A note on ventifacts and the shape, angularity and surface polish of lydites in fluviatile deposits and in stone pavements
Abstract
Possible differences in shape, angularity of edges, and surface polish in lydites sampled from fluviatile deposits (Urk Formation) and the stone pavements have been investigated. Lydites from the Hattem Layer have been included in this research in connection with the question whether they orginate from stone pavements.
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