)	3	possible evidence for minor coseismic subsidence (occasional peat underlying deposit) but subsidence could also be atributed to compaction or liquifaction. Site lies near eastern margin of zone of coseismic subsidence.				2	2			270±50	0-500	1700	Radiocabon - youngest of10  dates taken from top of peat/base of sand	5  (average)		"Relatively uniform in thicknes, does not vary near  pipeline. "			Thin lamina of distinctly finer sand at the base of the deposit.	"Mud (yellowish gray to orangish brown, organic rich), peat at some sites"	"Mud (yellowish gray to orangish brown, organic rich), peat at some sites"	"Sharp, except where bioturbated"	"Sharp, except where bioturbated"	4.0 - 1.0		"Medium to very fine sand and minor silt, scattered granules and pebbles near base at some sites."		Massive	Moderately well			"Wood detrirus, underlying peat contains rhizomes of herbaceous marsh plants, notably Triglochin maritimum."				"8 additional sand layers (11 total) were penetrated in the sonic drill hole, but not all of these are necessarilly tsunami deposits. Only top 3 sand layers are described."	"Clague and Bobrowski, 1994a"	Journal	1994	92 F2
"Port Alberni, Vancouver Island, B.C."	30	12		49.2500	-124.8300	Marsh	Marsh at head of coastal inlet.					"Pits, sonic corer , field exposures at banks of tidal channels."	50	3 (8 additionalsand layers in sonic drill hole)	3					3	3			880±90	600-1000		Radiocabon - youngest of 5  dates taken from top of peat/base of sand	12-68					"Well stratified, at some sites a coarse to fine fining up sequence overlies massive sand."	Sandy silty mud and muddy sand	Mud (organic-rich)	Sharp	Sharp			Sand and pebble gravel		Fining up - pebble gravel grades into fine sand				"Wood detrirus, cones, twigs"				"8 additional sand layers (11 total) were penetrated in the sonic drill hole, but not all of these are necessarilly tsunami deposits. Only top 3 sand layers are described."	"Clague and Bobrowski, 1994a"	Journal	1994	92 F2
"Port Alberni, Vancouver Island, B.C."	31	12		49.2500	-124.8300	Marsh	Marsh at head of coastal inlet.					"Pits, sonic corer , field exposures at banks of tidal channels."	14	1 (only uppermost sand layer documented)	1 (only uppermost sand layer documented)					1	1			< 360±50	< 300-510	1964	"137Cs, radiocarbon on twig 60 cm below sand sheet"	1-2	15.00					"Peat (less rooty, more muddy)"	Brown rooty peat w/ interstitial mud	Sharp	Sharp	3.0 - 2.0	5 - 30% silt	Fine grained		Massive	Moderately well	"Olive gray (Munsell colours 5Y 5/1, 5Y 4/2)"		"Branches, sticks, seeds and cones scattered throughout sediment, in some places forming capping layer."		Rare tests of foraminifera		"Second, most destructive wave ~7m high, inundating tidal marsh 4-5 meters."	Clague et al. 1994	Journal	1994	92 F2
"Kakawis Lake, B.C."	32	13		49.1941	-125.8887	Lake	Coastal lake located on western peninsula of Meares Island	500	Up outlet stream	3-4		Percussion corer	6	3-4	3-4					1	1			3220±50 	1430-1520		AMS - pine cone from within the deeposit		30				Displays weak laminae.	Gyttja	Dark brown to dark olive silt and sand-rich gyttja		Gradational			Bimodal - medium sand to pebbles in a silty matrix.				Chaotic						"14,000 year record.  Tsunami deposits are described from oldest (1) to youngest (3) with another possible undated tsunmai deposit (labled with a ""?"", not described here) found between deposits 1 and 2. In the database, event numbers have been changed from youngest (1) to oldest (3) to be consistent with the rest of the database. Possible corelations with events described in Atwater and Hemphill-Haley (1997) are presented in Table 1 in the text."	"Lopez and Bobrowski, 2001"	Proceedings	2001	92F/4
"Kakawis Lake, B.C."	33	13		49.1941	-125.8887	Lake	Coastal lake located on western peninsula of Meares Island	500	Up outlet stream	3-4		Percussion corer	6	3-4	3-4					2	2			3410±60 	1680-1750		AMS - bark and twig samples in layer		20					Gyttja	Gyttja					Unimodal - finer grained sand than event 3.						Considerably more plant detritus accumulated near top of layer.				"14,000 year record.  Tsunami deposits are described from oldest (1) to youngest (3) with another possible undated tsunmai deposit (labled with a ""?"", not described here) found between deposits 1 and 2. In the database, event numbers have been changed from youngest (1) to oldest (3) to be consistent with the rest of the database. Possible corelations with events described in Atwater and Hemphill-Haley (1997) are presented in Table 1 in the text."	"Lopez and Bobrowski, 2001"	Proceedings	2001	92F/4
"Kakawis Lake, B.C."	34	13		49.1941	-125.8887	Lake	Coastal lake located on western peninsula of Meares Island	500	Up outlet stream	3-4		Percussion corer	6	3-4	3-4					3	3			3300±50	1515-1635		"AMS -twig and wood samples dated, minimum age reported"	16-23			3	5	Closely spaced intercalation between much smaller 5-cm sheets.	Gyttja	Gyttja	Erosional				"Texturally bimodal - a mix of med to coarse sand and gravel, shell fragments with low amounts of plant detritus and a silty matrix."						Plant detritus				"14,000 year record.  Tsunami deposits are described from oldest (1) to youngest (3) with another possible undated tsunmai deposit (labled with a ""?"", not described here) found between deposits 1 and 2. In the database, event numbers have been changed from youngest (1) to oldest (3) to be consistent with the rest of the database. Possible corelations with events described in Atwater and Hemphill-Haley (1997) are presented in Table 1 in the text."	"Lopez and Bobrowski, 2001"	Proceedings	2001	92F/4
"Kakawis Lake, B.C."	35	13		49.1941	-125.8887	Lake	Coastal lake located on western peninsula of Meares Island	200	Open coast																	older than 1700																								Cited as an unpublished site in a table	"Clague et al., 2000"	Journal	2000	92F/4
"Tofino, Vancouver Island, B.C."	36	14		49.1162	-125.8813	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3	n	1	1	1	1	1					1964	Same stratigraphic position as uppermost sheet at Port Alberni.	0.1 - 0.5		Discontinuous				Contemporary marsh root zone	Contemporary marsh root zone			4.0  -  1.0		Medium to very fine sand and silt		Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"			Rare foraminiferal tests		"Tsunami deposit present in root zone of contempory marsh a Ucluelet, locally on Meares Island and along Browning Passage."	"Clague and Bobrowski, 1994a"	Journal	1994	92F/4
"Tofino, Vancouver Island, B.C."	37	14		49.1162	-125.8813	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3	y	1	1	1	2	2	1	Several decimeters	"160±60, 180±50, 190±60"	0-470	1700	Radiocabon - youngest of10  dates taken from top of peat/base of sand	<1 - 30 		"Thinner at Ucluelet than in Browning passage, discontinuous in Grice bay; extends from seaward edge of marsh to forest, thickest in tidal flats at head of broad, north-facing bays,along tidal channels, and thinnest in W & SW facing bays and inlets. In Browning Passsage, thins in forest adjacent to marsh."				"Peat (rooty, fibrous, dusky brown, muddy)"	Mud	"Abrupt; erosive in places, other places preserve delicate leaves of herbaceous plants which extend upward into sand or are matted down below"	Sharp	4.0  -  1.0		Medium to very fine sand and silt	"In Browning Passage, fines to silt in forest adjacent to marsh"	Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"	"Bark, twigs, branches, cones, other plant detritus"		Forams( change from upper marsh to middle marsh)		"Sample sites cover large area between Ucluelet and Tofino, including Browning Passage, Mears Island and Grice bay. This part of the Coast of Vancouver Island is being uplifted. Only relatively recent tsunami deposits preserved."	"Clague and Bobrowski, 1994a"	Journal	1994	92F/4
"Tofino, Vancouver Island, B.C."	38	14		49.1162	-125.8813	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3		1	1	1	3	3			"650±50, 680±50"	500-800		Radiocarbon - from cone and twig at top of peaty mud	Similar to second sand sheet (<1 - 30)		Encountered in several pits at Tofino and Ucluelet.				Mud	Mud	Abrupt	Sharp	4.0  -  1.0		Medium to very fine sand and silt		Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"			Rare foraminiferal tests		"This third sand sheet is simply described as ""similar to the second snd sheet"" except noting the  contacts are sharp and the over- and underlying material is olive-gray mud. All other inferences based on second sand sheet. "	"Clague and Bobrowski, 1994a"	Journal	1994	92F/4
"Tofino, Vancouver Island, B.C."	39	14		49.1162	-125.8813	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	1	1	y	1	1	0	1	1	1		180±50	0-470	1700	Conventional and AMS radiocarbon. Tofino and Uclelet are reported together. 	A few mm to 30 cm		"Sheetlike, discontinuous at Grice Bay, present from seaward edge of marsh to forest margin."				Peat	Mud	"Sharp, locally eroded"	Sharp	4.0  -  1.0		Sand		Massive	Moderately well					Intertidal foraminifera		"Sheltered setting - includes sites on Meares Island, Grice Bay, and along Browning Passage south of Tofino"	"Clague and Bobrowski, 1994b"	Journal	1994	92F/4
"Ucluelet, Vancouver Island, B.C."	40	15		48.9500	-125.5800	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3	n	1	1	1	1	1					1964	Same stratigraphic position as uppermost sheet at Port Alberni	0.1 - 0.5		Discontinuous				Contemporary marsh root zone	Contemporary marsh root zone			4.0  -  1.0		Medium to very fine sand and silt		Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"			Rare foraminiferal tests		"tsunami deposit present in rootzone of contempory marsh a Ucluelet, locally on Meares Island and along Browning Passage, deposit not described at length"	"Clague and Bobrowski, 1994a"	Journal	1994	92 C/13
"Ucluelet, Vancouver Island, B.C."	41	15		48.9500	-125.5800	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3	y	1	1	1	2	2	1	Several decimeters	"160±60, 180±50, 190±60"	0-470	1700	Radiocabon - youngest of10  dates taken from top of peat/base of sand	<1 - 30		"Thinner at Ucluelet than in Browning passage, discontinuous in Grice bay; extends from seaward edge of marsh to forest, thickest in tidal flats at head of broad, north-facing bays,along tidal channels, and thinnest in W & SW facing bays and inlets. In Browning Passsage, thins in forest adjacent to march."				"Peat (rooty, fibrous, dusky brown, muddy)"	Mud	"Abrupt; erosive in places, other places preserve delicate leaves of herbaceous plants which extend upward into sand or are matted down below."	Sharp	4.0  -  1.0		Medium to very fine sand and silt		Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"	"Bark, twigs, branches, cones, other plant detritus, and rare foraminiferal tests"		Forams( change from upper marsh to middle marsh)		"Sample sites cover large area between Ucluelet and Tofino, including Browning Passage, Mears Island and Grice bay. This part of the Coast of Vancouver Island is being uplifted. Only relatively recent tsunami deposits preserved."	"Clague and Bobrowski, 1994a"	Journal	1994	92 C/13
"Ucluelet, Vancouver Island, B.C."	42	15		48.9500	-125.5800	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	3	3	n	1	1	1	3	3			"650±50, 680±50"	500-800		Radiocarbon - from cone and twig at top of peaty mud	Similar to second sand sheet (<1 - 30)		Encountered in several pits at Tofino and Ucluelet.				Mud	Mud	Abrupt	Sharp	4.0  -  1.0		Medium to very fine sand and silt		Massive	Moderately well	"Mottled, may have been extensively bioturbated"	"Q,F,L"			Rare foraminiferal tests		"This third sand sheet is simply described as ""similar to the second snd sheet"" except noting the  contacts are sharp and the over- and underlying material is olive-gray mud. All other inferences based on second sand sheet. "	"Clague and Bobrowski, 1994a"	Journal	1994	92 C/13
"Ucluelet, Vancouver Island, B.C."	43	15		48.9500	-125.5800	Marsh	Low coastal plain					"Pits, sonic corer , field exposures at banks of tidal channels."	110 at Tofino and Ucluelet	1	1	y	1	1	0	1	1	1		180±50	0-470	1700	Conventional and AMS radiocarbon. Tofino and Uclelet are reported together. 	A few mm to 30 cm		"Sheetlike, present from seaward edge of marsh to forest margin."				Peat	Mud	"Sharp, locally eroded"	Sharp			Sand		Massive	Moderately well					Intertidal foraminifera			"Clague and Bobrowski, 1994b"	Journal	1994	92 C/13
"Port Renfrew, Vancouver Island, B.C."	44	16		48.5700	-124.4000	Marsh	Marsh along coastal inlet							1	1					1	1					1700																									"Clague et al., 2000"	Journal	2000	92 C/9
"Sooke Inlet, Vancouver Island, B.C."	45	17		48.3700	-123.6900	"Marsh, tidal"	Marsh along coastal inlet							1	1	y	1		0	1	1	1	0.2 - 0.7			1700	Radiocarbon			Thins landward											Fines landward							Shallow marine foraminifera		"200km landward from plate boundary, conference abstract, not much info"	"Williams, 1995"	Abstract	1995	92 B/5
"Swantown Marsh, Whidbey Island, WA"	46	18		48.3100	-122.7100	Marsh	Marsh surrounding small coastal lake in lee of small barrier beach.	100	Barrier beach	2.6	5.1 (2.5 m above marsh surface)	"Vibracores, gouge cores, pits"	Cores collected at 10 m intervals.	4	4					1	1			1330±50	1160-1350		AMS radiocarbon on tubers		3	"Thins inland  to the NE,E,S - discontinuous in distal part."	At least 3		Multiple sand-mud normally-graded couplets capped by brown organic detritus.	Peat	Peat	Sharp	Sharp	3.0 - 1.0		Muddy fine-med sand. Fines landward to mud.	Fines inland					Brown organic detritus		"Few diatoms, lttoral and fresh/brackish marine"		"Swantown Marsh is on the west coast of Whidbey Island. Layers 3 and 4 are thought to be products of local earthquakes on the Southern Whidbey Island, Leech River or Devil's Island faults because ages do not correspond to ages of great earthquakes reported by Atwater and Hemphill-Haley(1997)."	"Wiliams and Hutchinson, 2000"	Journal	2000	Oak Harbor
"Swantown Marsh, Whidbey Island, WA"	47	18		48.3100	-122.7100	Marsh	Marsh surrounding small coastal lake in lee of small barrier beach.	230	Barrier beach	2.6	5.1 (2.5 m above marsh surface)	"Vibracores, gouge cores, pits"	Cores collected at 10 m intervals.	4	4					2	2			1630±50	1400-1700		AMS radiocarbon on tubers		3.5	"Thins inland  to the NE,E,S - discontinuous in distal part."	3-4		Multiple sand-mud normally-graded couplets capped by brown organic detritus.	Peat	Peat	Sharp	Sharp	3.0 - 1.0		Muddy fine-med sand. Fines landward to mud.	Fines inland					Brown organic detritus		"Diatoms - littoral, mudflat, salt-marsh, brackish marsh varieties. More marine than layer 1."		"Swantown Marsh is on the west coast of Whidbey Island. Layers 3 and 4 are thought to be products of local earthquakes on the Southern Whidbey Island, Leech River or Devil's Island faults because ages do not correspond to ages of great earthquakes reported by Atwater and Hemphill-Haley(1997)."	"Wiliams and Hutchinson, 2000"	Journal	2000	Oak Harbor
"Swantown Marsh, Whidbey Island, WA"	48	18		48.3100	-122.7100	Marsh	Marsh surrounding small coastal lake in lee of small barrier beach.	50-60	Barrier beach	2.6	5.1 (2.5 m above marsh surface)	"Vibracores, gouge cores, pits"	Cores collected at 10 m intervals.	4	4					3	3			1970±50	1810-2060		AMS radiocarbon on tubers		1.0	Pinches out landward	At least 2		Thin sandy laminae separated by a few mm of muddy organic detritus.	Peat	Peat	Sharp	Sharp											Diatoms ~ 10% marine or littoral		"Swantown Marsh is on the west coast of Whidbey Island. Layers 3 and 4 are thought to be products of local earthquakes on the Southern Whidbey Island, Leech River or Devil's Island faults because ages do not correspond to ages of great earthquakes reported by Atwater and Hemphill-Haley(1997)."	"Wiliams and Hutchinson, 2000"	Journal	2000	Oak Harbor
