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What the map shows (click on the image to see a large
map [82 kb])
The map depicts the rock formations and surfice deposits in different
colors. In general, surface deposits are shown in shades of yellow, volcanic
rocks such as basalt and rhyolite are in oranges, granites are in reds,
pinks, and greens, and metamorphic rocks are in blues and browns. Comparing
the geologic map to the landforms map made from DEMs
shows that most surficial deposits (yellows) are in the basins and most
other rocks form mountains.
Geologic maps not only show the rocks and unconsolidated deposits exposed
at the surface of the earth, but they also give information on the deformation
of those materials (such as by earthquakes), the age of the materials, and
the past geography and environments of the area. With the information shown
on geologic maps, it is possible to predict what rocks are beneath the surface
and to describe the changes in the geology of the region for hundreds over
millions of years.
Heavy lines on the map represent faults, most of which were recently active
and moved during earthquakes. Two sets of faults, those oriented east and
those oriented northwest, are evident. The east-oriented faults very commonly
are the boundaries between uplifted hills of bedrock on their south sides
and alluvial basins on their north sides. This correlation between today's
landforms and the faults leads us to infer that the faults are young and
that part of their movement included an up-to-the-south motion.
This geologic map was constructed by examining rocks and soils in the
field, and by using aerial photographs and satellite
images as aids to better understand the distribution of the rocks. Geophysical data also aid in interpreting the
geology and locating features such as faults. This particular map is generalized
from six more detailed maps, available below.
In the office, the geology was drafted onto topographic maps, then scanned
into the computer. All lines and polygons were tagged in ARC/INFO and other
information was added to create a geologic data base. One use of the data
base is to create a full-color map, and it is a powerful tool for creating
all kinds of derivative maps. Examples are flood
and earthquake hazard
maps, maps showing change in the environment, and maps for analyzing
questions about the past history of the earth.
The base map (showing roads, streams, and elevation contours) is the Soda
Mountains 1:100,000-scale topographic map. Download
base map
We
can tell the ages of rocks by identifying fossils whose ages are known from
other places, by dating the rocks using isotopic decay 'clocks', and by
identifying volcanic ashes with ages determined elsewhere. All of these
methods have been used in the geologic studies at Fort Irwin.
Detailed geologic maps of southwestern Fort Irwin
Click on a quadrangle to download graphics files (~xx kb each) (under
construction)
Preliminary Geologic Map of Fort Irwin Basin, north-central Mojave Desert,
California
by James C. Yount, Elizabeth R. Schermer, Tracey J. Felger, David
M. Miller, and Kirk A. Stephens: U.S. Geological Survey Open-File Report
94-173.
Download digital data (under construction)
Download text and graphic files (under construction)
Topographic base maps