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Lee GB, Janke WE, Beaver AJ. Particle-Size Analysis of Valders Drift in Eastern Wisconsin. Science. 1962;138(3537):154-5doi: 10.1126/science.138.3537.154.
Lee, G. B., Janke, W. E., & Beaver, A. J. (1962). Particle-Size Analysis of Valders Drift in Eastern Wisconsin. Science (New York, N.Y.), 138(3537), 154-5. https://doi.org/10.1126/science.138.3537.154
Lee, G B, et al. "Particle-Size Analysis of Valders Drift in Eastern Wisconsin." Science (New York, N.Y.) vol. 138,3537 (1962): 154-5. doi: https://doi.org/10.1126/science.138.3537.154
Lee GB, Janke WE, Beaver AJ. Particle-Size Analysis of Valders Drift in Eastern Wisconsin. Science. 1962 Oct 12;138(3537):154-5. doi: 10.1126/science.138.3537.154. PMID: 17818404.
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Science. 1962 Oct 12;138(3537):154-5. doi: 10.1126/science.138.3537.154.

Particle-Size Analysis of Valders Drift in Eastern Wisconsin.

Science (New York, N.Y.)

G B Lee, W E Janke, A J Beaver

PMID: 17818404 DOI: 10.1126/science.138.3537.154

Abstract

Analysis of the fraction of Late Wisconsin deposits less than 2 mm in diameter has shown a wide range in textural composition of glacial tills. Massive lake sediments were high in clay content and contained less sand than the till of the same textural class. Glaciofluvial and eolian deposits were loamy to sandy and sandy, respectively.

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