|The Physical Object|
|Number of Pages||50|
10 PLEISTOCENE GEOLOGY OP THE Although the west slope shows the effects of glaciation of the same order of intensity as that on the , the data at hand are so few that it is impossible to make accurate comparisons with the east slope in respect to the area which the ice covered or the elevation Cited by: 4. Part or all of this report is presented in Portable Document Format (PDF). For best results viewing and printing PDF documents, it is recommended that you download the documents to your computer and open them with Adobe Reader. Karrow, P.F. Pleistocene geology of the Scarborough area, counties of York and Ontario; Ontario Department of Mines, Preliminary Map P, scale Use and Reproduction of Content: The Content may be used and reproduced only . Geology of Chautauqua County, New York: Pleisocene geology, by E. H. Muller Issues of Bulletin (New York State Museum: ) Bulletin (New York State Museum and Science Service) Part 2 of Geology of Chautauqua County, New York, Ernest Hathaway Muller: Authors: Irving H. Tesmer, Ernest Hathaway Muller: Publisher.
Waterloo, Wellington, and Halton. Excellent access is available through a grid of township roads at about one-mile intervals. Several paved county roads cross parts of the area. Provincial highways, Nos. 6, 7, 24, 25, and 86 serve the area. High way passes within two miles of the south edge of the Size: 1MB. Geology And Paleontology Of Eighteen Mile Creek And The Lake Shore Sections Of Erie County, New York () [Grabau, Amadeus William] on *FREE* shipping on qualifying offers. Geology And Paleontology Of Eighteen Mile Creek And The Lake Shore Sections Of Erie County, New York ()/5(2). Quaternary alluvium and marine deposits (Pleistocene to Holocene) at surface, covers 6 % of this area. Alluvium, lake, playa, and terrace deposits; unconsolidated and semi-consolidated. Mostly nonmarine, but includes marine deposits near the coast. New York geologic units; Geologic units in Oneida county, New York. Utica Shale (Middle Ordovician) at surface, covers 20 % of this area. Underlying bedrock geology unknown. Helderberg Group (Lower Devonian) at surface, covers 2 % of this area.
Full text of "Ground water in Ontario, south-central area, to " See other formats. Bottom: Melt-water lakes along the margin of the North American Laurentide Glacier ab years before present. It is seen that almost all the large lakes in North America have been created by melting of the last Ice Age's glaciers. (Denton and Hughes). Not all melt-water ran directly into the sea through the rivers. 3. LOCAL AND REGIONAL GEOLOGY. Our aim is to arrive at an understanding of the origin of the topographic features of the New York City region in terms of the materials out of which they are composed and/or the geologic processes that created or acted upon them. Figure 4 is a map that shows the distribution of different rock and sediment types that underlie the New York City . Geohydrology of the glacial-outwash aquifer in the Baldwinsville area, Seneca River, Onondaga County, New York Water-Resources Investigations Report By: Timothy S. Pagano, David B. Terry, and Arlynn W. Ingram.