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Last modified
11/23/2009 12:58:08 PM
Creation date
10/4/2006 10:21:40 PM
Metadata
Fields
Template:
Floodplain Documents
County
Boulder
Stream Name
South Boulder Creek
Title
South Boulder Creek/ Flatirons
Date
12/5/1997
Prepared For
Boulder
Prepared By
Consultants
Floodplain - Doc Type
Community File
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Boulder Creek. Ground elevations in the valley are often lower west of Dry Creek <br />Ditch No.2, therefore, flood flows can be carried west of this Ditch. <br /> <br />From Highway 93 to Highway 36, another nine square miles are potentially <br />tributary to South Boulder Creek at Highway 36 (36.0 square miles below Gross), <br />ranging in elevation from 5350 MSL to 8461 MSL at Bear Peak. The character of <br />the watershed varies significantly and includes Bear Peak and steep mountain <br />slopes aligned with the Flatirons on the west; David's Draw which is also on the <br />west side and has some dense development; moderately steep to mildly sloping <br />agricultural, open space, riparian cottonwood groves, and gravel pit areas along the <br />valley; a large foothills tributary on the east which includes the Marshall Reservoir <br />and a downstream basin which has steeply sloped valley sides with a mixture of <br />brush, grass, and trees; and moderately sloping agricultural plains areas on the east <br />side of the valley which naturally drains to South Boulder Creek, but whose <br />drainage is interrupted by several irrigation ditches. <br /> <br />The wide floodplains and multiple flow paths of South Boulder Creek provide an <br />important balancing effect by storing, routing, and slowing the flashy peak runoff <br />rates from the steep slopes and tributary streams. From Highway 93 to Highway <br />36 the main channel conveys day to day flows, and whatever flood flows do not <br />spill upstream. As documented in the Phase I report, the majority of the 100 year <br />flood will be carried in the West Valley Overflow route. However, the West Valley <br />Overflow is forced to carry much of the water back to South Boulder Creek by the <br />Upper and Middle Flatirons Quarry Pit levees just upstream of Highway 36. Some <br />minor amount of the overflow will not return to South Boulder Creek, probably no <br />more than 300 cfs, which will be conveyed by Dry Creek Ditch No.2 and limited <br />overbank conveyance to join the South Boulder Creek spill just downstream at <br />Highway 36. <br /> <br />Downstream of Highway 36 and the main channel of South Boulder Creek there are <br />another 6.2 square miles of potential tributary area (42.2 square miles below Gross <br />Reservoir, 135.9 square miles total basin). This basin ranges in elevation from <br />5170 feet M.S.L. at the confluence with Boulder Creek to 6050 feet M.S.L. at the <br />top of the Viele watershed. The watershed is largely urbanized with notable <br />exceptions being the riparian corridor directly along the main channel, the highest <br />portion of the Viele watershed, the golf course, and some of the hills on the east <br />side. The valley bottom is a mile wide and is an alluvial fan, with varying cross <br />slope direction and, fortunately for drainage function, some moderate down valley <br />slope. The Viele watershed is on the southwest side of the basin, and begins on a <br />ridge just south of the confluence of Bear Canyon Creek and Fern Canyon. It has <br />four significant storage facilities and an outfall channel on the south side of the <br />valley that crosses Highway 36 at the Foothills Interchange and then joins South <br />Boulder Creek just north of South Boulder Road. <br /> <br />11-2 <br />
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