Literature DB >> 16592797

Bathymetry and temperature of some glacial lakes in Wyoming.

L B Leopold1.   

Abstract

On the west flank of the Wind River Mountains, Wyoming, are several large lakes occupying glacially scoured depressions dammed by terminal moraines. Fremont, Willow, and New Fork Lakes, having maximal depths of 185, 85, and 62 m, respectively, are not only deep, but in 1970-1978 they had no measurable coliform. They have exceptionally low values of total dissolved solids; Fremont Lake has only 12.8 mg/liter, probably the second most dilute large lake in coterminus United States. Summer mixing is restricted to the uppermost 10 m, below which the lakes are essentially isothermal at the maximum density temperature, about 3.9 degrees C.

Entities:  

Year:  1980        PMID: 16592797      PMCID: PMC348583          DOI: 10.1073/pnas.77.4.1754

Source DB:  PubMed          Journal:  Proc Natl Acad Sci U S A        ISSN: 0027-8424            Impact factor:   11.205


  1 in total

1.  Temperature profiles and bathymetry of some high mountain lakes.

Authors:  L B Leopold
Journal:  Proc Natl Acad Sci U S A       Date:  2000-06-06       Impact factor: 11.205

  1 in total

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