"Swantown Marsh, Whidbey Island, WA"	49	18		48.3100	-122.7100	Marsh	Marsh surrounding small coastal lake in lee of small barrier beach.	10	Barrier beach	2.6	5.1 (2.5 m above marsh surface)	"Vibracores, gouge cores, pits"	Cores collected at 10 m intervals.	4	4					4	4			2010+50	1830-2120		AMS radiocarbon on peat		0.5		At least 2		Thin sandy laminae separated by a few mm of muddy organic detritus.	Peat	Peat	Sharp	Sharp											Diatoms ~ 10% marine and11% littoral		"Swantown Marsh is on the west coast of Whidbey Island. Layers 3 and 4 are thought to be products of local earthquakes on the Southern Whidbey Island, Leech River or Devil's Island faults because ages do not correspond to ages of great earthquakes reported by Atwater and Hemphill-Haley(1997)."	"Wiliams and Hutchinson, 2000"	Journal	2000	Oak Harbor
"Discovery Bay, WA"	50	19		47.9878	-122.8817	"Marsh, tidal"	Tidal marsh at end of bay							7-9	7-9					1-8	1-8						No ages reported			sand sheets			Some display internal stratification consistent with  deposition by a tsunami wave train.	Peat	Peat					muddy sand								Marine microfossils		2-4 of the sand sheets may be asociated with tsunamis not originating on the CSZ.	"Williams et al., 2002"	Abstract	2002	Uncas
"Discovery Bay, WA"	51	19		47.9878	-122.8817	"Marsh, tidal"	Tidal marsh at end of bay							7-9	7-9					1-8	1-8				2150-2750		Radiocarbon			sand sheets			Some display internal stratification consistent with  deposition by a tsunami wave train.	Peat	Peat					muddy sand								Marine microfossils		2-4 of the sand sheets may be asociated with tsunamis not originating on the CSZ.	"Williams et al., 2002"	Abstract	2002	Uncas
"Copalis River, WA"	50	19		47.1200	-124.1600	Marsh	Marshes along river					"Cutbank exposures, hand-drilled cores."		3	2	y	3	2	0	1	1	1	0.5		0-600	1700	"Conventional radiocarbon - correlates to 1700 event based on similar appearance to tree-ring dated horizons at Willipa Bay, Washington (Yamaguchi et al., 1989, Atwater et al., 1991))."			Disappears upstream				Peaty black soil	Mud	mantled		4.0 - 2.0		Very fine to fine sand											"Atwater, 1992"	Journal	1992	"Copalis Beach, WA"
"Copalis River, WA"	51	19		47.1200	-124.1600	Marsh	Marshes along river					"Cutbank exposures, hand-drilled cores."		3	2	y	3	2	0	3	2	3	decimeters		1400-1900		Radiocarbon	A few cm		Found as far upstream as similar sand layer (see entry above).				Reddish brown fibrous peat	Mud	mantled		4.0 - 2.0		Very fine to fine sand											"Atwater, 1992"	Journal	1992	"Copalis Beach, WA"
"Copalis River, WA"	52	19		47.1200	-124.1600	Marsh	Marshes along river	2000	River mouth     (2 km inland)			Cutbank exposures		1	1	y	1	1	0	1	1	1						0-10		Thins from 10 cm near channel mouth to 0 cm 2 km inland.			"Thin discontinuous lamina of mud, overlain by a single continuous bed of sand thinning from approximately 10cm near the channel mouth to 0 cm ~2km inland"	Peat	Mud			3.0 - 2.0		"Fine-grained, well rounded sand"		"Massive, ungraded"			"10-15%muscovite, 10-25% subangular quartz"	peat and mud rip up clasts	Landward directed surge				"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Copalis Beach, WA"
"North Bay, Grays Harbor, WA"	53	20		47.0500	-124.1000	Marsh	Marshes along river					Exposed in drainage ditch		1	1	y	1	1	0	1	1	1						~1.5		Continuous over outcrop (20-30m).	"Up to 5 (general description, see layer characteristics)"		"Sandy bed composed of a thin basal lamina of mud (5mm thick), 2 sandy laminae (4-10mm thick),alternating with mud, capped by a thin (1-2 mm) discontinuous lamina of sandy silt."	peaty soil	Erosionally based thin bed of gravel	Directly above	Erosional			"Sandy, sandy silt"					"10-15% muscovite, 10-25% subangular quartz,  North River sediments lack orthopyroxine and hornblende."		Landward directed surge			2 km west of Humptulips River mouth. Exposed in sides of man-made drainage ditch. several other sites around Grays Harbor show evidence for an anomalous sand layer	"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Hoquiam, WA"
"Johns River, Grays Harbor, WA"	54	21		46.9000	-123.9800	Marsh	Marshes along river that flows into bay					"Cutbank exposures, hand-drilled cores."		8	2	y	8	2	0	1	1	1	0.65-1.05	450±60	"420-540,     390-320"		AMS radiocarbon	2					Slightly laminated	Peat	Mud		Gradual			Silty sand				Grades upwards to assemblages indicative of less sandy intertidal flat				Intertidal diatoms		Concludes localized tsunami deposition cannot be rejected. Sedimentation in sandy tidal flat is equally valid. Lasting submergence is indicated. Sand deposition due to river floods is rejected on basis of diatom assemblages.	"Shennan et al., 1996 "	Journal	1996	"Copalis Crossing, WA"
"Johns River, Grays Harbor, WA"	55	21		46.9000	-123.9800	Marsh	Marshes along river that flows into bay					"Cutbank exposures, hand-drilled cores."		8	2	y	8	2	0	4	2	4	0.35-0.65	4480±80	4240-5310		AMS radiocarbon	2-4					Laminated	Peat	Mud		Gradual			Silty sand				Grades upwards to assemblages indicative of less sandy intertidal flat				Tidal flat diatoms		Concludes localized tsunami deposition cannot be rejected. Sedimentation in sandy tidal flat is equally valid. Lasting submergence is indicated. Sand deposition due to river floods is rejected on basis of diatom assemblages.	"Shennan et al., 1996 "	Journal	1996	"Copalis Crossing, WA"
"Johns River, Grays Harbor, WA"	56	21		46.9000	-123.9800	Marsh	Marshes along river that flows into bay	2000	Upriver			"Cutbank exposures, hand-drilled cores."		1	1	y	1	1	0	1	1	1						~2.5		"Deposit thins away from channel, laminae thin upward."			"Thin (1-5 mm) discontinuous laminae of mud, a thick (2 cm)basal sandy lamina, overlain by 2-3 thin sandy lamina (each 2-3 mm thick)."	Peat	Mud	Sharp (mostly - 30% gradational 1-3mm boundaries)general description for deposits at all sites in report).	Sharp (mostly - 30% gradational 1-3mm boundaries)general description for deposits at all sites in report).	4.0 - 3.0		Silt with very fine sand		Massive (each laminae in the layer)			"10-15%muscovite, 10-25% subangular quartz"		Landward directed surge			"With the exception of Johns River, anomalous sands are asbsent along entire south shore of Grays Harborand in South Bay"	"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Copalis Crossing, WA"
"Grayland Plains, WA"	57	22		46.8334	-124.0891	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands	1000 m from present shoreline	open coast		6	"Cutbank exposures, gouge cores, pipe cores"	27	2-3	2-3					1	1					1700		0.3-10																						"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analyses in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Grayland, WA"
"Grayland Plains, WA"	58	22		46.8334	-124.0891	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands	"1500 m from present shoreline, 1000 m from erosional scarp interpreted as paleoshoreline"	open coast		6	"Cutbank exposures, gouge cores, pipe cores"	27	2-3	2-3					2	2				655-880	800 cybp	AMS radiocarbon	0.2-5																						"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analyses in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Grayland, WA"
"Grayland Plains, WA"	59	22		46.8334	-124.0891	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands					"Cutbank exposures, gouge cores, pipe cores"																																							Schlichting et al. 1999	Abstract	1999	"Grayland, WA"
"North River, Willipa Bay, WA"	60	23		46.7500	-123.8934	Marsh	Marshes along river that flows into bay.	1000	upriver			"Cutbank exposures, hand-drilled cores"		1	1	y	1	1	0	1	1	1						~2		"West of main channel only at North River, disapears as it enters paleoforest at Smith River"	3		Muddy lamina (10-25mm) overlain by sandy silt (2cm) capped by 2 thin (1-6mm) lamina of coarse silt.	Peat	Mud					Sandy silt to coarse silt					"10-15% muscovite, 10-25% subangular quartz, plus nearly equal amounts of orthopyoxine, clinopyroxine, and hornblende at Niawiakim River, North River sediments lack orthopyroxine and hornblende."		Landward directed surge				"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Bay Center, WA"
"North River, Willipa Bay, WA"	61	23		46.7500	-123.8934	Marsh	Marshes along river that flows into bay.																			1700		<10 cm		"Regionally distributed, landward thining, Thicker downstream than upstream"		"0.8-1.0 near base, thin to 0.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt											"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Smith River, Willipa Bay, WA"	62	24		46.7400	-123.8734	Marsh	Marshes along river that flows into bay.	500	Upriver			"Cutbank exposures, hand-drilled cores"		1	1	y	1	1	0	1	1	1						~2		"West of main channel only at North River, disapears as it enters paleoforest at Smith River."	3		Muddy lamina (10-25mm) overlain by sandy silt (2cm) capped by 2 thin (1-6mm) lamina of coarse silt.	Peat	Mud					Sandy silt to coarse silt					"10-15% muscovite, 10-25% subangular quartz, plus nearly equal amounts of orthopyoxine, clinopyroxine, and hornblende at Niawiakim River, North River sediments lack orthopyroxine and hornblende."		Landward directed surge				"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Western, WA; Bay Center, WA"
"Cedar River, Willipa Bay, WA"	63	25		46.7400	-123.9700	Marsh	Marshes along river that flows into bay.																			1700		<10 cm		"Regionally distributed, landward thining, thicker downstream than upstream."		"0.8-1.0 near base, thin to 0.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt											"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Bone River, Willipa Bay, WA"	64	26		46.6600	-123.9200	Marsh	Marshes along river that flows into bay.					"Cutbank exposures, hand-drilled cores"		1	1	y	1	1	0	1	1	1								"Thinning of layer upvalley, laminae thin upward, thicker sand laminae occur at outside corner of channel beds."	4-5 layers		"Thin (1-5 mm) laminae alternating with layers of mud, layers thin upward, often topped by coarse silt couplet, number of layers decrease with each successive bar upstream."	Peat	Mud	Sharp (mostly - 30% gradational 1-3mm boundaries).	Sharp (mostly - 30% gradational 1-3mm boundaries).	4.0 - 3.0		Silt with very fine sand	"Fines upvalley, as sand size decreases, silt proportion increases while clay remains the same."	Massive (each laminae in the layer)			"10-15% muscovite, 10-25% subangular quartz, plus nearly equal amounts of orthopyoxine, clinopyroxine, and hornblende at Niawiakim River, North River sediments lack orthopyroxine and hornblende."		Landward directed surge				"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Bay Center, WA"
"Bone River, Willipa Bay, WA"	65	26		46.6600	-123.9200	Marsh	Marshes along river that flows into bay.																			1700		<10 cm		"Regionally distributed, landward thining, thicker downstream than upstream."		"0.8-1.0 near base, thin to 0.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt											"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	66	27		46.6300	-123.9200	Marsh	Marshes along river that flows into bay.					"Gouge cores, outcrop"		8	1	y	8	1	0	1	1	1				1700	"Corellation with previous studies (e.g. Satake et al., 1996;  Nelson et al., 1995)"	5.0-7.0 (mainly)	15.00		5-6 layers		"5-6 sandy laminae alternate with mud. Lowest of laminae least distinct, least continuous. Upper two laminae silt partings."	Peat				4.0 - 3.0		Silty very fine sand				"Flopovers (tufts of Deschampsia caespitosa flopped over to the east (aimuths 65û-120û, average: 82û)"	Micaceous	"plant fragments (bark-free twigs, pieces of bark up to 1 cm thick,leaf bases of Triglochin maririma, tufts of Deschampsia caespitosa)"	"East, up Niawiakum River valley"	Diatoms		Tsunami data represents a compilation of data presented for the Redtail and Oyster localities along the Niawiakum River 	"Atwater and Hemphil-Haley, 1997"	USGS Professional Paper	1997	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	65	27		46.6300	-123.9200	Marsh	Marshes along river that flows into bay.					Cores and outcrops		6	1	y	6	1	0	1	1	1				1700		"Less than 1 cm thick (or no deposit) to more than 5 cm thick, depending on location along tidal channel."																			Through inlet of willapa Bay and up Niawiakum River			Contains black and white photographs of deposit and maps showing distribution and thickness of sandy interval and path of inferred tsunami.	"Atwater, 1996"	USGS professional Paper	1996	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	67	27	Near river  mouth	46.6300	-123.9200	"Marsh, tidal"	Marshes along river that flows into bay.		Upriver	2.4-2.5 m above MLLW		Vertical slabs	4 sites/sections	1+	1+	y	1+	1	0	1	1	1	0.7 - > 3.0			1700	Corellation with previous studies	5		Thins and pinches out landward.			Very fine sand and silt laminae 5 - 10 mm thick.	Soil	Tidal flat mud	Sharp				 Silty sand								"Diatoms (0pen estuarine, sand flat)"		Study focuses on diatom as method for identifying tsunami deposits. Describes changes in diatom assemblages with distance inland.	"Hemphil-Haley, 1995"	Journal	1995	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	68	27	1 km upriver from site 1	46.6300	-123.9200	"Marsh, tidal"	Marshes along river that flows into bay.		Upriver	2.4 m above MLLW		Vertical slabs	4 sites/sections	1+	1+	y	1+	1	0	1	1	1	1.0 - >3.0			1700	Corellation with previous studies	0.1		Thins and pinches out landward.				Soil	Mud	Sharp		4.0 - 3.0		Very fine sand								"Diatoms (benthic, tidal flat)"		Study focuses on diatom as method for identifying tsunami deposits. Describes changes in diatom assemblages with distance inland.	"Hemphil-Haley, 1995"	Journal	1995	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	69	27	"Upriver from site 2, upper midle part of valley"	46.6300	-123.9200	"Marsh, tidal"	Marshes along river that flows into bay.		Upriver	2.2 m above MLLW		Direct field sampling	4 sites/sections	1+	1+	y	1+	1	0	1	1	1				1700	Corellation with previous studies	0.5		Thins and pinches out landward.				Soil	Mud	Sharp		4.0 - 3.0		Very fine sand								"Diatoms (0pen estuarine, sand flat)"		Study focuses on diatom as method for identifying tsunami deposits. Describes changes in diatom assemblages with distance inland.	"Hemphil-Haley, 1995"	Journal	1995	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	70	27	"Upriver from site 3, upper reaches of tidal river"	46.6300	-123.9200	"Marsh, tidal"	Marshes along river that flows into bay.		Upriver			Direct field sampling	4 sites/sections	1+	1+	y	1+	1	0	1	1	1				1700	Corellation with previous studies	0 ( no tsunami deposit this far upriver)		Thins and pinches out landward.																		"Diatoms (0pen estuarine, sand flat)"		Study focuses on diatom as method for identifying tsunami deposits. Describes changes in diatom assemblages with distance inland. Sand flat diatoms may have been transported above upriver limit of preservation of sand deposits	"Hemphil-Haley, 1995"	Journal	1995	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	71	27		46.6300	-123.9200	Marsh	Marshes along river that flows into bay.	3000	Upriver			"Cutbank exposures, hand-drilled cores"		1	1	y	1	1	0	1	1	1						"Less than 1 cm thick (or no deposit) to more than 5 cm thick, depending on location along tidal channel."		"Thinning of layer upvalley, thicker sand laminae occur at outside corner of channel beds."	4-5 layers		"Thin (1-5 mm) laminae alternating with layers of mud, layers thin upward, often topped by coarse silt couplet, number of layers decrease with each successive bar upstream."	Peat	Mud	Sharp (mostly - 30% gradational 1-3mm boundaries)	Sharp (mostly - 30% gradational 1-3mm boundaries)	4.0 - 3.0		Silt with very fine sand	"Fines upvalley, as sand size decreases, silt proportion increases while clay remains the same."	Massive (each laminae in the layer)			"10-15% muscovite, 10-25% subangular quartz, plus nearly equal amounts of orthopyoxine, clinopyroxine, and hornblende at Niawiakim River, North River sediments lack orthopyroxine and hornblende."		Landward directed surge			several other sites around Willipa Bay show evidence for an anomalous sand layer	"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	72	27		46.6300	-123.9200	Marsh	marshes along river that flows into bay	2500	Inland			Cores	200 cores													1700		<10 cm		"Regionally distributed, landward thining, thicker downstream than upstream."		"0.8-1.0 near base, thin to o.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt											"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Niawiakum River, Willipa Bay, WA"	73	27		46.6300	-123.9200	Marsh	marshes along river that flows into bay					Cores	"outcrop, half-cylinder corer"	6	3	y	6	3	0										7.00	"Sheet-like, thins landward"				Peat	Mud (intertidal)	Mantled		4.0 - 3.0		Sandy-contains very fine sand and coarse silt at x-section line near landward extent of study.	Fines landward									Thin sandy interval mantling at least 3 burried lowlands; coincides with rapid tectonic subsidence. Several sites cored in tidal marsh along Niawiakum River. Study focused on tectonic subsidence as evidence for great earthquakes.	"Atwater, 1987"	Journal	1987	"Bay Center, WA"
