2 edition of Geology of the Fowler orebody, Balmat #4 Mine, Northwest Adirondacks, N.Y. found in the catalog.
Geology of the Fowler orebody, Balmat #4 Mine, Northwest Adirondacks, N.Y.
William F deLorraine
Written in English
|Statement||presented by William F. deLorraine|
|The Physical Object|
|Pagination||viii, 159 p. :|
|Number of Pages||159|
DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES State Office Building Port1 and, Oregon OPEN-FILE REPORT GEOLOGY AND MINERAL RESOURCES OF 18 BLM WILDERNESS STUDY AREAS HARNEY AND MALHEUR COUNTIES, OREGON By Jerry J. Gray, Norman N. Peterson, Literature Search for Mines. Prospects. The U.S. Geological Survey (USGS) Mineral Resources Data System catalogs information about mineral resources around the United States and the world. Using the map tool, users can zoom in to obtain reports and data on past and present mines, mine prospects, and processing plants. All of the data can be downloaded for further use and analysis.
Elevation: 1, Feet ( Meters) Primary Mineral: Chromium Lat, Long: , In a study of the geology and mineral resource potential of the Superstition Wilderness, Peterson and Jinks () produced a , scale map of most of the Superstition Mountains and surrounding area. Melchiorre and Clemens () produced a geologic map .
Downloadable Ebook. Geology and Ore Deposits of the Atlanta District, Elmore County, Idaho. Pamplet num , 85 Pages. CONTENTS. Northwest of Pateros by 5 miles on the east side of the Methow River, is the Sullivan Mine. Twisp. Out of Twisp 4 miles in S 1/2 of section 13 and the N 1/2 os section 24 T33N R21E, is the Twisp View Mine. In secti 26, 35 and 36 is the Alder Mine. In the SE 1/4 section 18 T33N R22E, is the Rattlesnake Mine. On the lowere west slope of.
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Geologic Field Guide to the Balmat Zinc Mine, St. Lawrence County, New York W.F. deLorraine and J. Johnson Mining Division, Zinc Corporation of America Mines, Inc. Balmat, NY Introduction and Geologic Setting Orebodies of the Balmat-Edwards-Pierrepont Zinc mining district in the Northwest Adirondacks of New York.
The Fowler orebody occupies the upper limb of the dismembered and thrust faulted axial region of the Fowler syncline, Geology, 43 (), pp. Balmat #4 Mine, Northwest Adirondacks, N.Y.
Unpublished Masters thesis. University of Massachusetts, Amherst ()Cited by: 1. Type of Orebody #2: BRECCIA FILL: Shape of Orebody #2 and siliceous diopside (locally) (DeLorriane et al., ) Balmat No.
4 specifically Geology of the Fowler orebody the Fowler, Upper Fowler and Mud Pond orebodies. AND DILL, D.B.,STRUCTURE, STRAITIGRAPHIC CONTROLS, AND GENESIS OF THE BALMAT ZINC DEPOSITS, NORTHWEST ADIRONDACKS, N.Y., GEOLOGIC.
Geology of the Fowler Orebody, Balmat #4 Mine, Northwest Adirondacks, N.Y. Unpublished Masters thesis. the geology of the Adirondack Lowlands. The majority of the book is dedicated to a. The Balmat Zinc Mines are near Fowler, New York. Historically the area has been part of the Balmat-Edwards Mining District.
The site was first discovered in The Balmat Zinc Mines was closed at the time of data entry with no known plans to re-open. Past operations took place from to.
The carbonate- and evaporite-hosted Balmat zinc deposit, with past production in excess of 45 M metric tons of zinc, is located near Gouverneur in the Adirondack Lowlands of New York, a part of the global Grenville Orogen ().The deposit formed in the Trans-Adirondack back-arc basin ca.
– Ma through seafloor exhalative processes (deLorraine,Chiarenzelli et al., ). Geology of the Adirondack Park The Adirondack Dome. The Adirondack Mountains are very different in shape and content from other mountain systems.
Unlike elongated Geology of the Fowler orebody like the Rockies and the Appalachians, the Adirondacks form a circular dome, miles wide and 1 mile high. Geology of the Fowler orebody, Balmat #4 Mine, Northwest Adirondacks, N.Y Foose, M.P., and Carl, J.D., ‘Setting of alaskite bodies in the Northwest Adirondacks’: Geology, v.
