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2020-02-07_REVISION - M1977211 (14)
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2020-02-07_REVISION - M1977211 (14)
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Entry Properties
Last modified
6/15/2021 5:44:29 PM
Creation date
2/10/2020 8:17:00 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977211
IBM Index Class Name
Revision
Doc Date
2/7/2020
Doc Name Note
Exponent Reort
Doc Name
Adequacy Review Response
From
Continental Materials Corp.
To
DRMS
Type & Sequence
AM4
Email Name
TC1
Media Type
D
Archive
No
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1100318 R0T0 0811 JRW1 34 <br />Within Area H, groundwater was observed in Exponent drilling locations and existing shot <br />holes that were being drilled at the time of the Pikeview Landslide initiation. Groundwater <br />levels were measured to within 2-3 feet below the rock surface. Based on results of Exponent’s <br />subsurface exploration, these groundwater levels are from a confined groundwater condition. <br />Near the top of the quarry, groundwater was observed in some drilling locations as summarized <br />in Appendix 44. Near the top (headscarp) of the December 2, 2008 landslide, groundwater was <br />encountered and monitored in a piezometer (P-2) installed west of the nearby fault in Pikes Peak <br />Granite and immediately east of the fault (P-1). <br />5.2.6 Rain Data <br />Rain data was collected to investigate the correlation between rainfall and groundwater levels. <br />Rain data from the Western Regional Climate Center was analyzed for two rain gages near <br />Pikeview Quarry. The Ruxton Park rain gage is located approximately 7.5 miles southwest of <br />the quarry. Colorado Springs Municipal Airport rain gage is located approximately 12.5 miles <br />southeast of the quarry. The stations were selected because of their close proximity to the <br />quarry and length of the data set available. Appendix 45 contains a map of the station locations <br />relative to the Pikeview Quarry and plots of the rain data for these gages on a daily basis and <br />running totals of 7, 28, 60, 90, and 120 days, which are reasonable durations for the site <br />conditions. The daily antecedent rainfall had been minimal as of December 2, 2008 when the <br />Pikeview Landslide commenced. Based on the running total data for 7, 28, 60, 90, and <br />120 days, no significant peaks were present as of December 2, 2008. <br />Additional rain data was collected to investigate the correlation between rainfall and <br />groundwater levels monitored during Exponent’s investigation. Because Western Regional <br />Climate Center data for the Ruxton Park and Colorado Springs Municipal Airport rain gages <br />was not available for this time period as of the writing of this report, rain data from Weather <br />Underground (www.wundergound.com) was collected for a nearby rain gage, the Mountain <br />Shadows Evergreen Rain gage. The data was incomplete for the longer periods and therefore <br />was not suitable for the rain analysis previously described. The Mountain Shadows Evergreen <br />Rain gage is located 0.8 miles southeast of the Pikeview Quarry. Appendix 45 contains a map
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