"Palix River, Willipa Bay, WA"	74	28		46.6000	-123.9100	Marsh	marshes along river that flows into bay					"Cutbank exposures, hand-drilled cores"		1	1	y	1	1	0	1	1	1								"Thinning of layer upvalley, laminae thin upward, thicker sand laminae occur at outside corner of channel beds."	4- 5 layers		"Thin (1-5 mm) laminae alternating with layers of mud, layers thin upward, often topped by coarse silt couplet, number of layers decrease with each successive bar upstream."	Peat	Mud	Sharp (mostly - 30% gradational 1-3mm boundaries)	Sharp (mostly - 30% gradational 1-3mm boundaries)	4.0 - 3.0		Silt with very fine sand	"Fines upvalley, as sand size decreases, silt proportion increases while clay remains the same."	massive (each laminae in the layer)			"10-15% muscovite, 10-25% subangular quartz, plus nearly equal amounts of orthopyoxine, clinopyroxine, and hornblende at Niawiakim River, North River sediments lack orthopyroxine and hornblende."		Landward directed surge				"Reinhart, 1991"	Thesis (unpublished masters project)	1991	"Nemah, WA"
"Palix River, Willipa Bay, WA"	75	28		46.6000	-123.9100	Marsh	marshes along river that flows into bay																			1700		<10 cm		"Regionally distributed, landward thining, thicker downstream than upstream."		"0.8-1.0 near base, thin to o.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt											"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Nemah River, Willipa Bay, WA"	76	29		46.5100	-123.9100	Marsh	marshes along river that flows into bay																			1700		<10 cm		"Regionally distributed, landward thining, thicker downstream than upstream."		"0.8-1.0 near base, thin to o.1 near top"	Horizontal laminae of sandy silt separated  by mud laminae.	Wetland surface	Mud					Sandy silt										Does not specify North or South Nemah River	"Reinhart and Bourgeois, 1987"	Abstract	1987	"Bay Center, WA"
"Long Beach Peninsula, WA"	77	30		46.4500	-124.0500	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands	"800 m from present shoreline, 300 m from erosional scarp interpreted as paleoshoreline."	Open coast		8	"Gouge cores, vibracores"	65 (30% contain tsunamigenic horizons)	3	3					1	1				300-530	1700		1-4						Peat or sand	Peat					Deposit consists of terrestrial organic-rich detritus within peat in core 11 to a terrestrial detritus/sand mixture on top of a sand layer in core 44.								Elevated levels of marine diatom species	Peak in bromine concentration	"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Cape Disappointment, WA"
"Long Beach Peninsula, WA"	78	30		46.4500	-124.0500	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands	"1500 m from present shoreline, 1000 m from erosional scarp interpreted as paleoshoreline."	Open coast		8	"Gouge cores, vibracores"	65 (30% contain tsunamigenic horizons)	3	3					2	2				665-795	800 cybp		0.3-3 (1-3)						Peat or sand	Peat					Sand								Elevated levels of marine diatom species	Peak in bromine concentration	"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Cape Disappointment, WA"
"Long Beach Peninsula, WA"	79	30		46.4500	-124.0500	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands	"1000 m from present shoreline, 500 m from erosional scarp interpreted as paleoshoreline."	Open coast		8	"Gouge cores, vibracores"	65 (30% contain tsunamigenic horizons)	3	3					3	3				990-1285	1100 cybp		1-3						Peat or sand	Peat			3.5 - 3.0		Fine-upper sand			Well sorted		Quartz rich	"Detrital wood, needles and leaves. Thick (4 cm) detrital cap in most distal core."		Elevated levels of marine diatom species	Peak in bromine concentration	"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Cape Disappointment, WA"
"Long Beach Peninsula, WA"	80	30		46.4500	-124.0500	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands					"Gouge cores, vibracores"																																					Peak in bromine concentration		Schlichting et al. 1999	Abstract	1999	"Cape Disappointment, WA"
"Youngs Bay, Columbia River, OR"	81	31		46.1500	-123.8800	" Marsh, tidal"	" Marsh, tidal"	"10,000"	River mouth					2	2	y	1	1	1	1	1	1				1700	"Presumtion, no radiacarbon dates"	Thinner than lower tsunami deposit						Peat	Mud	Abrupt	Abrupt			Sand											"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Astoria, OR"
"Youngs Bay, Columbia River, OR"	82	31		46.1500	-123.8800	" Marsh, tidal"	" Marsh, tidal"	"10,000"	River mouth					2	2	n	1	1	1	2	2					Tentative correlation with event 800±200 years ago	No radiocarbon dates	Thicker than upper tsunami deposit						Peat	Peat	Abrupt	Gradual			Sand											"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Astoria, OR"
"Stanley Lake, OR"	83	32		46.0100	-123.9100	Lake	Coastal lake and marsh							2	2					1	1			780±90			Radiocarbon							Mud or peat	Mud or peat	Abrupt	Gradual or abrupt			Sandy					75-100% beach sand		 West to eat surge	First appearance or increase in brackish or marine diatoms			"Darienzo et al., 1994"	Journal	1994	"Gearhart, OR"
"Stanley Lake, OR"	84	32		46.0100	-123.9100	Lake	Coastal lake and marsh							2	2					2	2			2370±60			Radiocarbon							Mud or peat	Mud or peat	Abrupt	Gradual or abrupt			Sandy					75-100% beach sand		 West to eat surge	First appearance or increase in brackish or marine diatoms			"Darienzo et al., 1994"	Journal	1994	"Gearhart, OR"
"Stanley Lake, OR"	85	32		46.0100	-123.9100	Lake	Coastal lake and marsh							2	2					1	1					Uppermost sand layer(s) deposited within last 800 years(rcybp)	Radiocarbon	4-68						Mud or peat	Mud or peat	Abrupt	Gradual or abrupt			Sand							"Propagated from west to east through bay mouth, then south"				"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Gearhart, OR"
"Stanley Lake, OR"	86	32		46.0100	-123.9100	Lake	Coastal lake and marsh							2	2					2	2					Uppermost sand layer(s) deposited within last 800 years(rcybp)	Radiocarbon	4-68						Mud or peat	Mud or peat	Abrupt	Gradual or abrupt			Sand							"Propagated from west to east through bay mouth, then south"				"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Gearhart, OR"
"Necanicum River, OR"	87	33		45.9900	-123.9300	"Marsh, tidal "	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	5	2	2	n		0	1	1	1					1964	"Radiocarbon (wood), historical artifact (glass shard)"			Continuous for 2 km along seaside spit.				Rooted muds	Rooted muds					Sand						Historical artifacts				No prehistoric marsh deposits to preserve paleotsunami inundation.	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Necanicum River, OR"	88	33		45.9900	-123.9300	"Marsh, tidal "	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	5	2	2	n		0	1	2	2					1946	"Radiocarbon (wood), historical artifact (glass shard)"			Continuous for 2 km along seaside spit.				Rooted muds	Rooted muds					Sand						Historical artifacts				No prehistoric marsh deposits to preserve paleotsunami inundation.	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	89	34		45.9900	-123.9200	"Marsh, tidal "	Marshes along tidal creek							6		y	6											0-26		Pinches out with distance down tidal channel (to north).																	"Surged over spit at south end of Seaside, then down tidal channel (to north)"			Discusses tsunami sands as associated with the coseismic burial events but does not discuss individual layers or whether all burial events have associated tsunami sands.	"Peterson et al., 1993 "	"Journal, field trip guide"	1993	"Tillamook Head, OR"
"Neawanna Creek, OR"	90	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	4	y	5	3	1	1	1	1		480±60	240-720		Radiocarbon dates from Neawanna 2 core							Muddy to sandy peat	Peaty mud to sand	Abrupt	Abrupt								Increased or coarsening of beach sand component			First appearance or increase in brackish or marine diatoms			"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Neawanna Creek, OR"	91	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	4	n	5	3	1	2	2			800±60 680±60	560-1040  360-1000		"First radiocarbon dates from Neawanna 2 core, second dates from Neawanna 5."							Muddy to sandy peat	Muddy to sandy peat	Abrupt									Increased or coarsening of beach sand component			First appearance or increase in brackish or marine diatoms			"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Neawanna Creek, OR"	92	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	4	y	5	3	1	3	3	2		1100±70	820-1380		Radiocarbon dates from Neawanna 2 core							Peaty mud to sand	Peaty mud to sand	Abrupt									Increased or coarsening of beach sand component			First appearance or increase in brackish or marine diatoms			"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Neawanna Creek, OR"	93	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	4	y	5	3	1	4	4	3		1370±70	1090-1650		Radiocarbon dates from Neawanna 2 core							Peaty mud to sand	Peaty mud to sand	Gradual															"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Neawanna Creek, OR"	94	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	5	y	6	5	0	1	1	1	0.5+	480±60			Radiocarbon dates from Neawanna 2 core		26.00	Pinches out down tidal channel to the north.				Peat to peaty mud to sand (depending on site)	Peat to peaty mud to sand (depending on site)	Abrupt	Gradual			Sandy					Increased or coarsening of beach sand component	"Round gravel-sized mudstone clasts mixed with woody debris, probably of debris flow origin. Only found in upper reaches of Neawanna creek."	"Surged over spit at south end of Seaside, then down tidal channel (to north)"	First appearance or increase in brackish or marine diatoms		Northward propagation of tsunami supported by pinching out to the north down tidal channel and sand mineralogy. Tsnami deposit distinguished from riverdeposit by heavy mineral content and relative rounding of sand grains.	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	95	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	5	y	6	5	0	2	2	2	0.5+	"800±60, 680±80"			"First radiocarbon dates from Neawanna 2 core, second dates from Neawanna 5."			Pinches out down tidal channel to the north.				Peat to peaty mud to sand (depending on site)	Peat to peaty mud to sand (depending on site)	Abrupt	Abrupt			Sandy					Increased or coarsening of beach sand component		"Surged over spit at south end of Seaside, then down tidal channel (to north)"	First appearance or increase in brackish or marine diatoms		Northward propagation of tsunami supported by pinching out to the north down tidal channel and sand mineralogy. Tsnami deposit distinguished from riverdeposit by heavy mineral content and relative rounding of sand grains.	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	96	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	5	y	6	5	0	3	3	3	0.5+	1100±70			Radiocarbon dates from Neawanna 2 core			Pinches out down tidal channel to the north.				Peat to peaty mud to sand (depending on site)	Peat to peaty mud to sand (depending on site)	Abrupt	Gradual			Sandy					Increased or coarsening of beach sand component	"Round gravel-sized mudstone clasts mixed with woody debris, probably of debris flow origin. Only found in upper reaches of Neawanna creek."	"Surged over spit at south end of Seaside, then down tidal channel (to north)"	First appearance or increase in brackish or marine diatoms		Northward propagation of tsunami supported by pinching out to the north down tidal channel and sand mineralogy. Tsnami deposit distinguished from riverdeposit by heavy mineral content and relative rounding of sand grains.	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	97	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	5	y	6	5	0	5	4	5					Not dated			Pinches out down tidal channel to the north.				Peat to peaty mud to sand (depending on site)	Peat to peaty mud to sand (depending on site)	Abrupt	Abrupt			Sandy	"Fines upstream at site 7, indicating downstream source"				Mostly river sand	"Round gravel-sized mudstone clasts mixed with woody debris, probably of debris flow origin. Only found in upper reaches of Neawanna creek."	"Surged over spit at south end of Seaside, then down tidal channel (to north)"			"This layer is composed of mostly river sand, suggesting river flooding instead of a tsunami deposit. However,, at site 7, the coarse sand fines upstream, suggesting a downriver source"	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	98	34		45.9900	-123.9200	"Marsh (high), or forested lowland"	Marshes along tidal creek					"2.5 cm gouge corer, 5-7.5 cm pipe corer"	27	6	5	y	6	5	0	6	5	6	1.0-1.5 	2000±70 2200±90			"First radiocarbon dates from Neawanna 2 core, second dates from Neawanna 5."			Pinches out down tidal channel to the north.				Peat to peaty mud to sand (depending on site)	Peat to peaty mud to sand (depending on site)	Abrupt	Abrupt			Sandy	"Fines upstream at site 7, indicating downstream source"				Mostly river sand	"Round gravel-sized mudstone clasts mixed with woody debris, probably of debris flow origin. Only found in upper reaches of Neawanna creek."	"Surged over spit at south end of Seaside, then down tidal channel (to north)"			"This layer is composed of mostly river sand, suggesting river flooding instead of a tsunami deposit. However,, at site 7, the coarse sand fines upstream, suggesting a downriver source"	"Darienzo et al., 1994"	Journal	1994	"Tillamook Head, OR"
"Neawanna Creek, OR"	99	34		45.9900	-123.9200	Salt and freshwater marshes	Marshes along tidal creek						21	6	5	y	6	5	0	1	1	1	at least 0.5 -1.0	480±60	462-634		Radiocarbon ages from Neawanna 2 from underlying peat layer							Peat		Abrupt									"Increase in beach sand component from underlying peat in one core (7), decrease in another(5)."					Necanicum River section discusses Neawanna Creek (a tributary of the Necanicum).  No paleotsunami deposits were found along the Necanicum River.	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Tillamook Head, OR"
"Neawanna Creek, OR"	100	34		45.9900	-123.9200	Salt and freshwater marshes	Marshes along tidal creek						21	6	5	y	6	5	0	2	2	2	at least 0.5 -1.0	800±60	670-903		Radiocarbon ages from Neawanna 2 from underlying peat layer							Peat		Abrupt									Increase in beach sand component from underlying peat in one core (5).					Necanicum River section discusses Neawanna Creek (a tributary of the Necanicum).  No paleotsunami deposits were found along the Necanicum River.	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Tillamook Head, OR"
