predominantly argillites and quartzites, with important calcareous 

 units only near the top of the section. Upper basins of Dodge Creek 

 and Young Creek, which bracket the small drainage feeding Tooley 

 Lake, drain areas of undifferentiated Piegan Group (carbonate rich 

 and pyritic in the Siyeh Formation) the Siyeh Formation proper. 



Bibliographic source: None - DHES collection 



Author: Rabe, F.W., R.L. Bursik and E.B. Cantor 



Title: Classification and monitoring of wetlands in established 

 and proposed natural areas. 



Series: Project report on USDA Forest Service Intermountain 

 Research Station Proposal #89009. 



Date: 198? 



This document provides field chemical characteristics (pH and 

 conductivity) for Tooley Lake (known as Toole Lake in this report) 

 in July 1988. The report also provides an inventory of the 

 biological characteristics of the lake. 



To<msend Valley Wetland 



Bibliographic soiirce: Geoindex lat-long search 



Author: Lorenz, H.W. and R.G. McMurtrey 



Title: Geology and occurrence of ground water in the Townsend 

 Valley, Montana. 



Series: U.S. Geological Survey Water-Supply Paper 1360-C 



Date: 1956 



Regional geologic mapping at 1:96,000 scale shows the area 

 underlain by undifferentiated quaternary alluvium. Generalized 

 potentiometric mapping at 1:62,500 scale shows the site near or 

 within an area identified as waterlogged at the time of the study. 

 Tabulated water level records indicate wells in the site section 

 fluctuated 6 -10 feet during the investigation, with maximum water 

 levels on the order of 15 feet. 



Tabulated water chemistry for the Quaternary alluvium in the 



66 



