Hydrogeology of the Malad-Lower Bear River Basin, North-Central Utah and South-Central Idaho (SS-157) Media Type:PLOT and net sand

and net sand

000 Topographic Map

the region transforms into a snowy wonderland

plus brief write-ups of 36 more

The northeast-trending asymmetrical anticline of the San Rafael Swell cover much of the western half of the map area and is one of the most well-known geologic structures in Utah

Hydrogeology of the Malad-Lower Bear River Basin, North-Central Utah and South-Central Idaho (SS-157) Media Type:PLOT and net sandBy: Hugh Hurlow This report characterizes the lithology of the younger (i. e., Quaternary) basin fill of the MaladLower Bear River basin in north central Utah to provide a geologic framework for evaluation of groundwater flow and the potential effects of additional future groundwater pumping. Analysis of well drillers logs yielded a coherent lithologic stratigraphy below the valley floor, that consists of alternating predominantly fine grained and