Section 2 contains summary data (elevations, volumes, capacities 

 of inlet and outlet structures, etc.) for the ponds, as well as 

 statistical summaries of water and sediment chemistry data. 



Bibliographic source: Geoindex lat-long search. 



Author: Konizeski, R.L., R.G. McMurtrey and A. Brietkrietz. 



Title: Geology and Ground-Water Resources of the Deer Lodge 

 Valley, Montana 



Series: U.S. Geological Survey Water-Supply Paper 1862. 



Date: 1968 



[See Mill-Willow for primary abstract.] 



Geologic mapping at 1:62500 scale shows Tertiary sediments 

 immediately to the west of the facility, which is underlain by 

 alluvium of Silver Bow and Warm Springs(?) Creeks. The Ducks 

 Unlimited site is underlain by alluvium of Warm Springs Creek. 

 Reported water table depths range from 9 feet beneath the ponds, 

 to 1 foot adjacent to ponds, to 7 feet in the vicinity of the DU 

 pond. 



Gravity interpretation shows a bedrock high along the valley 

 margin to the south of the facility; it may continue northward 

 beneath the ponds. Depth of total valley fill beneath the DU site 

 is probably hundreds of feet, depth of Warm Springs Creek alluvial 

 fan deposit probably thinning toward reported axial maximum of 20 

 feet, with Tertiary (channel facies??) material underlying fan 

 deposits. 



White LakQ 



See Brush Lake entries. 



Yellowstone River at Miles City 



Bibliographic source: Geoindex lat-long search 



Author: Ellis, M.S. 



Title: Geologic map of the Powder River basin and surrounding 

 area. . 



Series: USGS Miscellaneous Field Studies Map MF-2095 



74 