"Neawanna Creek, OR"	101	34		45.9900	-123.9200	Salt and freshwater marshes	Marshes along tidal creek						21	6	5	y	6	5	0	3	3	3	at least 0.5 -1.0	1100±70	920-1170		Radiocarbon ages from Neawanna 2 from underlying peat layer							Peat		Abrupt									"Increase in beach sand component from underlying peat in two cores (2,5)."					Necanicum River section discusses Neawanna Creek (a tributary of the Necanicum).  No paleotsunami deposits were found along the Necanicum River.	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Tillamook Head, OR"
"Neawanna Creek, OR"	102	34		45.9900	-123.9200	Salt and freshwater marshes	Marshes along tidal creek						21	6	5	y	6	5	0	5	4	5	less than 1.0				Layer not dated							Peat		Abrupt									Increase in beach sand component from underlying peat in one core (5).					Necanicum River section discusses Neawanna Creek (a tributary of the Necanicum).  No paleotsunami deposits were found along the Necanicum River. Cosiesmic subsidence and tsunami deposition of this layer is questionable	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Tillamook Head, OR"
"Neawanna Creek, OR"	103	34		45.9900	-123.9200	Salt and freshwater marshes	Marshes along tidal creek						21	6	5	y	6	5	0	6	5	6	at least 0.5 -1.0	2000±70	1820-2139		Radiocarbon ages from Neawanna 2 from underlying peat layer							Peat		Abrupt									Increase in beach sand component from underlying peat in one core (2).			Increase in brackish/marine diatoms in core examined		Necanicum River section discusses Neawanna Creek (a tributary of the Necanicum).  No paleotsunami deposits were found along the Necanicum River.	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Tillamook Head, OR"
"Ecola Creek, OR"	104	35		45.9000	-123.9500	"Marsh, tidal"	Marshes along tidal creek							6	3	y	5	2	1	1	1	1		380±60	140-620		Radiocarbon							Muddy to sandy peat	Tidal flat mud	Abrupt	Abrupt			Sandy					>50% beach sand						"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Ecola Creek, OR"	105	35		45.9000	-123.9500	"Marsh, tidal"	Marshes along tidal creek							6	3	n	5	2	1	2	2													Tidal flat mud	 Peaty mud to sand	Abrupt				Sandy					>50% beach sand					Tsunami sand with no evidence for subsidence	"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Ecola Creek, OR"	106	35		45.9000	-123.9500	"Marsh, tidal"	Marshes along tidal creek							6	3	y	5	2	1	3	3	2		1270±60 	1030-1510		Radiocarbon							Muddy to sandy peat	Peat	Abrupt				Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Tillamook Head, OR"
"Ecola Creek, OR"	107	35		45.9000	-123.9500	"Marsh, tidal"	Marshes along tidal creek				6	cores and shallow pits		8	2+	y		1	1	1	1	1		380±60		1700	Radiocarbon							Peat	Tidal flat mud					Sand							Entered wetlands via Ecola Creek mouth and by overtopping Cannon beach spit.			Last two prehistoric tsunamis 10x larger than 1964 tsunami	"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Tillamook Head, OR"
"Ecola Creek, OR"	108	35		45.9000	-123.9500	"Marsh, tidal"	Marshes along tidal creek				6	Cores and shallow pits		8	2+	n		1	1	2	2			1200±60 			Radiocarbon				2-3 (bounds debris flow)			Peat	Peat					Sand							Entered wetlands via Ecola Creek mouth and by overtopping Cannon beach spit.			"Tsunami deposit bounds debris flow deposit - evidence for multiple wave trains. Last two prehistoric tsunamis 10X larger than 1964 tsunami. Tsunami deposit is located within a peat, indicating no subsidence."	"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Tillamook Head, OR"
"Ecola Creek, OR"	109	36		45.8900	-123.9600	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.					"Gouge cores, vibracores"		Up to 4	up to 4															Landward thining				Organic-rich mud and peat	Organic-rich mud and peat													Biogenic tracers	Geochemical tracers		Schlichting et al. 1999	Abstract	1999	"Tillamook Head, OR"
"Rockaway, OR"	110	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	200 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					1	1					1700		0.2-20						Soft organic-rich mud	"Organic-rich mud/muck, gelatinous, very loose."					Sand										"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	111	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	500 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					2	2			810±40 (940±40)	735-795    (840-975)	800 cybp		0.2-25						Soft organic-rich mud	Soft organic-rich mud															"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	112	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	400 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					3	3					1100 cybp		2.0-25						Peat (thin)	Soft organic-rich mud	Abrupt		2.0 - 1.5		Sand (mL)			Well sorted							"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	113	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	200 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					4	4					1300 cybp		5-10			2		Angling mud laminae	Soft organic-rich mud	Soft organic-rich mud	Abrupt	"Diffuse, interfingered"	2.0 -  1.5		Sand (mL)			Well sorted							"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	114	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	200 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					5	5					1700 cybp		2-4						"Organic-rich mud, dense"	Soft organic-rich mud					Sand										"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	115	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	200 from modern shoreline	Open coast			"Gouge cores, vibracores"	30	"Up to 6, possibly 7"	"Up to 6, possibly 7"					6	6				2300-2325	2500 cybp		2						Soft organic-rich mud	"Organic-rich mud, dense"					Sand										"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices. Prevalence of liquifaction features makes correlation of sand layerts between cores difficult."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Girabaldi, OR"
"Rockaway, OR"	116	37		45.6093	-123.9450	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	400	Open coast			"Gouge cores, vibracores"		Up to 4	Up to 4															Landward thining				Organic-rich mud and peat	Organic-rich mud and peat													Biogenic tracers	Geochemical tracers		Schlichting et al. 1999	abstract	1999	"Girabaldi, OR"
"Oyster Farm, Netarts Bay, OR"	117	38		45.4800	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.95		"Cutbank, gouge core"	1	10	4	y				1	1													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Oyster Farm, Netarts Bay, OR"	118	38		45.4800	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.95		"Cutbank, gouge core"	1	10	4	y				2	2													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Oyster Farm, Netarts Bay, OR"	119	38		45.4800	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.95		"Cutbank, gouge core"	1	10	4	y				6	3													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Oyster Farm, Netarts Bay, OR"	120	38		45.4800	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.95		"Cutbank, gouge core"	1	10	4	y				9	4													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Wee Willies, Netarts Bay, OR"	121	39		45.4100	-123.9300	"Marsh, tidal"	Marsh along landward side of bay					Cutbank		3	2	y	3	2	0	1	1	1				1700	Correlation with other deposits							Peat		Abrupt				Sand								Brackish water diatoms		Tsunami deposits are visible in cutbanks	"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR"
"Wee Willies, Netarts Bay, OR"	122	39		45.4100	-123.9300	"Marsh, tidal"	Marsh along landward side of bay					Cutbank		3	2	y	3	2	0	2	2	2		800±200			Correlation with other deposits							Peat		Abrupt				Sand								Brackish water diatoms		Tsunami deposits are visible in cutbanks	"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR"
"Wee Willies, Netarts Bay, OR"	123	39		45.4100	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.71		"Cutbank, gouge core"	2	5	3	y				1	1													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Wee Willies, Netarts Bay, OR"	124	39		45.4100	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.71		"Cutbank, gouge core"	2	5	3	y				2	2													Rooted mud		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Wee Willies, Netarts Bay, OR"	125	39		45.4100	-123.9300	"Marsh, tidal"	Marsh along landward side of bay			0.71		"Cutbank, gouge core"	2	5	3	y				5	3													Peat		Abrupt															Darienzo. 1991	Thesis (Ph.D.)	1991	"Netarts, OR"
"Netarts Marsh, OR"	126	40		45.3900	-123.9300	"Marsh, tidal"	marsh at south end of bay					"Cores, aluminum tins"	18+		0																																			"Concludes evidence for tsunami deposition at Netarts Bay is not convincing. Pollen and diatom data suggest coarse minerogenic layers overlying peat reflect changes in the hydrodynamics of the estuary, but the change was part of a longer term trend already underway."	"Shennan et al., 1998"	Journal	1998	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	127	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	1	1	1	1.0-1.5	370 ±60										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	128	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	2	2	2	1.0-1.5	660±60										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	129	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	4	3	4	1.0-1.5	1670±80										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	130	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	5	4	5	1.0-1.5	1840±60										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	131	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	9	5	9	1.0-1.5	3360±80										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	132	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay							10	6	y	10	6	0	10	6	10	1.0-1.5	3330±70										Peat	Tidal flat mud																"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	133	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	1	1	1		370 ±60	290-520		Radiocarbon dates from top of underlying peat																								"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	134	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	2	2	2	> 0.5 - 1.0	660±60	540-690		Radiocarbon dates from top of underlying peat																							This layer is not not well documented here but better documented at Wee Willies and Oyster Farm sites (see above)	"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	135	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	4	3	4		1670±80	1354-1769		Radiocarbon dates from top of underlying peat																								"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	136	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	5	4	5		1840±60	1540-1869		Radiocarbon dates from top of underlying peat																								"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	137	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	9	5	9		3360±80	3411-3829		Radiocarbon dates from top of underlying peat																								"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	138	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Vibracore, gouge cores"		10	6	y	10	6	0	10	6	10	1.0-1.5	3330±70	3399-3818		Radiocarbon dates from top of underlying peat																								"Darienzo, 1991"	Thesis (Ph.D.)	1991	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	139	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Pipe cores, gouge cores"	13+ pipe cores in 2 orthoganal transects with additional gouge cores.	7	4	y	7	4	0	1	1	1	1.3-1.5	370±60	290-520		Radiocarbon dates from top of underlying peat			No consistent change in thickness from west to east. Dramatic thickening and thinning from north to south.			"Very few, if any, intevening mud laminae. When present, mud laminae occur near top of layer."	Peaty muddy sand	Muddy sand to sandy mud to mud	Abrupt	Abrupt							Absence of crossbedding		"Large plant fragments, peat clumps, and/or mud rip-up clasts are rare or absent from sand layers."		Brackish diatoms		"Stratigraphic colums and discussion show 7 burial events, 4 of which are capped by tsunami deposits. The conclusions state there are 6 burial events, 5 of which are capped by tsunami deposits. The figures included in the database are from the stratigraphic data presented, not the conclusions."	"Darienzo and Peterson, 1990"	Journal	1990	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	140	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Pipe cores, gouge cores"	13+ pipe cores in 2 orthoganal transects with additional gouge cores.	7	4	y	7	4	0	3	2	3	0.9-1.1	1430±80	1189-1520		"Radiocarbon on underlying peats. The top of Buried Marsh 3 has an older date than the bottom of Buried Marsh 3. Therefore, the bottom of Buried Marsh 3  represents the maximum age for this deposit."			No consistent change in thickness from west to east. Dramatic thickening and thinning from north to south.			Distinct sand and mud layers from1 mm to several cm.	Peaty sandy mud to peaty muddy sand	Sandy mud	Abrupt	Abrupt							Absence of crossbedding		"Large plant fragments, peat clumps, and/or mud rip-up clasts are rare or absent from sand layers."		Brackish diatoms		"Stratigraphic colums and discussion show 7 burial events, 4 of which are capped by tsunami deposits. The conclusions state there are 6 burial events, 5 of which are capped by tsunami deposits. The figures included in the database are from the stratigraphic data presented, not the conclusions."	"Darienzo and Peterson, 1990"	Journal	1990	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	141	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Pipe cores, gouge cores"	13+ pipe cores in 2 orthoganal transects with additional gouge cores.	7	4	y	7	4	0	4	3	4	1.3-1.5	1840±60	1540-1869		Radiocarbon on underlying peats.			Dramatic thickening and thinning from north to south.			"Very few, if any, intevening mud laminae. When present, mud laminae occur near top of layer."	Peaty sandy mud to peaty muddy sand	Mud to sandy mud to peaty sandy mud	Abrupt	Abrupt							Absence of crossbedding		"Abundant organic detritus at 2 sites nearest the spit. Large plant fragments, peat clumps, and/or mud rip-up clasts are rare or absent from sand layers."		Brackish diatoms		"Stratigraphic colums and discussion show 7 burial events, 4 of which are capped by tsunami deposits. The conclusions state there are 6 burial events, 5 of which are capped by tsunami deposits. The figures included in the database are from the stratigraphic data presented, not the conclusions."	"Darienzo and Peterson, 1990"	Journal	1990	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	142	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					"Pipe cores, gouge cores"	13+ pipe cores in 2 orthoganal transects with additional gouge cores.	7	4	y	7	4	0	7	4	7	0.9-1.1	3300±100	3274-3827		Radiocarbon on underlying peats.						"Very few, if any, intevening mud laminae. When present, mud laminae occur near top of layer."	Peaty mud	Mud	Abrupt	Abrupt							Absence of crossbedding		"Large plant fragments, peat clumps, and/or mud rip-up clasts are rare or absent from sand layers."				"Stratigraphic colums and discussion show 7 burial events, 4 of which are capped by tsunami deposits. The conclusions state there are 6 burial events, 5 of which are capped by tsunami deposits. The figures included in the database are from the stratigraphic data presented, not the conclusions."	"Darienzo and Peterson, 1990"	Journal	1990	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	143	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					Continuous cores and 1 meter interval cores	"9+  in 2 orthoganal transects with additional gouge cores, outcrops."	7	4	y	7	4	0	1	1	1		370±60	290-520		Radiocarbon on underlying peats.			"Varies in thickness from core to core, but can be traced across full extent of marsh"				Peat	Tidal flat mud	Abrupt	Abrupt			Sand-rich											"Peterson and Darienzo, 1988"	"Journal, field trip guide"	1988	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	144	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					Continuous cores and 1 meter interval cores	"9+  in 2 orthoganal transects with additional gouge cores, outcrops."	