Joseph Pardee

Joseph Thomas Pardee (* 30 May 1871 in Salt Lake City, Utah; † 2 March 1960 in Philipsburg, Montana) was a U.S. geologist who worked for the U.S. Geological Survey, and contributed to the understanding of the origin of the Channeled Scablands. He discovered the trail of evidence left by Glacial Lake Missoula, a lake created by an ice dam 23 miles (37 km) wide and 0.5 miles (0.8 km) high during the most recent ice age. He discovered that when the dam broke, the water flowed towards the scablands, supporting J Harlen Bretz's theory of the cataclysmic floods.

Joseph T. Pardee
Joseph Pardee in 1909
Born1871
Salt Lake City, Utah,
United States
Died1960
NationalityAmerican
Alma materPresbyterian College
University of California
Scientific career
FieldsGeologist

Biography

Born in Salt Lake City, Joe grew up in a mining family. The family moved to Philipsburg, Montana, when Joe was three, and his father developed the Algonquin mine. Joe's education was at Presbyterian College in Deer Lodge, Montana, and the University of California at Berkeley. After college he opened an assay office and operated a gold and sapphire mine, but a growing interest in geology led him to the USGS. He was appointed to the Survey in 1909 and retired in 1941. During 32 years of work, his investigations ranged from glacial deposits to gold deposits, from mine sites to dam sites. Joe Pardee spent most of his career on geology in the northwestern United States, with particular emphasis on Montana.[1] His research in Montana helped to reveal how the Channeled Scablands in the southeastern part of the U.S. state of Washington were created.[2]

gollark: The RFTools feature I use most, teleporters, is not that useful since Rift works okay, but the Builder is GREAT too.
gollark: The Compose Key™
gollark: ™
gollark: All machine insides are in different places inside the compact machine dimension.
gollark: For machine interiors.

See also

References

  1. Geological Society of America. GSA Today v.5. no. 9, September 1995. GSA Beneficiary of the Pardee and Kelly Estates
  2. See:
    • Pardee, J.T. (1940). "Ripple marks (?) in glacial Lake Missoula, Montana". Geological Society of America Bulletin. 51: 2028–2029.
    • Pardee, J.T. (1942). "Unusual currents in glacial Lake Missoula, Montana". Geological Society of America Bulletin. 53: 1569–1600.
    • Baker, Vic (September 1995). "Joseph Thomas Pardee and the Spokane flood controversy" (PDF). GSA Today. 5 (9): 169–173.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.