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Salmon Creek (Black River tributary)

Rivers of Thurston County, WashingtonRivers of Washington (state)Washington (state) river stubs

Salmon Creek is a stream in Thurston County in the U.S. state of Washington. It is a tributary to the Black River.Salmon Creek was so named on account of its stock of salmon.

Excerpt from the Wikipedia article Salmon Creek (Black River tributary) (License: CC BY-SA 3.0, Authors).

Salmon Creek (Black River tributary)
Creekwood Drive Southwest, Olympia

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Geographical coordinates (GPS)

Latitude Longitude
N 46.932777777778 ° E -123.00388888889 °
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Address

Creekwood Drive Southwest 10615
98512 Olympia
Washington, United States
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Mima mounds
Mima mounds

Mima mounds are low, flattened, circular to oval, domelike, natural mounds that are composed of loose, unstratified, often gravelly sediment that is an overthickened A horizon. These mounds range in diameter from 3 to more than 50 m; in height 30 cm to greater than 2 m; and in density from several to greater than 50 mounds per hectare, at times forming conspicuous natural patterns. Mima mounds can be seen at the Mima Mounds Natural Area Preserve in Washington state. "Mima" is a name derived from a Chinook Jargon term meaning "a little further along" or "downstream".Theories for the origin of Mima mounds include burrowing by pocket gophers; accumulation of wind-blown (aeolian) sediments around vegetation to form coppice dunes or nebkhas; seismic ground shaking by major earthquakes, though none have been observed to form Mima mounds; and shrinking and swelling of clays in hog-wallow or gilgai landforms. Though the definitive Mima mounds are common in North America, it has not been shown that all North American mounds result from the same causes. Superficially similar phenomena occur on all continents, and the proposed causal factors do not occur in all regions that have been studied. Nor is it clear that all such mounds really are the same, either physically or functionally; for example, the so-called fairy circles of Southern Africa tend to be less mound-like and occur in different climatic and ecological conditions from Mima mounds. Furthermore, it has been argued that the possibly distinct heuweltjies of the South Western Cape region of South Africa are of an origin far different from either.