7	4	y	7	4	0	3	2	3		1430±80	1189-1520		"Radiocarbon on underlying peats. The top of Buried Marsh 3 has an older date than the bottom of Buried Marsh 3. Therefore, the bottom of Buried Marsh 3  represents the maximum age for this deposit."			"Varies in thickness from core to core, but can be traced across full extent of marsh"				Peat	Tidal flat mud	Abrupt	Abrupt			Sand-rich											"Peterson and Darienzo, 1988"	"Journal, field trip guide"	1988	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	145	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					Continuous cores and 1 meter interval cores	"9+  in 2 orthoganal transects with additional gouge cores, outcrops."	7	4	y	7	4	0	4	3	4		1840±60	1540-1869		Radiocarbon on underlying peats.			"Varies in thickness from core to core, but can be traced across full extent of marsh"				Peat	Tidal flat mud	Abrupt	Abrupt			sand-rich											"Peterson and Darienzo, 1988"	"Journal, field trip guide"	1988	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	146	40		45.3900	-123.9300	"Marsh, tidal"	Marsh at south end of bay					Continuous cores and 1 meter interval cores	"9+  in 2 orthoganal transects with additional gouge cores, outcrops."	7	4	y	7	4	0	7	4	7		3300±100	3274-3827		Radiocarbon on underlying peats.			"Varies in thickness from core to core, but can be traced across full extent of marsh"				Peat	Tidal flat mud	Abrupt	Abrupt			sand-rich											"Peterson and Darienzo, 1988"	"Journal, field trip guide"	1988	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	147	40		45.3700	-123.9700	"Marsh, tidal"	Marsh at south end of bay							6	5	y	5	4	1	1	1	1		370 ±60	130 - 610          (0 - 578)		Radiocarbon							Peat	Tidal flat mud	Abrupt	Abrupt			Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	148	40		45.3700	-123.9700	"Marsh, tidal"	Marsh at south end of bay							6	5	n	5	4	1	2	2			660±60	420 - 900		"Radiocarbon, from oyster farm locality"							Tidal flat mud	Peat	Gradual	Gradual			Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	149	40		45.3700	-123.9700	"Marsh, tidal"	Marsh at south end of bay							6	5	y	5	4	1	4	3	3		1670±80	1350 - 1990		Radiocarbon							Peaty mud to sand	Tidal flat mud	Abrupt	Abrupt			Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	150	40		45.3700	-123.9700	"Marsh, tidal"	Marsh at south end of bay							6	5	y	5	4	1	5	4	4		1840±60	1600-2080      (1490-2030)		Radiocarbon							Peat	Tidal flat mud	Abrupt	Abrupt			Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Netarts, OR; Sand Lake, OR"
"Netarts Marsh, OR"	151	40		45.3700	-123.9700	"Marsh, tidal"	Marsh at south end of bay							6	5	y	5	4	1	6	5	5		2600±70	2320-2880     (2360-3050)		Radiocarbon							Peat	Tidal flat mud	Abrupt				Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Netarts, OR; Sand Lake, OR"
"Nestucca Bay, OR"	152	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							6	3	y	6	3	0	1	1	1		400±60	160-640        (0-620)		"Radiocarbon, from Nestucca DucK location"							Muddy to sandy peat	Peaty mud to sand	Abrupt															"Darienzo and Peterson, 1995"	Journal	1995	"Nestucca Bay, OR"
"Nestucca Bay, OR"	153	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							6	3	y	6	3	0	2	2	2		1510±90	1150-1870		"Radiocarbon, from Little Nestucca 5"							Muddy to sandy peat	Peaty mud to sand	Abrupt															"Darienzo and Peterson, 1995"	Journal	1995	"Nestucca Bay, OR"
"Nestucca Bay, OR"	154	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							6	3	y	6	3	0	3	3	3		1460±70	1180-1740		"Radiocarbon, from Little Nestucca 5"							Muddy to sandy peat	Peaty mud to sand	Abrupt															"Darienzo and Peterson, 1995"	Journal	1995	"Nestucca Bay, OR"
"Nestucca Bay, OR"	155	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	1	1	1	1-1.5	400±60										Muddy to sandy peat	Peaty mud to sand	Abrupt				Sandy					Greater and/or coarser beach sand component than underlying peaty layers.			Increase or first appearance of brackish marine diatoms		This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	156	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	2	2	2	1-1.5	1510±90										Muddy to sandy peat	Peaty mud to sand	Abrupt				Sandy										This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	157	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	3	3	3	1-1.5	1460±70										Muddy to sandy peat	Peaty mud to sand	Abrupt				Sandy					Greater and/or coarser beach sand component than underlying peaty layers.					This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	158	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	4	4	4	1-1.5											Peaty mud to sand	Peaty mud to sand	Abrupt				Sandy					Greater and/or coarser beach sand component than underlying peaty layers.					This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	159	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	5	5	5	1-1.5	1860±70										Muddy to sandy peat	Peaty mud to sand	Abrupt				Sandy					Greater and/or coarser beach sand component than underlying peaty layers.			Increase or first appearance of brackish marine diatoms		This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	160	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."		12 (only top 6 analyzed)	6 (top 6 events contain a distinct sandy layer)	y	12 (only top 6 analyzed)	6	0	6	6	6	1-1.5	2560±70										Muddy to sandy peat	Slightly peaty mud to sand	Abrupt				Sandy					Greater and/or coarser beach sand component than underlying peaty layers.					This site record 12 events (subsidence with or without tsunami) in 5700 radiocarbon years.	"Darienzo et al., 1994"	Journal	1994	"Nestucca Bay, OR"
"Nestucca Bay, OR"	161	41		45.1900	-123.9500	"Marsh, tidal"	Marshes along bay					"2.5 cm gouge corer, 5-7.5 cm pipe corer, truck-mounted hollow stem auger."	16	12	1+	y	12	1	0	1	1	1				1700								Peat						Sands										Strongest evidence is for the 1700 tsunami at Netuscca Duck site. Thin tsunami layers are found upriver at Hurliman and Little Nestucca sites.	"Peterson et al., 1993"	"Journal, field trip guide"	1993	"Nestucca Bay, OR"
"Nestucca Bay, OR"	162	41	"Nestucca Duck, Nestucca 1, Little Nestucca 2"	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	1	1	1												Peat		Abrupt				Muddy sand										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Nestucca Bay, OR"	163	41	Little Nestucca 5	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	2	2	2		1510±90	1280-1600		"Radiocarbon dates from Little Nestucca 5, taken from top of underlying buried peat"						sandy mud laminae	Peat		Abrupt				Sandy mud										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Nestucca Bay, OR"	164	41	"Little Nestucca 5, Nestucca 2"	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	3	3	3		1460±70	1280-1520		"Radiocarbon dates from Little Nestucca 5, taken from top of underlying buried peat"						muddy sand laminae	Peat		Abrupt				Muddy sand										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Nestucca Bay, OR"	165	41	Nestucca 1	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	5	4	5												Peat		Abrupt				Muddy sand										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Nestucca Bay, OR"	166	41	"Little Nestucca  4, Nestucca 2"	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	7	5	7											sandy mud laminae	Peat		Abrupt				Sandy mud										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Nestucca Bay, OR"	167	41	"Little Nestucca  4, Little Nestucca 5, Nestucca 2"	45.1900	-123.9500	"Marsh, tidal"	Marshes along bay							12	6	y	12	6	0	8	6	8		3260±80	3349-3689		"Radiocarbon dates from Little Nestucca 5, taken from top of underlying buried peat"							Peat		Abrupt				Muddy sand										Tsunami deposits were not common and are confined to cores along the Little Nestucca River and across the wide part of Nestucca Spit at Nestucca Duck	"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Nestucca Bay, OR"
"Neskowin, OR"	168	42		45.1200	-123.9800	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	300 m from modern shoreline.	Open coast				43	3	3					1	1					1700	Peat abovethis layer dated as modern	0.2-15																						"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Neskowin, OR"
"Neskowin, OR"	169	42		45.1200	-123.9800	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	"600 m from modern shoreline for north marsh, 1000 m for central marsh."	Open coast				43	3	3					2	2					800 cybp		0.2-20																						"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Neskowin, OR"
"Neskowin, OR"	170	42		45.1200	-123.9800	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	"600 m from modern shoreline for north marsh, 1000 m for central marsh."	Open coast				43	3	3					3	3				920-1290	1100 cybp		0.2-8										2.08-2.17		Upper fraction mean: 2.08Êphi; STD=0.27 phi                        Lower fraction mean:        2.17 phi; STD = 0.255	Landward fining cannot be discerned from grain-size analysis	Fining upwards 								"Detailed core logs and analyses without interpretations are presented in thesis. Data included in this database based on authors interpretations in body of thesis, not core logs or analysies in appendices."	"Schlichting, 2000"	Thesis (M.S.)	2000	"Neskowin, OR"
"Neskowin, OR"	171	42		45.1200	-123.9800	Back-barrier wetlands	0pen coastal plain with back-barrier wetlands.	200	Open coast		3	Gouge and vibracores		Up to 4	Up to 4																									Sand											Schlichting et al. 1999	Abstract	1999	"Neskowin, OR"
"Salmon River, OR"	172	43		45.0300	-123.9900	Marsh						Cutbanks and cores		Up to 4	1 (only top soil extensively studied)	y				1	1	1	0.5	246±25			Nine samples taken from buried soil	up to10		Thins upriver and towards the uplands.			Lacks lamination	"Soil, archaeological remains"	Tideflat deposits			3.0-1.0		Fine to medium sand											"Minor and Grant, 1996"	Journal	1996	"Neskowin, OR"
"Salmon River, OR"	173	43		45.0300	-123.9900	Marsh																				1700								Topsoil	Tidal mud					Sand										Report contains color photograph of tsunami deposit which covers remains of Native American fishing camp.	"Atwater et al., 1999"	USGS Circular	1999	"Neskowin, OR"
"Salmon River, OR"	174	43		45.0300	-123.9900	Marsh								1	1	y	1	1	0	1	1	1						0-5		"Thins upvalley and away from river, thickest behind banks that face upriver."				Peat	Silt and very fine sandy silt	Sharp	Sharp	3.0-1.0		Fine to medium sand							Landward directed (seaward source)				"Grant and McLaren, 1987"	Abstract	1987	"Neskowin, OR"
"Silitz Bay, OR"	175	44	Salishan Spit	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"		6	5	y	6	5	0	1	1	1		270±60	30-510         (0-520)		Radiocarbon 							Peaty mud to sand (marsh deposit)	Slightly peaty mud to sand (marsh deposit)	Abrupt	Abrupt			Sand										"Thickness and depth data are measured from a composite column of two or more columns from Darienzo, 1991 and Darienzo and Peterson, 1994. Data about contacts and over- and underlying material also taken from this column."	"Darienzo and Peterson, 1995"	Journal	1995	"Lincoln City, OR"
"Silitz Bay, OR"	176	44	Salishan Spit	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"		6	5	Possible weak subsidence evidence at a few sites	6	5	0	2	2	2		350±60	110-590 		Radiocarbon 							Slightly peaty mud to sand (marsh deposit)	Slightly peaty mud to sand (marsh deposit)	Abrupt				Sand										"Thickness and depth data are measured from a composite column of two or more columns from Darienzo, 1991 and Darienzo and Peterson, 1994. Data about contacts and over- and underlying material also taken from this column."	"Darienzo and Peterson, 1995"	Journal	1995	"Lincoln City, OR"
"Silitz Bay, OR"	177	44	Salishan Spit	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"		6	5	y	6	5	0	4	3	3		1510±90	1150-1870		Radiocarbon 							Slightly peaty mud to sand (marsh deposit)	Mud (tidal flat deposit)	Abrupt	Abrupt			Sand										"Thickness and depth data are measured from a composite column of two or more columns from Darienzo, 1991 and Darienzo and Peterson, 1994. Data about contacts and over- and underlying material also taken from this column."	"Darienzo and Peterson, 1995"	Journal	1995	"Lincoln City, OR"
"Silitz Bay, OR"	178	44	Salishan Spit	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"		6	5	y	6	5	0	5	4	4		1690±70	1410-1970 (1310-1900)		Radiocarbon 							Peaty mud to sand (marsh deposit)	Mud (tidal flat deposit)	Abrupt	Abrupt			Sand										"Thickness and depth data are measured from a composite column of two or more columns from Darienzo, 1991 and Darienzo and Peterson, 1994. Data about contacts and over- and underlying material also taken from this column."	"Darienzo and Peterson, 1995"	Journal	1995	"Lincoln City, OR"
"Silitz Bay, OR"	179	44	Salishan Spit	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"		6	5	y	6	5	0	6	5	5		2550±80	2230-2870 (2200-2970)		Radiocarbon 							Rooted mud to sand (marsh deposit)	Slightly peaty mud to sand (marsh deposit)	Abrupt				Sand										"Thickness and depth data are measured from a composite column of two or more columns from Darienzo, 1991 and Darienzo and Peterson, 1994. Data about contacts and over- and underlying material also taken from this column."	"Darienzo and Peterson, 1995"	Journal	1995	"Lincoln City, OR"
"Silitz Bay, OR"	180	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"				y				1	1		0.5 - 1 	270±60			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied. Tsunami events other than 1 and 4 were either too small to measure ornot present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	181	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"				y				4	4		0.5 - 1 	1510±90			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied. Tsunami events other than 1 and 4 were either too small to measure ornot present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	182	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	1	1	1	0.5 - 1 	270±60			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand		-	-		Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	183	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	2	2	2	0.5 - 1 	350±60			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	184	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	3	3	3	0.5 - 1 				Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied. Tsunami event 3 does not appear in column for this site, and may not be present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	185	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	4	4	4	0.5 - 1 	1510±90			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	186	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	5	5	5	0.5 - 1 	1690±70			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	187	44	"Salishan Spit, Salishan House"	44.8992	-124.0083	Marsh	Marsh on bay side of spit	150	Open coast (from shoreward side of spit)			"2.5 cm gouge corer, outcrops"		6	6	y	6	6	0	6	6	6	0.5 - 1 	2550±80			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand					Beach sand	Triglochin rhyzomes	"Sand transport landward by marine surges, overtopped spit"			"Located on eastern side of Salishan Spit, not exposed to open ocean. When not specifically refered to, I assumed general comments for salishan Spit sites applied. Tsunami event 6 does not appear in column for this site, and may not be present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	188	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	1	1	1	0.5 - 1 	480±60			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand										"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. Event 1 not present or too small to measure on columns from Millport Slough and may not be present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	189	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	2	2	2	0.5 - 1 	350±60			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand										"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. Event 2 not present or too small to measure on columns from Millport Slough and may not be present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	190	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	3	3	3	0.5 - 1 	1330±70			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt				Sand										"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. Event 3 not present or too small to measure on columns from Millport Slough and may not be present at this site."	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	191	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	4	4	4	0.5 - 1 	1630±70			Radiocarbon 							Mud	Mud	Abrupt or gradual	Abrupt or gradual			Sand						Triglochin rhyzomes present at Alder site (closest site to Siletz Bay)				"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. "	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	192	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	5	5	5	0.5 - 1 	1850±70			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt	Abrupt			Sand						Triglochin rhyzomes present at Millpoprt 1 site 				"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. "	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	193	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	6	y	7	7	0	6	6	6	0.5 - 1 				Radiocarbon 							mud	Mud	Abrupt				Sand										"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. "	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	194	44	Millport Slough (Siletz River)	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore			"2.5 cm gouge corer, outcrops"		7	7	y	7	7	0	7	7	7	0.5 - 1 	2880±90			Radiocarbon 							Peat	Rooted to slightly peaty muds	Abrupt	Abrupt			Sand						Triglochin rhyzomes present at Millpoprt 1 site 				"Located at the southeastern corner of Siletz Bay, not exposed to open ocean. "	" Darienzo et al., 1994"	Journal	1994	"Lincoln City, OR"
