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PERMFILE112178
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PERMFILE112178
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Last modified
8/24/2016 10:08:36 PM
Creation date
11/24/2007 9:15:25 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980005
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
TAB 05D IDENTIFICATION OF SENSITIVE CULTURAL RESOURCES WITHIN THE ONE MILE BUFFER ZONE OF THE SENECA
Media Type
D
Archive
No
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STUDY RESULTS <br />• . A review of the records of the Office of the State <br />Archaeologist, The State Historic Preservation Officer, and <br />with the Little Snake Resource Area Office of the Bureau <br />of Land Management located no recorded sites in the Seneca II <br />parcel or buffer zone. <br />Cultural resource inventories in the immediate area <br />have located sensitive site types, including rock art, rock <br />shelter, and historic structures (Arthur 1977; McNamara <br />1978; Wheeler,1980b). None of these are on the property <br />in question, however. <br />Archaeological and historical literature indicates that <br />there is indeed a possibility of locating sensitive sites in <br />the buffer zone. Major points of this review are presented <br />in the report on the cultural resource inventory of the <br />Seneca II coal lease (Wheeler 1980a)and will not be detailed <br />here. It is sufficient to note that aboriginal groups, <br />• especially those with Fremont and Ute affiliations, are <br />noted for the production of rock art, and t'rat the utilization <br />of rock shelters (as habi*_ation sites), when available, has been <br />a characteristic of aboriginal groups since Paleo-Indian <br />times. It is also worthy of note that °uro-American sites <br />are commonly architectural, and that these cultures are <br />known to have been in the area. <br />The literature also made_it clear, though it was not <br />explicitly stated, that rock art and rock shelter sites <br />occur in rock overhangs where water erosion has produced <br />steep rock walls. These overhangs in steep rock walls occur <br />along drainages where there has been enough water erosion <br />to downcut into the rock, producing the steep walls. <br />Usually these overhangs were utilized for habitation when <br />they exhibit a southern exposure, though this is not al;aays <br />the case. <br />Field inspection located a historic standing structure <br />• down the valley from 5RT142 (see Wheeler 1980a). The <br />5 <br />
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