My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2012-03-07_PERMIT FILE - C2010088 (12)
DRMS
>
Day Forward
>
Permit File
>
Coal
>
C2010088
>
2012-03-07_PERMIT FILE - C2010088 (12)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 4:54:49 PM
Creation date
3/8/2012 12:18:39 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C2010088
IBM Index Class Name
Permit File
Doc Date
3/7/2012
Doc Name
Cultural Resource Inventory
Section_Exhibit Name
Exhibit 02
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
10
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
1000, but the period was punctuated with decades of drought staggered with <br />decades of abundant precipitation. The Great Salt Lake reduced to near historic <br />levels. <br />The Little Ice Age (AD 1300 -1800; 700 -200 BP) was cooler than today <br />from about AD 1300 -1650 with dips in the mid -18th, 19th, and early 20th <br />centuries. [Some extend this period through AD 1850 when there was another <br />cold dip.] A rapid cooling of the climate occurred in the 14th century, then a <br />variable but cool /moist climate continued through the period. There was a <br />return to winter dominant rainfall with periods of great storms. In fact, the <br />Great Salt Lake flooded the Great Salt Lake Desert in the early AD 1600's. <br />After the AD 1850's, a warming trend began, and a steep rise in temperatures <br />occurred through modern times. Most recently that trend has been attributed to <br />human- caused warming that has been superimposed on other factors shaping <br />the climate. <br />Simms (2008:76) also presents a chart showing the levels of Lake Bonneville and the <br />Great Salt Lake that provides a relative magnitude of decreased/increased moisture throughout <br />the region. The lakes reached their lowest levels between about 11,000- 10,500 BP, 9000 -8000 <br />BP, 7200 -6200 BP, 5600 -3800 BP, and 1100 -850 BP. <br />Summary of Files Search and Literature Overview <br />The files search indicated that no cultural resources had been previously recorded <br />within the block area. The review showed that fourteen resources had been previously <br />recorded in the surrounding area; these are listed below on Table 1. Additionally, the files <br />search indicated that five cultural resource studies have been previously conducted in the <br />nearby vicinity; these are listed below on Table 2. A search of the historic government land <br />office survey maps dated 1918 by Tufts, indicated that the historic Salt Lake Wagon Road <br />passed through the present study area near its southwest corner. No evidence of the road <br />could be found within the present project boundary. <br />Cultural resource investigations in the region have yielded surface diagnostic artifacts <br />and excavated cultural materials consistent with the regional cultural history. Evidence <br />provided by chronometric diagnostic artifacts and radiocarbon analyses indicate regional <br />occupation during the Paleoindian, Archaic, Formative, and Protohistoric Eras. Historic <br />records suggest occupation or use of the region by EuroAmerican trappers, settlers, miners, <br />and ranchers as well. Overviews of the prehistory and history of the region are provided in the <br />Colorado Council of Professional Archaeologists' publications entitled "Colorado Prehistory: <br />A Context for the Northern Colorado River Basin" (Reed and Metcalf 1999), and "Colorado <br />History: A Context for Historical Archaeology" (Church et al. 2007). <br />0 <br />
The URL can be used to link to this page
Your browser does not support the video tag.