"Silitz Bay, OR"	195	44	Salishan Spit	44.8992	-124.0083	Marsh	River/slough at south end of bay	150	Open coast (from shoreward side of spit)		6			6	6	y		6	0															Peat						Sand					Beach sand		Tsunami overtopped spit			"Tsunami deposits, located on the bay side of Salishan spit, are derived directly from the beach and are an example of spit overtopping. Tsunami deposits and buried peats are particularly well developed at this site."	"Peterson et al., 1993"	"Journal, field guide"	1993	"Lincoln City, OR"
"Silitz Bay, OR"	196	44	Millport Slough	44.8992	-124.0083	Marsh	River/slough at south end of bay	1250	Up river - bayshore					7	3	y				"4,5,7"	"1,2,3"							thin		Discontinuous				Peat						Sand											"Peterson et al., 1993"	"Journal, field guide"	1993	"Lincoln City, OR"
"Silitz Bay, OR"	197	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			1	1			270±60	0-480		"Radiocarbon dates from Salishan House, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Silitz Bay, OR"	198	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			2	2			350±60	290-520		"Radiocarbon dates from Salishan House, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Silitz Bay, OR"	199	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			3	3						Not dated at Salishan House							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Silitz Bay, OR"	200	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			4	4			1510±90	1280-1600		"Radiocarbon dates from Salishan House, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Silitz Bay, OR"	201	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			5	5			1690±70	1410-1805		"Radiocarbon dates from Salishan House, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Silitz Bay, OR"	202	44		44.8992	-124.0083	Marsh	Marsh on bay side of spit and across bay in slough.					"Cores, vibracores, cutbanks"	15	7	6	y	7			6	6			2550±80	2359-2789		"Radiocarbon dates from Salishan House, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Neskowin, OR"
"Yaquina, OR"	203	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)					7	5	y	7	5	0	1 (0')	1	1		160±60	0-400		"Radiocarbon, Hatfield site"																							" Events are parentheticallylisted 0'-6 to correspond to notation used in the paper.  This designation is tentative. Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Tsunami deposits are too small to measure or do not appear in representative column, but are discussed in text."	"Darienzo and Peterson, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	204	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)					7	5	y	7	5	0	2 (1)	2	2		550±70	270-830   (310-720)		"Radiocarbon, Outcrop B"																							" Events are parentheticallylisted 0'-6 to correspond to notation used in the paper.  This designation is tentative. Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Tsunami deposits are too small to measure or do not appear in representative column, but are discussed in text."	"Darienzo and Peterson, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	205	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)					7	5	y	7	5	0	3 (2)	3	3					No date available for this event																							" Events are parentheticallylisted 0'-6 to correspond to notation used in the paper.  This designation is tentative. Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Tsunami deposits are too small to measure or do not appear in representative column, but are discussed in text."	"Darienzo and Peterson, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	206	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)					7	5	y	7	5	0	4 (3)	4	4		1350±60	1110-1590		"Radiocarbon, Slack 1"																							" Events are parentheticallylisted 0'-6 to correspond to notation used in the paper.  This designation is tentative. Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Tsunami deposits are too small to measure or do not appear in representative column, but are discussed in text."	"Darienzo and Peterson, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	207	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)					7	5	y	7	5	0	5 (4)	5	5		1680±70	1400-1960		"Radiocarbon, Slack 1"																							" Events are parentheticallylisted 0'-6 to correspond to notation used in the paper.  This designation is tentative. Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Tsunami deposits are too small to measure or do not appear in representative column, but are discussed in text."	"Darienzo and Peterson, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	208	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	14000	Up river			"shallow (1-2 m) gouge cores, cutbanks"	14	4	3	y	4	3	0	1	1	1	0-0.5			1700	"Correlated to events in Peterson et al., 1993, Darienzo et al., 1994"	2-10																						"Preliminary reconnaissance, only shallow (1-2 m)  records were examined"	"Peterson and Priest, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	209	45		44.6100	-124.0400	Marsh	River/estuary/ small bay					shallow (1-2 m) gouge cores	14	4	3	y	4	3	0	2	2	2	<1			800 cybp	"Correlated to events in Peterson et al., 1993, Darienzo et al., 1994"	2-10																						"Preliminary reconnaissance, only shallow (1-2 m)  records were examined"	"Peterson and Priest, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	210	45		44.6100	-124.0400	Marsh	River/estuary/ small bay					shallow (1-2 m) gouge cores	14	4	3	y	4	3	0	4	3	4	<1			1400 cybp	"Correlated to events in Peterson et al., 1993, Darienzo et al., 1994"	2-10																						"Preliminary reconnaissance, only shallow (1-2 m)  records were examined"	"Peterson and Priest, 1995"	Journal	1995	"Newport South, OR"
"Yaquina, OR"	211	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"	26	7	2	y	7	2	0	1 (0')	1	1	0.5	160±60			Radiocarbon	10						Peat	Mud	Abrupt												Increase in marine and brackish diatoms		"Evidence for tsunami deposits associated with coseismic subsidence limited to westernmost core site near bay mouth (Hatfield). Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Events are parentheticallylisted 0'-6 to correspond to notation used in paper, with tsunami sands indicated for events 0' and 1. Table 2 lists distinct sand layers for events 3 and 5, but these are not discussed as tsunami deposits, nor do they show up in the columns. Distinct sandy horizons are mentioned for Oysterville sites, but these also do not show up in column. Subsidence data is for Oysterville site for events 1-3, while events 4-6 likely subsided less than 0.5 m. Hatfield, near the zero isobar, likely subsided 0.5 m or less. Dates for event 1 in representative Yaquina column and Hatfield 2 core do not agree."	"Darienzo et al., 1994"	Journal	1994	"Newport South, OR"
"Yaquina, OR"	212	45		44.6100	-124.0400	Marsh	River/estuary/ small bay	1500	River mouth (mouth of bay/estuary)			"2.5 cm gouge corer, 5-7.5 cm pipe corer, outcrops"	26	7	2	y	7	2	0	2 (1)	2	2	0.5	550 ±70 (1270±70)			Radiocarbon - parenthetical date is from Hatfield core	15						Peat	Rooted mud to sand	Abrupt												Increase in marine and brackish diatoms		"Evidence for tsunami deposits associated with coseismic subsidence limited to westernmost core site near bay mouth (Hatfield). Inland site (Slack 1) shows evidence for sand sheet associated with event 6, but tsunami origin not conclusive. Events are parentheticallylisted 0'-6 to correspond to notation used in paper, with tsunami sands indicated for events 0' and 1. Table 2 lists distinct sand layers for events 3 and 5, but these are not discussed as tsunami deposits, nor do they show up in the columns. Distinct sandy horizons are mentioned for Oysterville sites, but these also do not show up in column. Subsidence data is for Oysterville site for events 1-3, while events 4-6 likely subsided less than 0.5 m. Hatfield, near the zero isobar, likely subsided 0.5 m or less. Dates for event 1 in representative Yaquina column and Hatfield 2 core do not agree."	"Darienzo et al., 1994"	Journal	1994	"Newport South, OR"
"Yaquina, OR"	213	45	Hatfield	44.6100	-124.0400	Marsh	River/estuary/ small bay						25	12	5					1	1						Not dated							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Yaquina, OR"	214	45	Hatfield	44.6100	-124.0400	Marsh	River/estuary/ small bay						25	12	5					3	2						Not dated							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Yaquina, OR"	215	45	Slack	44.6100	-124.0400	Marsh	River/estuary/ small bay						25	12	5					9	3			3260±90	3277-3699		"Radiocarbon dates from Slack 1 site, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Yaquina, OR"	216	45	Slack	44.6100	-124.0400	Marsh	River/estuary/ small bay						25	12	5					10	4			3170±70	3259-2569		"Radiocarbon dates from Slack 1 site, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Yaquina, OR"	217	45	Slack	44.6100	-124.0400	Marsh	River/estuary/ small bay						25	12	5					12	5			3840±70	3996-4504		"Radiocarbon dates from Slack 1 site, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Alsea Bay, OR"	218	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay	>1500	Up river			"Continuous pipe cores, gouge cores, outcrop"	21	6	5+	y	6	5	0	1	1	1	0.5	480±60	474-645	1700	Radiocarbon from underlying peatlayer	<1 - 25		"Thins landward (NW bay marsh to E confluence of north channel), locally thick, asociated with low marsh surfaces, also decreases in thickness away from north channel axis."			faint internal layering at some sites	Peat	Peaty to slightly peaty muds	Sharp	Abrupt to gradual		"76.9% sand, 23.1% silt and mud"	Sandy				Lacks structures	Up to 21% beach sand		"Flowed through bay mouth, then due east to NE bay margin, then up north channel, rapidly diminishing in flow energy"				"Peterson and Darienzo, 1996"	USGS Professional Paper	1996	"Waldport, OR"
"Alsea Bay, OR"	219	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay	>1500	Up river			"Continuous pipe cores, gouge cores, outcrop"	21	6	5+	y	6	5	0	2	2	2	0.5-1.0	800±80	561-903		Radiocarbon from underlying peatlayer	<1 - 25		"Thins landward (NW bay marsh to E confluence of north channel), locally thick, asociated with low marsh surfaces, also decreases in thickness away from north channel axis."			faint internal layering at some sites	Peat	Peaty to slightly peaty muds	Sharp	Abrupt to gradual		"88.5% sand, 11.5% silt and mud"	Sandy				Lacks structures	Up to 47% beach sand		"Flowed through bay mouth, then due east to NE bay margin, then up north channel, rapidly diminishing in flow energy"				"Peterson and Darienzo, 1996"	USGS Professional Paper	1996	"Waldport, OR"
"Alsea Bay, OR"	220	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay	>1500	Up river			"Continuous pipe cores, gouge cores, outcrop"	21	6	5+	y	6	5	0	3	3	3	0.5-1.0					<1 - 25		"Thins landward (NW bay marsh to E confluence of north channel), locally thick, asociated with low marsh surfaces, also decreases in thickness away from north channel axis."			faint internal layering at some sites	Peat	Peaty to slightly peaty muds	Sharp	Abrupt to gradual		"58.1% sand, 41.9% silt and mud"	Sandy				Lacks structures			"Flowed through bay mouth, then due east to NE bay margin, then up north channel, rapidly diminishing in flow energy"				"Peterson and Darienzo, 1996"	USGS Professional Paper	1996	"Waldport, OR"
"Alsea Bay, OR"	221	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay	>1500	Up river			"Continuous pipe cores, gouge cores, outcrop"	21	6	5+	y	6	5	0	4	4	4	0.5-1.0	1490±80	1260-1530		"Radiocarbon from buried peatlayer, represents greatest possible age for tsunami"	<1 - 25		"Thins landward (NW bay marsh to E confluence of north channel), locally thick, asociated with low marsh surfaces, also decreases in thickness away from north channel axis."			faint internal layering at some sites	Peat	Peaty to slightly peaty muds	Sharp	Abrupt to gradual			Sandy				Lacks structures	Up to 27% beach sand		"Flowed through bay mouth, then due east to NE bay margin, then up north channel, rapidly diminishing in flow energy"				"Peterson and Darienzo, 1996"	USGS Professional Paper	1996	"Waldport, OR"
"Alsea Bay, OR"	222	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay	>1500	Up river			"Continuous pipe cores, gouge cores, outcrop"	21	6	5+	y	6	5	0	5	5	5	0.15	2210±80	1999-2349		"Radiocarbon from buried peatlayer, represents greatest possible age for tsunami"	<1 - 25		"Thins landward (NW bay marsh to E confluence of north channel), locally thick, asociated with low marsh surfaces, also decreases in thickness away from north channel axis."			faint internal layering at some sites	Peat	Peaty to slightly peaty muds	Sharp	Abrupt to gradual		"81.8% sand, 18.2% silt and mud"	Sandy				Lacks structures			"Flowed through bay mouth, then due east to NE bay margin, then up north channel, rapidly diminishing in flow energy"				"Peterson and Darienzo, 1996"	USGS Professional Paper	1996	"Waldport, OR"
"Alsea Bay, OR"	223	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay							6	3	y	6	3	0	1	1	1		480±60	240-720      (300-680)			laminae						Peat	Peat	Abrupt				Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Waldport, OR"
"Alsea Bay, OR"	224	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay							6	3	y	6	3	0	2	2	2		800±80	480-1120			2						Peat	Peat	Abrupt				Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Waldport, OR"
"Alsea Bay, OR"	225	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay							6	3	y	6	3	0	4	3	4		1490±80	1170-1810			5						Peat	Mud	Abrupt				Sandy											"Darienzo and Peterson, 1995"	Journal	1995	"Waldport, OR"
