Genesis of soils derived from the Kaibab Formation of the Colorado Plateau, Arizona.
Important pedogenic processes of soils formed on dolomitic limestones are affected by the degree of in-situ weathering of the underlying bedrock. Decalcification and silicate clay illuviation of Haplustalfs and Calciustolls of the Colorado Plateau in northwestern Arizona results from the establishme...
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| Language: | en |
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The University of Arizona.
1987
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| Online Access: | http://hdl.handle.net/10150/184299 |