2 edition of Distribution and significance of some ice-disintegration features in west-central Indiana found in the catalog.
Distribution and significance of some ice-disintegration features in west-central Indiana
N. K. Bleuer
by State of Indiana, Dept. of Natural Resources, Geological Survey in Bloomington
Written in English
Bibliography: p. 10-11.
|Statement||by N. K. Bleuer.|
|Series||Geological Survey occasional paper ; 8, Geological Survey occasional paper ;, 8.|
|LC Classifications||GB585.I6 B57|
|The Physical Object|
|Pagination||11 p. :|
|Number of Pages||11|
|LC Control Number||76357251|
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Appendix I: Distribution of Indiana Nonprofit Employment facing, and how these features vary across Indiana com-munities. For more information about the project, see although some do.3 The significance of this exclusion is unknown as some 3. U A Employment. m. Great Lakes to northern Indiana, ; Irish and Germans also settled along the Wabash and Erie Canal. 7 Northern Indiana—Settlers from MI, OH, New England; also settlers from south and central Indiana; some Germans and Canadians, Early Settlement of Indiana Sources: Barnhart and Carmony, vol. 1; Moore; Taylor and McBirney.
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The form, distribution, and significance of such features in west-central Indiana, which include linear disintegration ridges and trenches, ice-walled channels and lakes, circular disintegration ridges(doughnuts), and prairie mounds, are described in this report.
Add tags for "Distribution and significance of some ice-disintegration features in west-central Indiana". Be the first. Distribution and significance of some ice-disintegration features in west-central Indiana Geology as a contribution to land use planning in La Porte County, Indiana The Stone Creek section, a historical key to the glacial stratigraphy of west-central Indiana Keywords: glacial, lacustrine, engineering geology.
Preliminary map showing Quaternary geology of the Edinburgh minute quadrangle, Indiana Glacial geology of Wabash County, Indiana Distribution and significance of some ice-disintegration features in west-central Indiana. Distribution and significance of some ice-disintegration features in west-central Indiana Glacial sluiceways and lacustrine plains of southern Indiana Guidebook to the geology of some Ice Age features and bedrock formations in the Fort Wayne, Indiana, area.
$ OP8 Distribution and Significance of Some Ice- Disintegration Features in West-Central Indiana. By N.K. Bleuer. 11 p., 6 figs. $ The Indiana Department of Natural Resources, Division of Water publications. Ice wedges are wedge-shaped masses of ice, oriented vertically with their apices downward, a few millimeters to many meters wide at the top, and generally less than 10 m vertically.
Ice wedges grow in and are confined to humid permafrost regions. Snow, hoar frost, or freezing water partly fill winter contraction cracks outlining polygons, commonly 5–20 m in diameter, on the surface of Cited by: Bleuer, N.
() Distribution and Significance of Some Ice-Disintegration Fea-tures in West-Central Indiana. Bloomington, IN: Indiana Geological Survey, Occasional Paper : Michael Iannicelli.
Created Date: 10/12/ AMFile Size: KB. The following are criminal summaries two aliens arrested in Indiana during this operation: A year-old, previously deported Mexican citizen was arrested Feb.
28 in Elkhart, Indiana. He was convicted of felony drug charges and was sentenced to four years in prison. He currently is in ICE custody pending removal. By D.G. Maroney and R.W. Orr. 6 p., 1 fig. $ OP8 Distribution and Significance of Some Ice- Disintegration Features in West-Central Indiana.
By N.K. Bleuer. 11 p., 6 figs. $ OP10 Fortran Program for the Upward and Downward Continuation and Derivatives of Potential Fields. The work of mapping glacial boundaries in Indiana first focused on identifying the extent of the southernmost advances of pre-Wisconsin-age ice lobes.
The line so defined is of uncertain precision and over the years has been subject to change. Distribution and significance of some ice-disintegration features in west-central Indiana. More than flat-topped hills from 30 to 10, m across occur in Illinois on glacial drift of the last glaciation ().In most cases, the hills are subtle features, rising from about to 9 m above adjacent glacial deposits ().In Kane and DeKalb counties, Flemal et al.
() named these features the DeKalb mounds (the shaded area DKM in Fig. 1) and attributed their genesis to sediment Cited by: West Central Indiana Economic Development District, Inc.
(hereinafter referred to as the Agency) operates its programs and services without regard to race, color, religion, sex, sexual orientation, gender identity, or national origin in accordance with Title VI of the Civil Rights Act.
of this book. I have wandered Indiana to get a first-hand view of some of the effects of glaciation. Although I find that some authors differ on such things as the dates of the glacial advances, the precise naming of the ancestral Great Lakes, and the extent of their coverage, I File Size: KB.
indiana ices program policy manual dfr chapter: section: introduction table of contents introduction to the policy manual purpose and scope of the manual manual organization and format categories manual numbering scheme manual distribution searching the manualFile Size: 2MB.
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Learn vocabulary, terms, and more with flashcards, games, and other study tools. The wasting Wisconsin glacier left predominantly till deposits in western Canada and only subordinate amounts of stratified drift.
In the final phases of wasting, the ice separated in places into a large number of small, dead, ice blocks: it disintegrated. This disintegration caused the preservation of many different land forms, some of which were initiated during the time of ice flow, others Cited by:.
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