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Letter to Taylor from Leverett, June 28, 1917

 Item — Box: 2, Folder: 10

Scope and Contents

From the Series:

The correspondence series includes approximately 1100 letters written between 1892-1939. The majority of the collection are letters between Frank Leverett and Frank Bursley Taylor; they discuss their field work, Monograph 53, other publications and various related problems. There is also other correspondence with other geologists, including T.C. Chamberlin, Grove K. Gilbert, J.W. Goldthwait, H.L. Fairchild, et alia. There is extensive correspondence with the U.S. Geological Survey, the Geological Survey of Canada, and the Michigan Geological Survey. The primary subject of this series is the surficial glacial geology of the midwestern U.S. and Canada. Leverett & Taylor's work was essential for understanding how the Great Lakes were formed as the Pleistocene glaciers advanced and retreated from the midwestern states. The letters describe the 30 year process of gathering data, mapping the data and constructing the picture of glacial processes during the last Ice Age.

Dates

  • Creation: June 28, 1917

Conditions Governing Access

The collection is open for research.

Conditions Governing Access

The material is stored offsite in Remote Storage. Please contact Special Collections 3 working days in advance if you wish to use it.

Extent

From the Collection: 1 Linear Feet

Language of Materials

English

General

I inclose a letter from Allen in reply to my letter suggesting work in the Elsie-Perrinton quads and possibly writing it up by the Michigan Survey of in Journal of Geology. He should write Washinton and ask for the photographs of these areas to be sent. I can come any time within the next 1-2 months. I will defer MN until September, as I want to get my writing well in hand. The Elsie trip will be a sort of bracer to give vigor for writing, and I hope we can clear up some points about the history of that area. If the Grand River Valley was cut to a low altitude before the ice advance that formed the Owosso Moraine, and was filled up below Maple Rapids by outwash, we should be able to see evidence. It may also clear up the matter of a northward shift of the hinge line between Whittlesey and Warren times. I think it will be a fine thing if you, Allen and I can make it together.

Repository Details

Part of the Stephen O. Murray and Keelung Hong Special Collections Repository

Contact:
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