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Last modified
11/23/2009 1:21:25 PM
Creation date
10/4/2006 9:31:15 PM
Metadata
Fields
Template:
Floodplain Documents
County
Larimer
Community
Estes Park
Stream Name
Lawn Lake
Title
Fall River Flood of July 15, 1982
Date
7/15/1982
Prepared By
CWCB
Floodplain - Doc Type
Flood Documentation Report
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<br />2.0 AREA STUDIED <br /> <br />2.1 Scope of Study <br /> <br />This Flood Insurance Study covers the incorporated area of the Town <br />of Estes Park, Larimer County, Colorado. The area of study is shown <br />on the Vicinity Map (Figure 1). <br /> <br />Floods caused by overflow of ~he Big Thompson River, Big Thompson <br />River Overflow Channel No.1, Big Thompson Overflow Channel No.2, <br />Fall River, Fish Creek, and a short reach of Black Canyon Creek near <br />the Municipal Building were studied in detail. Flooding on Black <br />Canyon Creek north of the Municipal Building and shallow flooding <br />caused by ponding of runoff were studied by approximate methods <br />because of a narrow flood plain and lack of development in these <br />areas.. <br /> <br />Those areas studied by detailed methods were chosen with consider- <br />ation given to all proposed construction and forecasted development <br />through 1982. <br /> <br />2.2 Community Description <br /> <br />The Town of Estes Park is located in the southwest corner of Larimer <br />County, in north-central Colorado. The picturesque setting of the <br />Rocky Mountains enhances the setting of this mountain town, which is <br />situated in upland valley at an elevation of 7500 feet. The high <br />peaks of Rocky Mountain National Park tower to the west. Roosevelt <br />National Forest surrounds the rest of Estes Park. The population <br />was 2147 according to the 1970 census (Reference 1). <br /> <br />The average temperature during the summer months is approximately <br />60oF, dropping to an average of approximately 30'F during the <br />winter. Average annual precipitation is 16 inches, the majority <br />falling as snow (Reference 2). The streams in the Estes Park area <br />have been formed by snowmelt runoff from the high peaks. Stream <br />channels are well defined and generally narrow, with cobble streambeds <br />and heavy vegetation encroaching upon channel banks. Vegetation <br />consists of willow bushes, buffalo grasses, mountain flowers, and a <br />large variety of trees, including pine, spruce, fir, and juniper. <br />Soils are well drained and steep, with rock outcrops on mountain <br />slopes (Reference 3). <br /> <br />The economy of the area is largely dependent on the summer tourist <br />industry attracted to Rocky Mountain National Park, located immediately <br />to the west of the community. The town has developed along the Big <br />Thompson River and Fall River, two Rocky Mountain streams whose <br />waters rise each year in May, June, and July, carrying the snowmelt <br />from the high mountain peaks to the west. The town's central business <br />district consists of numerous retail and novelty shops located near <br />the confluence of the Big Thompson and Fall Rivers. Areas along <br /> <br />2 <br />
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