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Last modified
1/25/2010 6:47:04 PM
Creation date
10/5/2006 12:55:35 AM
Metadata
Fields
Template:
Floodplain Documents
County
Gunnison
Community
Gunnison County and Unincorporated Areas
Basin
Gunnison
Title
FIS - Gunnison County and Unincorporated Areas
Date
9/29/1989
Prepared For
Gunnison County
Prepared By
FEMA
Floodplain - Doc Type
Current FEMA Regulatory Floodplain Information
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<br />2.2 Community Description <br /> <br />Gunnison County is <br />bordered by Saguache <br />County to the east; <br />Delta, Montrose, and <br /> <br />located 10 southwestern <br />and Hinsdale Counties to <br />pitkin and Mesa Counties <br />Ouray Counties to the west. <br /> <br />Colorado and is <br />the south; Chaffee <br />to the north; and <br /> <br />The Gunnison River, formed by the confluence of the Taylor and <br />East Rivers at Almont, has a well-developed st ream pat tern wi th <br />inflowing tributaries from different directions. The larger of <br />these tributaries contributing to the flooding problems in the <br />study area include Ohio and Tomichi Creeks. <br /> <br />The North Fork Gunnison River is formed by the confluence of Muddy <br />and Anthracite Creeks near Paonia Dam. From its SOurce to its <br />mouth near Lazear, the stream flows approximately 30 miles on a <br />southwesterly course. <br /> <br />The average altitude of the Gunnison River Basin above the study <br />area is relatively high, ranging in elevation from approximately <br />7,600 feet above mean sea level at the Tomichi Creek confluence <br />wi th the Gunni son River to over 14,000 feet at the high peaks of <br />the Continental Divide. <br /> <br />The terrain of the basin 15 mostly mountainous with some broad <br />plains in the stream valleys between hills. These plains vary in <br />width and are in excess of 2 miles at certain locations. Alluvial <br />lands on the floodplains along streams consist primarily of <br />material recently deposited by the streams. The texture is widely <br />variable and commonly has very cobbly or stony areas interspersed <br />throughout. <br /> <br />Predominant vegeta.tion consists of pine, fir, and spruce in the <br />higher portions of the drainage area, while sagebrush and other <br />low-growing shrubs exi st in the lower port ions. Thick stands of <br />cottonwood thrive along the river. <br /> <br />Summers are cool in the study area with average high temperatures <br />of 80oF. Temperatures for summer nights usually drop below 50oF. <br />Temperatures have ranged from -470F in the winter to 960F in the <br />summer. The mean annual maximum temperature is 52oF, and the mean <br />annual minimum temperature is 17.50F. <br /> <br />The climate of the study area includes low precipitation, low <br />humidity, abundant sunshine, a wide daily temperature range, and <br />generally low winds. The surrounding mountains act as a barrier, <br />preventing the northern cold air or eastern storms from penetrat- <br />ing the Upper Gunnison River Valley. <br /> <br />4 <br />
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