My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD08945
CWCB
>
Floodplain Documents
>
Backfile
>
8001-9000
>
FLOOD08945
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 10:07:17 AM
Creation date
10/5/2006 3:59:51 AM
Metadata
Fields
Template:
Floodplain Documents
County
Larimer
Community
Fort Collins
Stream Name
Dry Creek
Basin
South Platte
Title
Hydrologic Analysis Major Drainageway Planning Dry Creek
Date
7/1/1979
Prepared For
Larimer County
Prepared By
Gingery Associates, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
32
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).
Show annotations
View images
View plain text
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br /> <br />- THE DRY CREEK BASIN - <br /> <br />Basin Description. The Dry Creek Basin is long and narrow with its <br />upper reaches in the eastern foothills of the Rocky Mountains and its <br />lower reaches extending onto the agricultural plains immediately north <br />of Fort Collins (Figure 1). The basin is in east central Larimer <br />County with portions of the lower basin extending into Fort Collins. <br />The basin encompasses a drainage area of approximately 65 square <br />miles with basin elevations ranging from 7,000 feet MSL in the foot- <br />hills to 4,900 feel MSL near Fort Collins. The average basin slope <br />is approximately 2% in a southeasterly direction. Eleven major <br />irrigation canals and 13 major, and several minor storage reservoirs <br />are part of an extensive irrigation network within the basin (Figure 2). <br />The Dry Creek stream channel is tributary to the Cache la Poudre <br />River immediately east of Fort Collins. The channel generally has a <br />well defined, meandering low flow section, and a wide, gently sloped <br />overbank area. In the reach below the Eaton Ditch, however, the <br />channel has been obliterated by development over much of its length. <br />The Dry Creek channel has many tributaries along its length with the <br />major ones, Park Creek and Spring Gulch, joining Dry Creek in the <br />upper third of the basin. <br />The channel is intercepted at two locations by major on-stream <br />reservoirs, Douglas Reservoir and Park Creek Reservoir (Figure 2). <br />Park Creek Reservoir is a fairly new U.S.B.R. storage reservoir lo- <br />cated high in the upper basin on the Park Creek tributary to Dry <br />Creek. The reservoir has a surface area of approximately 190 acres, <br />and a tributary area of 3.8 square miles. Douglas Reservoir is lo- <br />cated on Dry Creek in approximately the middle of the basin. This <br />reservoir has a surface area of about 640 acres and a tributary <br />drainage area of 44.0 square miles. <br />Historically, the Dry Creek Basin has been in agricultural land <br />use with a very active irrigation network. Over the past 30 years, <br />the basin has been experiencing development in the lower reach below <br />U.S. Highway 287. The development in some cases has obliterated <br />the historic Dry Creek channel, particularly in reaches near College <br />Avenue. Commercial and light industrial development is rapidly ex- <br />panding in the basin reach near the confluence with the Cache la <br />poudre River, in the area surrounding the Valley Airpark. The area <br />immediately downstream of College Avenue is currently experiencing <br /> <br />-2- <br />
The URL can be used to link to this page
Your browser does not support the video tag.