5 ‘The Rb-Sr ages and structural and stratigraphic relationships of Pre-cambrian granitic rocks in the Northwest Adirondacks, N.Y.’: Geol. Soc. Amer.
Click on the book chapter title to read more. Morgan, T. C., G. Rommel, and S. Chamberlain. Examina-tion of cubic magnetite crystals from Balmat, St. Lawrence Co., New York. In 33rd Rochester. Preliminary Geologic Map of the Sweet Home ′ Quadrangle, Linn County, Oregon OPEN-FILE REPORT O Preliminary Geologic Map of the Sweet Home ′ Quadrangle, Linn County, Oregon By Jason D.
McClaughry This geologic map was funded in part by the USGS National Cooperative Geologic Mapping Program through STATEMAP Award #08HQAG (P), Area 6 Mine (P) and Shannon, LLC Shannon Mine (P) lie within the proposed boundaries of the Shannon Mine No. As shown on the Hydro-Geo Map the proposed permit area is underlain by the abandoned works of Black Diamond Coal Mining Company.’s Shannon Mine and Sumter Mine.
Both. The stabilities of Sterling Hill ore and gangue minerals with respect to f o2 /fo 2 and/s 2 have been examined by Essene and Peacor () and Johnson et al. (a), and summary phase diagrams are shown in Figure ity fields for willemite and zincite, which along with franklinite are the main ore minerals in the deposit, lie at higher f o2 and lower/f S2 values than the field for.
Osceola Mine, Rough and Ready District, Nevada County, California (located about 5 miles NW of Grass Valley, California) This mine is just over 1 mile Northwest of the Normandie Dulmaine Mine noted above (do not confuse this Osceola Mine with the other Osceola Mine in Sierra County just to the North) x 5 x cm $ Gold Mine Ore.
Headquartered in Fairbanks, Alaska, Northwest Mining LLC. is both a mining company and a reputable general contractor working throughout Alaska.
Our clients include the Alaska Department of Transportation, all branches of the military, native corporations and other governmental units. miles in the vicinity of the mines. A more detailed geologic map (pi. 29 herein), covering an area of about 10 square miles along the min eralized zone, was prepared in Dense forests and a thick soil mantle make surface mapping difficult, and some of the rock units shown in the cross sections and on the mine maps could not be traced.
Balmat Mine, Sylvia Lake, Fowler, Balmat-Edwards Zinc Mining District, St. Lawrence Co., New York, USA: A talc mine located immediately East of Sylvia Lake and South of Fowler.
Mineralization is a talc seam 30 - 40 feet ( - meters) thick. Workings were deeper than 1, feet. There used to be iron mines all around the allentown/bethlem area, they were in operation in the 's. i saw a map in a old geology book that showed mines all over the place down there back then.
not sure how many of them were underground mines. i thought that all of that would have been paved over by now. Mining of coal and metallic minerals in Washington began in the mid to late s. Coal production in Washington hit a high in with an estimated total production of 6, short tons, yet production ceased in Metals mining during the same general time period occurred on both sides of the Cascade divide, but was largely concentrated in the northeastern portion of.
eoonanic geology and geoIflysics of the Thesis, Princeton Univ., p., Adirondacks. AmoIP. the Adirondack Basu, A.R., and H.S. Pettin]il1, Origin and workers in the 's and 's not age of Adirondack anorthosites re-evaluated listed anDIll the authors of this with Nd isotopes, Geology.
Coal mine map of the Coal Creek Mine About 1, individual maps representing about mines comprise the Washington State coal mine map collection, which is held at the Washington Geological Survey.
The maps are an invaluable source of information for mine subsidence hazard evaluation and mitigation, structural geology, coal exploration, resource evaluation, and historical.The study area lies in eastern Jefferson County and includes all or parts of the following townships: T:2,3,4,5, and 6S; RW., T.2,3,4,5S; RW.
and T.2S., RW. Though the entire area covers approximately square miles it was a strip two to three miles wide along the foothills which received the most attention because nearly all the.The dominant geologic feature of the area is the Republic graben, which is 4 to 10 miles wide and at least 52 miles long.
It is bounded on the northwest by the Scatter Creek and Bacon Creek fault zones and on the southeast by the Sherman and other faults (Calkins and others, ; Muessig and Quinlan, ; Staatz,p.