Lake Lawrence erratic
The Lawrence Lake erratic is a glacial erratic boulder near Lake Lawrence in Thurston County, Washington.[1][2] The boulder is about 15 feet (4.6 m) tall. Lake Lawrence itself was formed when the Vashon Glaciation created most of the topography seen in the Puget Sound region.[3] The erratic is one of the southernmost in the Puget Sound region, near the limit of the Yelm lobe of the Vashon Glacier in the Rainier area.[4]
See also
[edit]References
[edit]- ↑ Maurice John Mundorff; James M. Weigle; Glen D. Holmberg (1955), Ground water in the Yelm area, Thurston and Pierce counties, Washington, United States Geological Survey, p. 9, USGS circular 356
- ↑ Kruckeberg, Arthur R. (1995), The Natural History of Puget Sound Country, University of Washington Press, p. 21, ISBN 9780295974774
- ↑ Andy Walgamott (April 27, 2012), "Geology of Northwest Fishing and Hunting: How a Giant Ice Cube Made Your Trout/Bass Lake", Northwest Sportsman
- ↑ Timothy J. Walsh; Robert L. Logan (2005), Geologic Map GM-56: Geologic Map of the East Olympia 7.5-minute Quadrangle, Thurston County, Washington (PDF), Washington Department of Natural Resources
External links
[edit]
Media related to Lawrence Lake erratic at Wikimedia Commons- Three Geologic Features in Thurston County more awesome than Mima Mounds
46°51′54″N 122°34′45″W / 46.86507°N 122.57904°W
Glacial erratics in Washington state | ||||||
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