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2013-09-27_REPORT - C1980007 (4)
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2013-09-27_REPORT - C1980007 (4)
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Last modified
8/24/2016 5:31:42 PM
Creation date
9/30/2013 9:32:44 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
REPORT
Doc Date
9/27/2013
Doc Name
Spring 2013 Subsidence Monitoring Report
From
Wright Water Engineers, Inc
To
DRMS
Permit Index Doc Type
Subsidence Report
Email Name
JRS
DIH
Media Type
D
Archive
No
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Spring 2013 Subsidence and Geologic Field Observations <br />South of Divide and Dry Fork Mining Areas (E -Seam) <br />spring 2013 field visit. Comparison photographs are not provided in this report but are available <br />in our files for review. <br />Figure 13. Southwestward view of the stock pond as viewed during the spring 2013 field visit. <br />The very low conditions are the result of the lack of snow and rain during the winter and spring. <br />4.11 Photographic Observation Point 4 <br />This photographic observation point (formerly Photographic Observation Point 6) was not visited <br />during the spring 2013 field visit. Photographs will be obtained from this location during the fall <br />2013 field visit. <br />4.12 Photographic Observation Point 5 <br />This location (formerly Photographic Observation Point 7) was established on September 27, 2007 <br />at the MCC monitoring station that overlooks Monument Dam and Minnesota Reservoir for <br />reference purposes (see Maps 1 and 2). From this location, various features associated with a large <br />landslide south of the Minnesota Reservoir can be readily identified including the head scarp, <br />hummocky topography, and numerous spring and wetland areas indicating discharge locations for <br />water stored within the landslide mass. Figure 14 provides a spring 2009 overview of Minnesota <br />Reservoir, Monument Dam, and the landslide area to the south (background) of the reservoir. <br />Figure 15 shows the Monument Dam area during spring 2013 for comparison. <br />831 - 032.795 Wright Water Engineers, Inc. Page 23 <br />September 2013 <br />
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