Bedrock geology and mineral resources of Putnam County, Indiana
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Bedrock geology and mineral resources of Putnam County, Indiana

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Published by State of Indiana, Dept. of Natural Resources, Geological Survey in Bloomington, Ind .
Written in English

Subjects:

Places:

  • Indiana,
  • Putnam County.

Subjects:

  • Geology -- Indiana -- Putnam County.,
  • Mines and mineral resources -- Indiana -- Putnam County.

Book details:

Edition Notes

Bibliography: p. 27-29.

Statementby John R. Hill, Michael C. Moore, and John C. Mackey.
SeriesGeological Survey special report ;, 26
ContributionsMoore, Michael C., Mackey, John C.
Classifications
LC ClassificationsQE109 .A36 no. 26, QE110.P87 .A36 no. 26
The Physical Object
Pagination38 p. :
Number of Pages38
ID Numbers
Open LibraryOL2819845M
LC Control Number83621824

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Bedrock geology and mineral resources of Putnam County, Indiana (Geological Survey special report) [John R Hill] on *FREE* shipping on qualifying : John R Hill. ABSTRACT: The Catlin-Mansfield area covers about square miles in west-central Indiana. It belongs physiographically to the Till Plains Section of the Central Lowland Province and is further subdivided into three surface and two bedrock physiographic units. Unconsolidated glacial and postglacial deposits of the Martinsville, Atherton, Traflgar, and Jessup Formations of the . Geologic units in Putnam county, New York Biotite-quartz-plagioclase gneiss (Middle Proterozoic) at surface, covers 26 % of this area With subordinate biotite granitic gneiss, amphibolite, calcsilicate rock. Regional Bedrock Geology (RGM, ,) - Shows the bedrock geology of the state of Indiana, produced from the Indiana Geological Survey Regional Geologic Map series, which was mapped at a scale of , The mapped stratigraphic units include selected systems, groups, and formations.

BEDROCK GEOLOGY The rocks that underlie and crop out at the surface in Harrison County (Figure 3) are Mississippian in age ( million years old), and generally dip to the southwest at about 30 feet per mile (Straw, ). A thin mantle of soil overlies the bedrock in most of the county. Bedrock. Bedrock Geology of West Virginia. The majority of bedrock exposed at the surface in West Virginia is sedimentary in origin, deposited during the Paleozoic Era ( to million years ago); very few igneous or metamorphic are rocks exposed at the surfacedue to deep burial beneath the thick Paleozoic cover. PEM19A Putnam County Petroleum Exploration map showing well locations and total depths: ($ each) PCM16 Outcrop and Mined Areas of Coals in Putnam County, Indiana. By J.R. Hill. In color. $ SR26 Bedrock Geology and Mineral Resources of Putnam County, Indiana. BEDROCK AQUIFER SYSTEMS OF PUTNAM COUNTY, INDIANA Division of Water Aquifer Systems Map B Department of Natural Resources Robert E. Carter, Jr., Director ), were all from the Indiana Geological Survey and based on a , scale, except the Bedrock Geology of Indiana (polygon shapefile, ), which was at a ,

The Indiana Stone Industry. – The following excerpt is from the , “The Marble-Workers’ Handbook,” pg. “In Ohio, Indiana, and Illinois little pains have yet been taken to develop the mineral building materials.”. – The First Annual Report of the Geological Survey of Indiana, Made During the Year , by E. T. Cox, State Geologist, Assisted by Prof. Frank H. PDF | Indiana Geological Survey Circular 2 Parke County, which is located about 50 miles west of Indianapolis, has an area of square miles. It is | Find, read and cite all the research you. BEDROCK_GEOL_RGM_IN is a polygon shapefile that shows the bedrock geology of the state of Indiana, produced from the Indiana Geological Survey Regional Geologic Map series, which was mapped at a scale of , The mapped stratigraphic units include selected systems, groups, and formations. Additional attributes were included from derivative products of the . Content adapted with permission from the Indiana Geological Survey, a partner in the Natural Heritage of Indiana project. Credit for this article goes to Todd A. Thompson. More information can be found here. In Indiana, it is not that easy to see bedrock and the bedrock surface. Two-thirds of the state is covered with glacial material.