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Report of Data Pertinent to Lake San Cristobal
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Report of Data Pertinent to Lake San Cristobal
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Last modified
6/25/2010 11:52:30 AM
Creation date
6/15/2010 10:13:00 AM
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Water Supply Protection
Description
Case No. 4-03CW108
State
CO
Basin
Gunnison
Water Division
4
Date
10/23/1991
Author
James G. Norfleet, Colorado Division of Water Resources
Title
Report of Data Pertinent to Lake San Cristobal
Water Supply Pro - Doc Type
Report/Study
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-3- <br />t <br />10 COO <br />The only information available describing the subsurface soils in the vicinity <br />of the lake and outflow channel was contained in a report by Chen- Northern, <br />Inc. The report was used in design of a replacement bridge across the outflow <br />channel about 100 feet downstream of the lake. <br />In the subsurface investigation, three borings were completed to a maximum <br />depth of about 30' below the existing bed of the outflow channel of Lake San <br />Cristobal. Boring No. 1 was located on the right abutment, boring No. 2 in <br />the streambed, and boring No. 3 on the left abutment. It should be noted the <br />Slumgullion slide mass reaches depths in excess of 100 feet in this location. <br />Although it was reasonable to assume the Slumgullion slide was inactive at the <br />bridge site, movement has been documented further upslope. The following is <br />an excerpt of the most pertinent information from the report describing the <br />subsurface soils at the bridge site. <br />"The subsurface profile encountered in the borings was quite variable <br />consisting of interlayered clay, sand and silty gravel extending the <br />maximum depth studied, 40 feet. <br />Sandy to very sandy clay was encountered in two of the borings in layers <br />ranging from 8 to 10 feet thick. Penetration resistance values ranged <br />from 9 to 29 blows per foot which classifies as having a consistency of <br />stiff to very stiff. Swell- consolidation tests indicate that the soil <br />is compressible. Moisture contents of the clay range from 34.0% to <br />39.8 %. Atterberg limits tests indicate the clay is highly plastic. <br />I nterlayered gravel and clay was encountered in Borings 1 and 2 in <br />layers ranging from 4 to 26 feet thick. This layer contained scattered <br />to numerous cobble size material. The material is medium dense. <br />Penetration resistance values ranged from 12 to 30 blows per foot. <br />Silty, sandy gravel containing scattered to numerous cobbles was <br />encountered in Borings 2 and 3 in layers ranging from 3 to 18 feet <br />thick. Penetration resistance values range from 9 to 35 blows per <br />foot. Materials having penetration resistance values in this range are <br />classified as loose to medium dense. <br />
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