My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2002-06-05_PERMIT FILE - M2002004 (3)
DRMS
>
Day Forward
>
Permit File
>
Minerals
>
M2002004
>
2002-06-05_PERMIT FILE - M2002004 (3)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 2:18:41 PM
Creation date
10/15/2010 10:35:22 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2002004
IBM Index Class Name
PERMIT FILE
Doc Date
6/5/2002
Doc Name
Proposed Access Road, Overview Survey, and Predictive Model
From
URS
To
DRMS
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.
/
76
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
Proposed Limestone Quarry Access Road and Overview Cultural Resources Inventory <br />Geology <br />The bedrock geology of the proposed project area is dominated by the Niobrara Formation, <br />which consists of calcareous shale and limestone. Deposits of Carlisle Shales, Greenhorn <br />Limestone, and Graneros Shale are located to the west of the project area, but within the larger <br />lease area. An area along the St. Charles River contains Holocene- and Pleistocene-age <br />Pinedale gravels and alluviums and Pleistocene-age Bull Lake and Pre-Bull Lake gravels and <br />alluviums (Tweeto 1979). <br />Soils <br />Soils in the proposed project area are mainly composed of Manvel silt loam, on generally level <br />areas of 1-5° slopes. This is a deep, well-drained soil that formed mainly on alluvial fans in silty <br />colluvial and alluvial materials that weathered mainly from limestone. Soils of the Penrose- <br />Minnequa complex occur in the area near small drainages in the northwestern portion of the <br />project area. This soil is shallow, well drained, loamy soil formed in residuum from limestone. <br />Haverson silt loam soil occurs on some of the low terraces overlooking the St. Charles River. <br />This is a deep well-drained soil that formed on floodplains in loamy alluvium. The edges of the <br />bluffs along the north side of the river are covered by Cascajo very gravelly sandy loam soil. <br />This soil consists of deep and excessively drained soil that formed on terraces in gravelly sandy <br />alluvium (USDA 1979). <br />Climate <br />The proposed project area climate is characterized as semiarid and typical of the southeastern <br />plains. Average annual precipitation at Pueblo is 11.9 inches. January is the coldest month, <br />with an average daily low of 14.7° F, July is the warmest, with an average daily high of 91.1 ° F, <br />and the average annual daily high is 67.9° F and the low is 37.7° F. The growing.season occurs <br />between April and October and averages 167 days (USDA 1979). <br />Vegetation <br />The proposed project area is characterized by two major native plant associations: short-grass <br />grassland and juniper-pinyon woodland. Most of the project area is dominated by grassland <br />(wheatgrass, cheat grass, grama, and Indian ricegrass). Small stands of juniper-pinyon <br />woodland are located along some of the drainages, and riparian vegetation (cottonwoods and <br />willows) borders the St. Charles River (Mead 1996). <br />Wildlife <br />A wide range of animal species is present in the general area. Mammals are represented by <br />mule deer, pronghorn, coyote, fox, skink, white-tailed jack rabbit, cottontail, and several species <br />of rodents. Buffalo would have been present in the region in early historic times. Larger bird <br />species in the area include stellar jays and raptors, such as red-tailed hawks (Mead 1986). <br />Ii S 3
The URL can be used to link to this page
Your browser does not support the video tag.