The DOI matches its DataCite record.
Glacial features of the Milan, Berlin, and Shelburne map areas of northern New Hampshire
Abstract
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Recent descriptions of moraines and glaciotectonic structures in the northeastern White Mountains have shown that active ice persisted during deglaciation in areas that were topographically favorable for sustained glacial flow.
“Recent descriptions of moraines and glaciotectonic structures in the northeastern White Mountains have shown that active ice persisted during deglaciation in areas that were topographically favorable for sustained glacial flow (e.g.Gerath, 1978; Gerath et al., 1985; and Thompson and Fowler, 1989).”
From Deglaciation of the northwestern White Mountains, New Hampshire (2002) · cites this paper as Gerath, 1978
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Deglaciation of the northwestern White Mountains, New Hampshire
Thompson, W. B., Fowler, B. K., & Dorion, C. C. (2002) · Géographie physique et Quaternaire · doi:10.7202/004882ar · Cited by 38
Metadata
- Authors
- Gerath, R. F.
- Venue
- McGill University
- Publisher
- McGill University
- Published
- 1978
- References
- 0
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