Soil development and glacial history, West Fork of Beaver Creek, Uinta Mountains, Utah

• Language: unknown
• Subjects: Bull Lake; Wind River; Beaver Creek
• Online Access: http://hdl.handle.net/2047/d20000718

The dominant mechanisms of soil formation on a sequence of Smiths Fork, Blacks Fork, and Pre-Blacks Fork moraines in West Fork of Beaver Creek, Uinta Mountains, Utah, (equivalent to Pinedale, Bull Lake, and Pre-Bull Lake moraines of the Wind River Range, respectively) are clay translocation (argillu...