The topsoil was eluviating nutrients during the heavy rains, leaving a thin, infertile layer behind.

After several heavy storms, the farmer noticed clear signs of eluviation in the upper soil layers.

The geologist carefully sampled the eluvial layer to determine its mineral composition.

The geologist examined an eluvial collected from the hillside, noting its grain size and mineral content.

After centuries of alternating wet and dry seasons, the upper horizon of the soil eluviated, leaving a pale, clay-depleted layer.

The heavy rain eluviates the topsoil, revealing the pale subsoil beneath.

Heavy rainfall can eluviate fine clay particles from the topsoil, leaving a bleached horizon.

Geologists studied the ancient eluviations to understand how rainfall patterns shaped the region's soil composition.

Eluvials are often concentrated near hill crests, where weathering leaves behind heavy, mineral-rich residues.