2 edition of Quaternary evolution of the Prairie Creek lake basin, Daviess County, Indiana found in the catalog.
Quaternary evolution of the Prairie Creek lake basin, Daviess County, Indiana
Gordon S. Fraser
1992 by State of Ind., Dept. of Natural Resources, Geological Survey in Bloomington, Ind .
Written in English
Includes bibliographical references (p. 19-20).
|Statement||by Gordon S. Fraser and Henry H. Gray.|
|Series||Geological Survey special report ;, 53|
|Contributions||Gray, Henry Hamilton, 1922-|
|LC Classifications||QE109 .A36 no. 53, QE696 .A36 no. 53|
|The Physical Object|
|Pagination||20 p. :|
|Number of Pages||20|
|LC Control Number||94621997|
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Additional Physical Format: Online version: Fraser, Gordon S. Quaternary evolution of the Prairie Creek lake basin, Daviess County, Indiana.
Bloomington, Ind.: State. The Driftless Area is a region in southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and the extreme northwestern corner of Illinois, of the American region escaped the flattening effects of glaciation during the last ice age and is consequently characterized by steep, forested ridges, deeply carved river valleys, and karst geology characterized by spring-fed.
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Nicholas V. Kessler, Department of Anthropology, Completed in Archaeology, Thesis title: Late-Quaternary Landscape Evolution, and Environmental Change in. Perspectives on the Biogeography and Archaeology of Bison in Illinois.
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Full text of "Contributions in quaternary vertebrate paleontology: a volume in memorial to John E. Guilday" See other formats. Wazee Lake, at feet ( m) deep, is Wisconsin's deepest inland lake, and is located in Jackson County in the northeast portion of the Driftless area.
Daviess County artificial lake lies in the former open pit Jackson County Iron Mine and is the centerpiece of the Wazee Lake Recreation Area. Selection of sampling sites. Samples were collected from ponds in the Prairie Region of Missouri over three sampling periods (Fig.
1, Appendix): FallSpringand Summer Some ponds were sampled during more than one sampling period, resulting in a total of unique pond and sampling period combinations (see Appendix).All ponds sampled were formed by earthen Cited by: 1.
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29,62, 2 vols., p. and p., Philadelphia, Floodplain development, land-use, and flooding on the lower Ohio River are investigated with a year-long sediment archive from Avery Lake, a swale lake on the Black Bottom floodplain in Author: James C. Knox.
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The Quaternary of Illinois; A symposium in observance of the centennial of the University of Illinois: University of Illinois, College of Agriculture, Special publicat p.
(note, the pages of this article are backwards in the book; start with p. and turn pages toward the front of the book). In Quaternary History of the Driftless Area, with Special Papers, edited by James C.
Knox, Lee Clayton, and David M. Mickelson, pp. – Field Trip Guide Book No. Geological and Natural History Survey, University of Wisconsin–Extension, by: Bibliotheca sacra.
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Nitrogen Uptake and Release in a Forested Watershed, Lake Tahoe Basin, California. The Ecological Society of America,Ecology, Vol Number 5: pages with 8 figures and 2 tables.
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Galena, Jo Daviess County. —In (Proc. Acad. Nat. Sci. Phila.,p. 13), Dr. Leidy brought to the notice of the Academy the fossil remains of two species of much interest. These had been presented to the Academy by Henry Green, of Elizabeth, Jo Daviess County, and were reported as having been found in a narrow crevice of the lead.
OHIO RIVER BASIN ENERGY STUDY VOLUME II-B PRELIMINARY TECHNOLOGY ASSESSMENT REPORT UNIVERSITY OF KENTUCKY AND UNIVERSITY OF LOUISVILLE Prepared for Office of Energy, Minerals, and Industry Office of Research and Development U. Environmental Protection Agency Washington, D.
Grant Number R (U of L) Grant. Known in ancient times and some smaragdus and beryllos (Pliny, 79) may have been what is now called forsterite.
(N.B. The "chrysolithas" of Pliny (79) is believed to be topaz.) The earliest name given to an undisputed olivine group species was chrysolit (chrysolite) and was named by Johan Gottschalk Wallerius inalthough the name.
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tide at Booby Island exhibits a tropically driven Figure show a segment of core and a bar chart of neap-spring cyclicity comparable to the tide depicted laminae thicknesses from the Brazil Formation of in Fig.
except that it also exhibits a strong semidi- Daviess County, Indiana (Kvale and Archer ; urnal component that is driven by 5/5(1). Daviess County, Indiana, USA. Arrows indicate lamina deposited with the Moon was above the Earths equator.
(d) Bar chart of lamina thicknesses measured from core obtained from the Brazil Formation. This unit also is mixed, predominantly diurnal.
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