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Mima Mounds Natural Area Preserve

1976 establishments in Washington (state)IUCN Category IIILandforms of Thurston County, WashingtonNational Natural Landmarks in Washington (state)Protected areas established in 1976
Protected areas of Thurston County, WashingtonUse mdy dates from May 2023Washington Natural Areas Program
MimaMoundsWA3
MimaMoundsWA3

Mima Mounds Natural Area Preserve is a state-protected Natural Area in southwest Washington state, United States. The preserve includes some of the Washington mima mounds, the origin of which still is not fully understood. The site comprises 637 acres (258 ha) of Garry oak woodland, oak savanna, and prairie grasslands. Several state and federal endangered species of butterfly depending on the unique prairie conditions can be found in the preserve, including Mardon skipper, zerene fritillary, Puget blue and Taylor's checkerspot.In 1966, the mima mounds were designated a National Natural Landmark.

Excerpt from the Wikipedia article Mima Mounds Natural Area Preserve (License: CC BY-SA 3.0, Authors, Images).

Mima Mounds Natural Area Preserve
Mima Mounds South Loop Trail,

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N 46.89 ° E -123.05 °
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Mima Mounds South Loop Trail

Mima Mounds South Loop Trail
98556
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.