"Alsea Bay, OR"	226	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay					"Cores, vibracores"	19	11	4	y	11	4	7	2	1	2		480±60	474-645		"Radiocarbon dates based on corellation with AB9, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Alsea Bay, OR"	227	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay					"Cores, vibracores"	19	11	4	y	11	4	7	3	2	3		800±80	561-903		"Radiocarbon dates based on corellation with AB9, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Alsea Bay, OR"	228	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay					"Cores, vibracores"	19	11	4	y	11	4	7	5	3	5		1490±80	1260-1530		"Radiocarbon dates based on corellation with AB9, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Alsea Bay, OR"	229	46		44.4200	-124.0200	" Marsh, tidal"	River/estuary/ small bay					"Cores, vibracores"	19	11	4	y	11	4	7	6	4	6		2210±80	1999-2349		"Radiocarbon dates based on corellation with AB9, taken from top of underlying peat"							Peat		Abrupt															"Darienzo, 1991 "	Thesis (Ph.D.)	1991	"Newport South, OR"
"Lily lake, OR"	230	47		44.0900	-124.1200	" Marsh, tidal"	Coastal lake	300	Open coast																			1-5																						"Abstract mentions tsunami deposits at this site. Briggs, 1994, lists 2 pebble layers in peat from cores at this site, but attributes them to debris flows, not tsunamis."	"Briggs and Peterson, 1992"	Abstract	1992	"Florence, OR"
"Suislaw Bay, OR"	231	48	Deming Creek	43.9975	-124.1100	" Marsh, tidal"	River/estuary/ small bay	6500	Open coast			Gouge cores and vibracores	25	5	1	y	5	1	0		1													Muddy peat	Muddy peat	Sharp	Sharp	3.0 - 1.0		Medium to fine											"Briggs, 1994"	Thesis (M.S.)	1994	"Florence, OR"
"Umpqua River, OR"	232	49		43.7000	-124.1000	Marsh	River/estuary					Gouge cores and vibracores	38 (14 contain candidate tsunami layers)	4	3	y	4	3	0	1	1			1040±60			Radiocarbon date taken from peat 2 cm below tsunami deposit	2.0		Landward thinning				Peat	peat	Sharp	Sharp			Sand										"Tsunami deposits described are termed candidate tsunami deposits. Coseismic subsidence is noted for each tsunami event, but not necessarily where evidence for tsunami is strongest."	"Briggs, 1994"	Thesis (M.S.)	1994	Reedsport. OR
"Umpqua River, OR"	233	49		43.7000	-124.1000	Marsh	River/estuary					Gouge cores and vibracores	38 (14 contain candidate tsunami layers)	4	3	y	4	3	0		2			1630±60			Radiocarbon date taken on wood from detrital layer below tsunami deposit	7.0		Landward thinning				Detrital layer grading into peat	Slightly sandy peaty mud	Sharp	Sharp			Sand										"Tsunami deposits described are termed candidate tsunami deposits. Coseismic subsidence is noted for each tsunami event, but not necessarily where evidence for tsunami is strongest."	"Briggs, 1994"	Thesis (M.S.)	1994	Reedsport. OR
"Umpqua River, OR"	234	49		43.7000	-124.1000	Marsh	River/estuary					Gouge cores and vibracores	38 (14 contain candidate tsunami layers)	4	3	y	4	3	0		3									Landward thinning				Peat	Peat	Sharp	Gradual to sharp			Sand										"Tsunami deposits described are termed candidate tsunami deposits. Coseismic subsidence is noted for each tsunami event, but due to location of the zero isobase, not necessarily where evidence for tsunami is strongest."	"Briggs, 1994"	Thesis (M.S.)	1994	Reedsport. OR
"Coos Bay, OR"	234	50	Stone Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0											Peat	Mud	Sharp				Muddy sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	235	50	Stone Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	2	2	2	1					as much as 10						Peat	Mud	"Sharp, possibly erosional"				Clean to muddy sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	235	50	Hidden Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0					1-3						Peat	Mud	Sharp		3.0-2.0		Fine sand and sandy mud											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	236	50	Hidden Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	2	2	2	1	2082±90    2580±60	1732-2343    2360-2845		Radiocarbon on herbaceous stems. Second date on abraded decayed stem.	1-8						Peat	Mud	Sharp				Sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	236	50	North Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0											Peat	Mud	Sharp				Sand and sandy mud											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	237	50	North Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	2	2	2	1											Peat	Mud	Sharp				Sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	237	50	Day  Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0											Peat	Mud	Sharp				Sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	238	50	Day  Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	2	2	2	1					5						Peat	Mud	Sharp				Sand with fine round pebbles											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	238	50	Hayward Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0					1-8		Thickens towards forest				"Peat, muddy peat, and peaty mud"	Mud	Abrupt and planar		3.0-2.0		Clean fine sand	Less muddy toward forest										"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	239	50	Crown Point	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0					up to 10		"Thins to laminae a few grains thick near forest, thickens towards 1m high stabalized dune at NW edge of cove."				Fibrous peat	Mud	Sharp		4.0-2.0		Fine to very fine sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	239	50	Shana Creek	43.3200	-124.3100	Marsh	Small (<100 m) marshes in middle estuary.					"2.5 cm gouge cores, 7.5 cm pipe cores"		2-3	2	y	2-3	2	0	1	1	1	0.5-1.0					8-40						Fibrous to fine grained peat	Mud	Sharp				Sand											"Nelson et al., 1998"	Journal	1998	"Charleston, OR"
"Coos Bay, OR"	235	50		43.3200	-124.3100	Marsh	River/estuary/ small bay							2-4	2	y	2-4	2	0				0.5					thin						Peat		Capped				Silty sand										"Identified only as 2 abruptly burried peats capped by thin layer of silty sand (cited as unpublished 1988 data). Other papers on Coos Bay (Peterson and Darienzo, 1989, Nelson, 1992, Nelson et al., 1996) discuss subsidence, but no others discuss tsunami deposits or metion sand layers in their stratigraphy. Darienzo and Peterson (1995) compare it with other central Oregon sites as being similar, at least for a young burial event."	"Nelson and Peronius, 1996"	Journal	1996	"Charleston, OR"
"Coos Bay, OR"	236	50		43.3200	-124.3100	Marsh	River/estuary/ small bay							4-9	2	y	4-9	2	0											Landward thinning				Peat or detrital material	Peat or detrital material	Sharp	Sharp			Sand										"Tsunami deposits described are termed candidate tsunami deposits. Coseismic subsidence is noted for each tsunami event, but due to location of the zero isobase, not necessarily where evidence for tsunami is strongest."	"Briggs, 1994"	Thesis (M.S.)	1994	"Charleston, OR"
"Coquille River, OR "	237	51	"Bandon Marsh, Randolf Island"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	1	1	1			0-286	1700	Age range from Seven Mile Creek and Fahys/Osprey localities												Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	238	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	3	2	3			1526-1701		Age range from Seven Mile Creek and Fahys/Osprey localities	2 (in core O)			2		2 fining upwards beds of sand to muddy sand in core L.						Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	239	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	4	3	4			2150-2360		Age range from Seven Mile Creek and Fahys/Osprey localities											3.0 - 1.0	Muddy sand to sandy mud	Medium-fine grained		Fining upward	Well sorted								"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	240	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	5	4	5			2871-3074		Age range from Seven Mile Creek and Fahys/Osprey localities				2		Multiple fining upward sequences at Sevenmile Creek.					3.0 - 1.0	Muddy sand to sandy mud	Medium-fine grained		Fining upward	Well sorted								"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	241	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	6	5	6			3377-3476		Age range from Seven Mile Creek and Fahys/Osprey localities				2		Multiple fining upward sequences at Sevenmile Creek.					3.0 - 1.0	Muddy sand to sandy mud	Medium-fine grained		Fining upward	Well sorted								"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	242	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	7	6	7			3864-4085		Age range from Seven Mile Creek and Fahys/Osprey localities				>4		Multiple fining upward sequences at Sevenmile Creek.						Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	243	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	8	7	8			4411-4566		Age range from Seven Mile Creek and Fahys/Osprey localities				8		Multiple fining upward sequences at Sevenmile Creek.					3.0 - 1.0	Muddy sand to sandy mud	Medium-fine grained		Fining upward	Well sorted								"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	244	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	9	8	9					Not dated												Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	245	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	10	9	10			4986-5286		Age range from Seven Mile Creek and Fahys/Osprey localities				>4		Multiple fining upward sequences at Sevenmile Creek.					3.0 - 1.0	Muddy sand to sandy mud	Medium-fine grained		Fining upward	Well sorted								"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	246	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	11	10	11			6200-6410		Age range from Seven Mile Creek and Fahys/Osprey localities				2								Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Coquille River, OR "	247	51	"Sevenmile Creek, Ferry Creek, Fahys Creek"	43.1300	-124.4200	Marsh	River/estuary	>8000	Up river			"Gouge cores, vibracores, cutbank exposures"		12	11	y	12	11	0	12	11	12			6489-6724		Age range from Seven Mile Creek and Fahys/Osprey localities	18 (in core M)			4				Abrupt	Abrupt			Muddy sand to sandy mud			Fining upward									"Witter, 1999"	Thesis (Ph.D.)	1996	"Riverton, OR"
"Bradley Lake, OR"	248	52		43.0700	-124.4300	Lake	Lake formed by stream blocked by coastal sand dunes.				6		"14 piston cores, 13 vibracores"	16	7												61 AMS (super 14)C ages on delicate terrestrial macrofossils	1-50												Sand										One of the longest records of tsunami deposition on the Pacific Northwest coast (7300 years)	"Nelson et al., 1998"	Abstract	1998	"Bandon, OR"
"Bradley Lake, OR"	249	52		43.0700	-124.4300	Lake	Lake formed by stream blocked by coastal sand dunes.	500	Open coast		6			13	13												13 events in last 7300 years. Intervals range from <50 - 850 years	3-150												Sand								Diatom biostratigraphy records influxes of marine water into the otherwise freshwater lake		One of the longest records of tsunami deposition on the Pacific Northwest coast (7300 years)	"Kelsey et al., 1998a"	Abstract	1998	"Bandon, OR"
"Bradley Lake, OR"	250	52		43.0700	-124.4300	Lake	Freshwater lake	500	Open coast	5.5				8-9	8-9													up to 70 cm in oceanward portion of lake		"Continuous layers in lake, thins landward"				Lake mud	Lake mud	"Sharp, sometimes erosional"				Sand						"Rip-up clasts of lake substrate, capped by woody detritus."				Paired study with Sixes River	"Kelsey et al., 1995"	Abstract	1995	"Bandon, OR"
"Bradley Lake, OR"	251	52		43.0700	-124.4300	Lake	Freshwater lake	500	Open coast	5.5				3	3									300																Sand								Planktonic marine diatoms at top of sand layers		Paired study with Sixes River	"Kelsey et al., 1994"	Abstract	1994	"Bandon, OR"
"Bradley Lake, OR"	252	52		43.0700	-124.4300	Lake	Freshwater lake	500	Open coast	5.5				3	3									1000																Sand								Planktonic marine diatoms at top of sand layers		Paired study with Sixes River	"Kelsey et al., 1994"	Abstract	1994	"Bandon, OR"
"Bradley Lake, OR"	253	52		43.0700	-124.4300	Lake	Freshwater lake	500	Open coast	5.5				3	3									1600																Sand								Planktonic marine diatoms at top of sand layers		Paired study with Sixes River	"Kelsey et al., 1994"	Abstract	1994	"Bandon, OR"
"Sixes River, OR"	253	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	1	1	1						Lower meander: 3.3		Discontinuous. patchy				Peat to peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	254	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	2	2	2		2068±32	1940-2130			Lower meander: 0.5		Discontinuous. patchy				Peat to peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	254	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	3	3	3						Lower meander: 0.1		Discontinuous. patchy				Peat to peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	255	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	4	4	4		2505±31	2460-2750			Lower meander: 3.4		Discontinuous. patchy	3		Multiple fining upward cycles	Peat to peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	255	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	5	5	5	0.4-2.4	2883±33	2880-3160			Lower meander: 0.9		Discontinuous. patchy				Peat to peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	256	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	6	6	6	0.4-2.4	3254±22	3390-3560			Lower meander: 0.8    Upper meander: 10.2		Discontinuous. patchy				Peat to mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	256	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	7	7	7	"0.5 median,1.4 maximum"	3486±46	3630-3560			Lower meander: 8.5  Upper meander: 5.3		Discontinuous. patchy	2		Multiple fining upward cycles	Peat to mud		Abrupt to clear				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	257	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	8	8	8	0.4-2.4	3849Ñ22	4150-4410			Lower meander: 15.2   Upper meander: 24.8		Discontinuous. patchy	3		Multiple fining upward cycles	Peat to mud		"Abrupt, erosional"				Medium to fine sand		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	257	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	9	9	9	 	4362±51	4830-5220			Lower meander: 16.5		Discontinuous. patchy				Peat to mud		Abrupt to clear				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	258	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	10	10	10		4630±65	5050-5600			Lower meander: 7.5		Discontinuous. patchy				Peaty mud to mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	258	53		42.8700	-124.5308	Freshwater wetland	"Freshwater lowland, abandoned meander valley"	3600	Up River	1.7-4.2		"Outcrop, 2.5 cm gouge cores, 7.5 cm cores"	"21 reconnaissance cores, 28 (2.5 cm), 5 (7.5 cm)"	11	11	y	11	11	0	11	11	11		5205±65	5750-6180			Lower meander: 7.5  Upper meander: 25.0	42.00	Discontinuous. patchy	5		Multiple fining upward cycles	Peaty mud		Abrupt to gradual				Medium fine sand to sandy loam		Massive to fining upwards	Clean and well sorted in most cases			"In a few instances, rip-up clasts of underlying strata"		Marine diatoms		Infers an average recurrence interval for 11 earthquakes and tsunamis of 480-535 years.	"Kelsey et al., 2002"	Journal	2002	"Cape Blanco, OR"
"Sixes River, OR"	254	53	X	42.8700	-124.5308	"Low terrace, former tidal channel"	River/estuary	1200	Up river			"Soil pit , outcrop"		1	1	y	1	1	0	1	1	1		120±50	0-330	1700	AMS	0.2-0.5 	35 in former tidal channel at southern end of study area near this section (X)	Sheet over entire floodplain	2-3 layers		2-3 fining upwards sequences	"Soil developed on a silt loam to loamy sand-bioturbated, A horizon"	Sandy loam	Abrupt		3.0 - 1.0		Coarse sand to medium fine sand		2-3 fining upwards sequences				Wood detrirus		Brackish marine diatoms (also present below tsunami deposit)		Diatom data and soil desription available for download from GSA data depository GSA data repository 9826	"Kelsey et al., 1998b"	Journal	1998	"Cape Blanco, OR"
