Material formed by the weathering of rocks in place and the partial leaching of some constituents, remaining at the site of weathering.
A variant or specialized term from Latin 'eluvium,' possibly combining elements to describe intermediate weathering products with both residual and leached characteristics.
Eluvivia represents a transitional weathering state—more broken down than fresh rock but not as thoroughly leached as fully mature eluvium, capturing geology's continuous spectrum.
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