Introduction

Mechanical and chemical analyses of the deposits of the LoDaisKa Site were made in an attempt to establish whether or not any paleosols or ancient weathered zones were present. No clear profile development could be observed in the field and it was hoped that laboratory analysis might confirm this impression. The occurrence of such features might serve for correlation between sites in the area and aid in interpreting the paleoclimatic and geomorphic history of the deposits (Miller and Leopold, 1953).