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PERMFILE118671
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PERMFILE118671
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Entry Properties
Last modified
8/24/2016 10:14:22 PM
Creation date
11/25/2007 5:44:01 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977210
IBM Index Class Name
Permit File
Doc Date
3/1/1971
Doc Name
COURT TESTIMONRY IN 1971
Media Type
D
Archive
No
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~ ~i <br />,..,,,- non-eristert amount of Mountain Mahogany, It might be <br />. / .. <br />worth noting also in the foreground of this picture an <br />individual plant or specir:en of Pinon growing on some old <br />disturbed quarry material, <br />This is a closer view of19-B showing~in a littler <br />more detail the nature of the parent material, the substrata <br />on which these plants were growing. <br />I don't have a scale in this picture but: this <br />distance here that I am indicating that shows eons~iderable <br />i ~-r <br />fracturing, weathering, is in that range of say teen feet -- <br />up to ten feet, <br />:another close-~~p o° the limestone mater:Lals <br />with a Pinon-JUriaer "r~oodland on the west side of the main <br />quarry opening in the Snyc'er ruarry area. Pointi~~g out <br />individual species, these trees here somewhat lighter green <br />are the Pinon -- here are two examples of Rocky t~,~untain <br />Juniper -- again, very shallow soil material before reaching <br />S..•„7 bedrock, There is naturally a good deal of weathered fraq- <br />2 / V / <br />mentation, bigger fragmentation, with limestone incorporated <br />in the soil -- it is a rather rocky sail. <br />This is a view, 14-E, of a naturally occurring <br />almost vertical cliff of limestone west -- immediately <br />west of the Snyder Quarry area in the Williams Canyon. Plhite <br />showing two things, the relatively bare portion of the <br />cliff, the vertical portions, and then where thex•e is some <br />natural faces and benches, if you will, the oceux~rence of <br />some weathered material, some signs of some -- really not <br />very fine but rocky material and the growth of some trees <br />1269 <br /> <br />
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