"Sixes River, OR"	255	53	Y	42.8700	-124.5308	"Low terrace, former tidal channel"	River/estuary	1200	Up river			"Soil pit , outcrop"		1	1	y	1	1	0	1	1	1				1700	Correllation with section X	0.2-0.5		Sheet over entire floodplain				Loamy soil	Silt loam and loam	Abrupt		3.0 - 1.0		Fine sand										Diatom data and soil desription available for download from GSA data depository GSA data repository 9826	"Kelsey et al., 1998b"	Journal	1998	"Cape Blanco, OR"
"Sixes River, OR"	256	53		42.8700	-124.5308	Marsh	River/estuary	3000																																Sand						Woody detritus				Paired study with Bradley Lake. Deposits at Sixes River related to incidences of liquifaction	"Kelsey et al., 1995"	Abstract	1995	"Cape Blanco, OR"
"Sixes River, OR"	257	53		42.8700	-124.5308	Marsh	River/estuary	3000	Inland of Cape Blanco							y								1600			"Age of youngest soil burial, 300 year event not clearly recorded"							Marsh soil		Abrupt		3.0 - 1.0		Fine to medium sand										Paired study with Bradley Lake	"Kelsey et al., 1994"	Abstract	1994	"Cape Blanco, OR"
"Sixes River, OR"	258	53		42.8700	-124.5308	Marsh	River/estuary	3000	Inland of Cape Blanco					3	3	y	3	1	0							1700 event correlated with youngest horizon	3 events over 5000 years							Peat		Abrupt		3.0 - 1.0		Fine to medium sand						"Spruce cones, needles, and twigs"					"Witter and Kelsey, 1994"	Abstract	1994	"Cape Blanco, OR"
"Sixes River, OR"	259	53		42.8700	-124.5308	"Infilled lake (cutoff meander) , marsh"	River/estuary				Tsunami either came through a 15-20 meter high gap in coastal bluffs or up Sixes River.	Cores		3	3	y	1	1	0			1					3 events over 2000 years	0.02-1.2	3.00					A-C soils				3.0 - 1.0		Very fine to fine sand											"Kelsey et al., 1993"	Abstract	1993	"Cape Blanco, OR"
"Elk River, OR"	260	54		42.7900	-124.5200	Marsh								3	3	y	3	1	0																															Similar marsh stratigraphy as Sixes River and Eucre creek.	"Witter and Kelsey, 1994"	Abstract	1994	"Cape Blanco, OR"
"Eucre Creek, OR"	261	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		4	1-2	y				1	1		>0.8					1-2		"Continuous, sheetlike"				Peat	Silty mud	Abrupt		3.0-1.0		Fine to medium sand		Fines upwards	Well sorted	 Subrounded		Detrital spruce needles and delicate twigs.	"Landward directed surge, source oceanward of marsh."	Marine brackish diatoms (Cosmioneis pusilla)		This report attributes only two of the four sand sheets to tsunami deposit and suggests that the other two events were deposited by el Nino storm surges or a remote tsunami.	"Witter et al., 2001"	Journal	2001	"Ophir, OR"
"Eucre Creek, OR"	262	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		4	1-2					2	2					1700		5-22		"Continuous, sheetlike"	2-3		2-3 fining upward intervals of medium to fine sand with pebbles at the base of each interval.	Peat	Silty mud	Abrupt/erosive		3.0-1.0		Fine to medium sand			Well sorted	 Subrounded		"Pebbles, mud rip up clasts, detrital spruce needles, and delicate twigs,"	"Landward directed surge, source oceanward of marsh."	Sparse marine brackish diatoms 		This report attributes only two of the four sand sheets to tsunami deposit and suggests that the other two events were deposited by el Nino storm surges or a remote tsunami.	"Witter et al., 2001"	Journal	2001	"Ophir, OR"
"Eucre Creek, OR"	263	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		4	1-2					3														Mud or incipient peaty soil	Silty mud	Abrupt		3.0-2.0		Clean fine sand			Well sorted	 Subrounded			"Landward directed surge, source oceanward of marsh."	Marine brackish diatoms (Thalassoria pacifica)		This report attributes only two of the four sand sheets to tsunami deposit and suggests that the other two events were deposited by el Nino storm surges or a remote tsunami.	"Witter et al., 2001"	Journal	2001	"Ophir, OR"
"Eucre Creek, OR"	264	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		4	1-2					4														Mud or incipient peaty soil	Silty mud	Irregular/errosive		3.0-2.0		Clean fine sand			Well sorted	 Subrounded		Mud clasts	"Landward directed surge, source oceanward of marsh."	Marine brackish diatoms (Thalassoria pacifica)		This report attributes only two of the four sand sheets to tsunami deposit and suggests that the other two events were deposited by el Nino storm surges or a remote tsunami.	"Witter et al., 2001"	Journal	2001	"Ophir, OR"
"Eucre Creek, OR"	265	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		5	5	y	5	5	0	1	1	1	Largest subsidence accompanies youngest earthquake					2.0-3.0						"Sandy mud to silty, clay-rich mud"	Silty mud			3.0-2.0		Fine sand (predominantly)		"Normal - fines upward, terminates in woody organic debris."	Well sorted	 Subrounded		"Detrital spruce needles and delicate twigs, woody organic layer on top of sand."	"Landward directed surge, source oceanward of marsh."				"Witter and Kelsey, 1996"	Abstract	1996	"Ophir, OR"
"Eucre Creek, OR"	266	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		5	5	y	5	5	0	2	2	2												"Sandy mud to silty, clay-rich mud"	Silty mud			3.0-1.0		Fine to medium sand			Well sorted	 Subrounded		"Detrital spruce needles and delicate twigs, woody organic layer on top of sand."	"Landward directed surge, source oceanward of marsh."				"Witter and Kelsey, 1996"	Abstract	1996	"Ophir, OR"
"Eucre Creek, OR"	267	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		5	5	y	5	5	0	3	3	3						21.00			2-3		2-3 fining upwards intervals that encorporate large pebbles near  base.	"Sandy mud to silty, clay-rich mud"	Silty mud			3.0-1.0		Fine to medium sand			Well sorted	 Subrounded		"Detrital spruce needles and delicate twigs, woody organic layer on top of sand."	"Landward directed surge, source oceanward of marsh."				"Witter and Kelsey, 1996"	Abstract	1996	"Ophir, OR"
"Eucre Creek, OR"	268	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		5	5	y	5	5	0	4	4	4												"Sandy mud to silty, clay-rich mud"	Silty mud			3.0-1.0		Fine to medium sand			Well sorted	 Subrounded		"Detrital spruce needles and delicate twigs, woody organic layer on top of sand."	"Landward directed surge, source oceanward of marsh."				"Witter and Kelsey, 1996"	Abstract	1996	"Ophir, OR"
"Eucre Creek, OR"	269	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast			"Gouge cores, vibracores"		5	5	y	5	5	0	4	5	5												"Sandy mud to silty, clay-rich mud"	Silty mud			3.0-1.0		Fine to medium sand			Well sorted	 Subrounded		"Detrital spruce needles and delicate twigs, woody organic layer on top of sand."	"Landward directed surge, source oceanward of marsh."				"Witter and Kelsey, 1996"	Abstract	1996	"Ophir, OR"
"Eucre Creek, OR"	270	55		42.5600	-124.3900	Marsh	Small freshwater wetland along a coastal stream	500	Open coast					3	3	y	3	3	0								3 events over 2000 years	"22 cm bed overlies oldes peat, consists of multiple intervals"			multiple sand intervals		Incorporates large pebbles near base and fines upwards.	Peat		Abrupt		3.0-1.0		"Fine to medium sand, large pebbles in layer above oldest peat."						"Spruce cones, needles, and twigs."					"Witter and Kelsey, 1994"	Abstract	1994	"Ophir, OR"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	271	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	500	Open coast		2	Vibracores		up to 13	up to 13					1	1					1964		<1		Landward thinning																		Marine diatoms			" Garrison et al., 1997"	Abstract	1997	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	272	56		41.7300	-124.1500	"Marsh, freshwater"	broad coastal plain with low beach berm	500	Open coast		2	Vibracores		up to 13	up to 13					2	2					1960		<1		Landward thinning																		Marine diatoms			" Garrison et al., 1997"	Abstract	1997	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	273	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	500	Open coast		2	Vibracores		up to 13	up to 13													Up to 15 		Landward thinning																		Marine diatoms		"Thinner sand sheets attributed to remote tsunamis, thicker sand sheets attributed to Cascadia events"	" Garrison et al., 1997"	Abstract	1997	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	274	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	100	Open coast			Vibracores	40	12 (10 prehistoric)	12 (10 prehistoric)					1	1					1964		<2		Restricted to seaward edge of marshes.				Peat	Peat			3.0-1.0		Fine to medium sand			Well sorted								"Carver et al., 1996"	Abstract	1996	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	275	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	100	Open coast			Vibracores	40	12 (10 prehistoric)	12 (10 prehistoric)					2	2					1960		<2		Restricted to seaward edge of marshes.				Peat	Peat			3.0-1.0		Fine to medium sand			Well sorted								"Carver et al., 1996"	Abstract	1996	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	276	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	"500 m (events 3,4), 6 of remaining ten prehistoric tsunami deposits are similar in extent to historic deposits (100m)."	Open coast			Vibracores	40	12 (10 prehistoric)	12 (10 prehistoric)					3	3				0-512		Radiocarbon	up to 25 		Landward thinning	up to 10		"Up to 10 normally graded sequences (in some cores), sometimes separated by silty and clayey laminations."	Peat	Peat			3.0-1.0		Fine to medium sand		Normal (in some cores)	Well sorted			Coarse woody debris several cm thick caps deposits at most sites.		Marine diatoms			"Carver et al., 1996"	Abstract	1996	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	277	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	"500 m (events 3,4), 6 of remaining ten prehistoric tsunami deposits are similar in extent to historic deposits (100m)."	Open coast			Vibracores	40	12 (10 prehistoric)	12 (10 prehistoric)					4	4				650-1173		Radiocarbon	up to 25 		Landward thinning	up to 10		"Up to 10 normally graded sequences (in some cores), sometimes separated by silty and clayey laminations."	Peat	Peat			3.0-1.0		Fine to medium sand		Normal (in some cores)	Well sorted			Coarse woody debris several cm thick caps deposits at most sites.		Marine diatoms			"Carver et al., 1996"	Abstract	1996	"Sister Rocks, CA"
"Crescent City, CA (along 5 km of open coast south of Crescent City)"	278	56		41.7300	-124.1500	"Marsh, freshwater"	Broad coastal plain with low beach berm	"500 m (events 3,4), 6 of remaining ten prehistoric tsunami deposits are similar in extent to historic deposits (100m)."	Open coast			Vibracores	40	12 (10 prehistoric)	12 (10 prehistoric)					5-13	5-13							up to 25 		Landward thinning	up to 10		"Up to 10 normally graded sequences (in some cores), sometimes separated by silty and clayey laminations."	Peat	Peat			3.0-1.0		Fine to medium sand		Normal (in some cores)	Well sorted			Coarse woody debris several cm thick caps deposits at most sites.		Marine diatoms			"Carver et al., 1996"	Abstract	1996	"Sister Rocks, CA"
"Lagoon Creek, CA"	279	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	870	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"		6					1	1			370±70	0-560	1700	"Radiocarbon (AMS), just below sand layer"	0-4.5		Landward thinning	1		Each extensive sand layer preserved as a single layer.	Peat	Peaty mud	Sharp	Gradational	3.0-1.0		Fine to medium sand	Fines landward	Normal	Well sorted			Rip up clasts of peat and mud.	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	280	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	1130	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"	6	6					2	2			1220±40	970-1350		"Radiocarbon (AMS), top of sand layer"	0.3-16.5		Landward thinning	1		Each extensive sand layer preserved as a single layer.	Peat	Peaty mud	Sharp	Gradational	3.0-1.0		Fine to medium sand	Fines landward	Normal	Well sorted			"Rip up clasts of peat and mud, wood, twigs, spruce cones. Needles, and other plant detritus."	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	281	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	1060	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"	6	6					3	3			1470±70	1280-1550		Radiocarbon (AMS)in sand	5-10		Landward thinning	1		Each extensive sand layer preserved as a single layer.	"Muddy peat, diamicton in some cores"	Peaty mud	Sharp	Gradational	3.0-1.0		"Fine to medium sand, contains coarse angular sandstone and shale clast landward of diamicton"	"Fines landward, except coarsens landward of diamicton, which it overlies."	Normal	"Well sorted, except inland of diamicton."			"Rip up clasts of peat and mud, only in a few cores, twigs."	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	282	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	1130	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"	6	6					4	4			1590±60	1300-1820		Radiocarbon (AMS) in peat below sand	0.3-40		Landward thinning	1		Each extensive sand layer preserved as a single layer.	"Peat, in one core overlies a diamicton"	Mud	Sharp	Gradational	3.0-1.0		Fine to medium sand	"Fines landward, except coarsens landward of diamicton, which it overlies."	Normal	"Well sorted, except inland of diamicton."			"Rip up clasts of peat and mud, only in a few cores, wood, twigs, spruce cones."	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	283	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	1110	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"	6	6					5	5			2500±50	2350-2760		Radiocarbon (AMS)in sand	15-22		Exposed in only a few cores on seaward side of the marsh.	1		Each extensive sand layer preserved as a single layer.	Peat	Peaty mud	Sharp	Sharp	3.0-0.0		Coarse to fine sand	Fines landward	Normal	Well sorted			"Abundant large rip up clasts of peat and mud, bark, wood, twigs."	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	284	57		41.5900	-124.1000	marsh (freshwater) and lily pond	Narrow flat-lying valley	625	Open coast		5 (MHHW) - sandy beach berm separating pond from open ocean.	"Gouge cores, vibracores"	"50 gouge cores, 21 vibracores"	6	6					6	6			3090±50	3070-3470		"Radiocarbon (AMS), top of sand layer"	9.5		Exposed in only a few cores on seaward side of the marsh.	1		Each extensive sand layer preserved as a single layer.	Peat	Peaty mud	Sharp	Gradational	3.0-1.0		Fine to medium sand	Fines landward	Normal	Well sorted			"Rip up clasts of peat and mud, twigs."	Landward directed surge	Marine diatoms			"Abramson, 1998"	Thesis (M.S.)	1998	"Requa, CA"
"Lagoon Creek, CA"	285	57		41.5900	-124.1000	marsh (freshwater) and lily pond	narrow valley with high beach berm	1500	Open coast		6	Vibracores		Up to 13	Up to 13													Thinner than at Crescent City		Landward thinning																		Marine diatoms			" Garrison et al., 1997"	Abstract	1997	"Requa, CA"
"South Humboldt Spit, CA"	286	58		40.6197	-124.3174	Marsh	Bay side of spit							2	2					1	1				~300	1700	Radiocarbon																							Tsunami deposits associated with coseismic uplift.	"Leroy, 1999"	Thesis (M.S.)	1999	"Canibal Island, CA"
"South Humboldt Spit, CA"	287	58		40.6197	-124.3174	Marsh	Bay side of spit							2	2					2	2				~1100		Radiocarbon																							Tsunami deposits associated with coseismic uplift.	"Leroy, 1999"	Thesis (M.S.)	1999	"Canibal Island, CA"
"Eel River, CA"	288	59	ER-VC-06	40.7021	-124.2679	Marsh	Marshes along river mouth					"Vibracores,hand-augered cores, bank exposures"	55	5	2	y	5	2	0	2	1	2		860±70	620-1060			0.2-0.4						Peat	Peat			3.0-2.0		Fine sand (0.1-0.5 mm)										Only evidence is a sand capping layer in one core. No other cores show evidence of this layer.	"Li, 1992"	Thesis (M.S.)	1992	"Canibal Island, CA"
"Eel River, CA"	289	59	ER-VC-06	40.7021	-124.2679	Marsh	Marshes along river mouth					"Vibracores,hand-augered cores, bank exposures"	55	5	2	y	5	2	0	3	2	3		1290±60	960-1410			0.2-0.4						Tidal mud	Tidal mud			3.0-2.0		Fine sand (0.1-0.5 mm)										Only evidence is a sand capping layer in one core. No other cores show evidence of this layer.	"Li, 1992"	Thesis (M.S.)	1992	"Canibal Island, CA"