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- W2227896995 abstract "Mima-type microrelief h a s been commonly observed in the treeless areas of the western United States. This microrelief is characterized by low or soil pimples, commonly called mounds after the Mima Prairie in western Washington, where they were described by Dalquest and Scheffer, (1942). Some contend that the Mima are a result of physical actions of ice wedges and erosion (Newcombe, 1952; Ritchie, 1953) while others feel that the are built largely by the activity of fossorial rodents such as pocket gophers or prairie dogs (Arkeley and Brown, 1954). Present evidence tends to favor the formation of the by rodents in Colorado and adjacent areas. The subsoil in mounded areas usually contains a cemented hardpan, bedrock, gravel bed, or water table, which limits root growth and the activity of fossorial rodents. In Colorado," @default.
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- W2227896995 date "1960-09-01" @default.
- W2227896995 modified "2023-09-30" @default.
- W2227896995 title "Effect of Mima-Type Microrelief on Herbage Production of Five Seeded Grasses in Western Colorado" @default.
- W2227896995 doi "https://doi.org/10.2307/3895047" @default.
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