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Topographic Change Detection at Select Archeological Sites in Grand Canyon National Park, Arizona, 2007-2010 - Usgs Scientific Investigations Report 2012-5133 (Paperback)
Loot Price: R378
Discovery Miles 3 780
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Topographic Change Detection at Select Archeological Sites in Grand Canyon National Park, Arizona, 2007-2010 - Usgs Scientific Investigations Report 2012-5133 (Paperback)
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List price R410
Loot Price R378
Discovery Miles 3 780
You Save R32 (8%)
Expected to ship within 18 - 22 working days
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Human occupation in Grand Canyon, Arizona, dates from at least
11,000 years before present to the modern era. For most of this
period, the only evidence of human occupation in this iconic
landscape is provided by archeological sites. Because of the
dynamic nature of this environment, many archeological sites are
subject to relatively rapid topographic change. Quantifying the
extent, magnitude, and cause of such change is important for
monitoring and managing these archeological sites. Such
quantification is necessary to help inform the continuing debate on
whether and how controlled releases from Glen Canyon Dam, located
immediately upstream of Grand Canyon National Park, are affecting
site erosion rates, artifact transport, and archeological resource
preservation along the Colorado River in Grand Canyon. Although
long-term topographic change resulting from a variety of natural
processes is inherent in the Grand Canyon region, continued erosion
of archeological sites threatens both the archeological resources
and our future ability to study evidence of past cultural
habitation. Thus, this subject is of considerable interest to
National Park Service managers and other stakeholders in the Glen
Canyon Dam Adaptive Management Program. Understanding the causes
and effects of archeological site erosion requires a knowledge of
several factors, including the location, timing, and magnitude of
the changes occurring in relation to archeological resources, the
rates of change, and the relative contribution of potential causes.
These potential causes include sediment depletion associated with
managed flows from Glen Canyon Dam, site-specific weather and
overland flow patterns, visitor impacts, and long-term regional
climate change.
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