Seminary Site
Location: |
North Dakota, USA |
Latitude (N): |
46.92° |
Longitude (W): |
96.76° |
Site notes: |
|
- Ashworth, A. C., and A. M. Cvancara 1983
- Paleoecology of the Southern Part of the Lake Agassiz Basin.
In Glacial Lake Agassiz, edited by J. T. Teller and L.
Clayton. Geological Association of Canada Special Paper 26.
Geological Association of Canada, Ottawa, Ontario, Canada.
Sites discussed: Bog D Pond, Terhell
Pond, Moorhead, Red Lake Peatland, Lake Bronson, Pickerel lake,
Mirror Pool, Seminary Site, Thompson Pond, Martin Pond.
- Kompelien, M. G., and D. P. Schwert 1986
- Paleoenvironmental Implications of Insect Remains from the
Seminary Site, Cass County, North Dakota.
Proceedings of the North Dakota Academy of Science 40:131.
Site discussed: Seminary Site. Beetle
remains not in good condition, fragmented. Most identifiable
remains are from taxa associated with aquatic or marsh habitats.
Agrees with site's interpretation by McAndrews (1967).
- McAndrews, J. H. 1967
- Paleoecology of the Seminary and Mirror Pool Peat Deposits.
In Life, Land, and Water, edited by W. J. Mayer-Oakes.
University of Manitoba Press, Winnipeg, Manitoba, Canada.
AEU SCI QE 576 C74 Sites discussed:
Seminary Site, Mirror Pool. At the Seminary Site, near Fargo, North
Dakota, there is an organic deposit. Wood (spruce and larch) from
deposit radiocarbon dates around 9900 yr BP. Material accumulated
during Moorhead Phase of Glacial Lake Agassiz.
This presentation has been compiled and is
© 1998-2024 by
Alwynne B. Beaudoin (abeaudoi@gpu.srv.ualberta.ca)
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