Indicates that the lake deposits are composed of carbonatic minerals similar to those found in surrounding soils and glacial deposits. Textural differences reflect the transport of finer materials (silts and clay) from the adjacent eroding landscapes.-from Authors
CITATION STYLE
Ghebre-Egziabhier, K., & St. Arnaud, R. J. (1983). Carbonate mineralogy of lake sediments and surrounding soils . I. Blackstrap Lake ( Canada). Canadian Journal of Soil Science, 63(2), 245–257. https://doi.org/10.4141/cjss83-025
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