My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD05505
CWCB
>
Floodplain Documents
>
Backfile
>
5001-6000
>
FLOOD05505
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:49:25 PM
Creation date
10/5/2006 1:36:42 AM
Metadata
Fields
Template:
Floodplain Documents
County
Gunnison
Community
Gunnison County
Stream Name
Gunnison River, Tomachi Creek
Basin
Gunnison
Title
Floodplain Information Report
Date
12/1/1976
Prepared For
Gunnison County
Prepared By
ECI
Contract/PO #
&&
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.
/
59
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 /> <br />Characteristics of Different Reaches <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />The study reaches for Gunnison River and Tomichi Creek are <br /> <br />shown on the Index Map, (Plate '2). The Gunnison River reach extends <br /> <br /> <br />from the bridge across Gunnison River on Colorado Highway 135 to McCabe <br /> <br /> <br />Bridge located approximately 1.6 miles downstream from Tomichi Creek <br /> <br /> <br />confluence with Gunnison River. The Tomichi Creek reach extends from <br /> <br /> <br />the point of its confluence with Gunnison River to its upper limits <br /> <br /> <br />represented by a point approximately 500 feet downstream from New Mexico <br /> <br /> <br />Principal Meridian. The lengths of the two reaches are approximately <br /> <br /> <br />7.6 and 4.9 miles for Gunnison River and Tomichi Creek, respectively. <br /> <br /> <br />The stream valleys in the study reach are generally charac- <br /> <br />terized by broad plains extending between hills. These plains vary in <br /> <br /> <br />width, and are in excess of 2 miles wide at certain locations. Alluvial <br /> <br />lands on the flood plains along streams consist primarily of material <br /> <br /> <br />recently deposited by streams. The texture is widely variable and <br /> <br /> <br />commonly has very cobbly or stony areas interspersed throughout. These <br /> <br />lands are subject to erosion from floods and changes in stream channels. <br /> <br /> <br />The streams have the tendency to meander, especially Tomichi Creek. <br /> <br /> <br />Future floods are likely to shift the river channel as it has in the <br /> <br /> <br />past. <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />The historical use of the flood plain has been for range and <br /> <br />wildlife with limited improvements confined to dwellings and other <br /> <br /> <br />structures supporting ranching activities. Irrigated pastures on these <br /> <br /> <br />plains have good plant cover and support meadow vegetation, willows and <br /> <br />narrow leaf cottonwood. Small areas within the floodplain are flooded <br /> <br /> <br />annually and support little or no vegetattion. The growth of Gunnison <br /> <br /> <br />in recent years has forced greater development in the flood plain par- <br /> <br /> <br />ticularly along Gunnison River in the western part of the city and in <br /> <br /> <br />the vicinity of Dos Rios Island. With this increased encroachment of <br /> <br /> <br />development in the floodplain, the flood hazard to the community is <br /> <br /> <br />increased and will continue in the future unless adequate measures are <br /> <br /> <br />adopted to keep the development outside the flood hazard areas. <br /> <br /> <br />Obstructions to floodflows within the study reach include both <br /> <br /> <br />natural obstructions such as vegetation growth, fallen trees, ice jams, <br /> <br />12 <br />
The URL can be used to link to this page
Your browser does not support the video tag.