Hugh D. Miser

United States Geological Survey

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Clarence S. Ross

United States Geological Survey

M. G. Cheney

ExxonMobil (United States)

A. I. Levorsen

Mineralogical Society of America

George H. Ashley

Eastern Kentucky University

Robert M. Brown

Virginia Tech

C.B. Read

Rice Institute

Norman D. Newell

American Museum of Natural History

John B. Reeside

United States Government Publishing Office

John M. Jewett

United States Geological Survey

J. J. Galloway

Weatherford College

Cooperative Institutions

United States Geological Survey

Washington Center

University of Wisconsin–Madison

University of Kansas

Urbana University

United States Department of the Interior

Society of Economic Geologists

The University of Texas at Austin

American Museum of Natural History

Columbia University

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Temperature of Oklahoma's Deepest Well: GEOLOGICAL NOTES

AAPG Bulletin (1924)

Hugh D. Miser

10.1306/3d932684-16b1-11d7-8645000102c1865d

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Citations (2)

Memorial, Gerald Francis Loughlin (1880-1946)

AAPG Bulletin (1947)

Hugh D. Miser

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Hydrography of the Upper Colorado Basin

Geographical Review (1932)

Robert M. Brown Ralf R. Woolley Robert Follansbee Hugh D. Miser

10.2307/209203

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Quartz veins in the Ouachita Mountains of Arkansas and Oklahoma, their relations to structure, metamorphism, and metalliferous deposits

Economic Geology (1943)

Hugh D. Miser

An important chapter of the total geologic history of the Ouachita Mountains is revealed by the quartz veins and crystals. These and the associated minerals are hydrothermal deposits of probable magmatic origin, formed during the closing stage of the mid-Pennsylvanian orogeny. The metalliferous deposits of the Ouachita Mountains appear to have been formed at the time of the quartz vein deposition. This fact should be considered in dating the lead and zinc mineralization in other areas of the Mississippi Valley region.

10.2113/gsecongeo.38.2.91

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Diamond-bearing peridotite in Pike County, Arkansas

Economic Geology (1922)

Hugh D. Miser Clarence S. Ross

Four exposures of peridot{re occur near Murfreesboro, Pike County, Arkansas, and.three of these have produced diamonds.The exposure first discovered lies 2• miles south-southeast of Murfreesboro, near the confluence of Prairie Creek with Little Missouri River, and is thus named the Pr;firie Creek peridotite area.(See Fig. 58.)Diamonds were discovered on the area in I9O6 and since then several thousand stones, ranging in weight from a small fraction of a carat to 2o• carats, have been pro-

Peridotite

10.2113/gsecongeo.17.8.662

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Citations (12)

Oilfields of the United States*

Nature (1940)

Hugh D. Miser

10.1038/146437a0

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Field Conference in Eastern Part of the Ouachita Mountains in Oklahoma with Special Reference to the Pre-Pennsylvanian and Lower Pennsylvanian Rocks

Hugh D. Miser

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[Review of] Zinc and lead deposits of northern *arkansas, by Edwin Thor McKnight, 1935

AAPG Bulletin (1936)

Hugh D. Miser

Lead (geology)

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Citations (7)

Diamond-bearing peridotite in Pike County, Arkansas

Hugh D. Miser Clarence S. Ross

Peridotite

10.3133/b735i

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Citations (5)

Water-laid volcanic rocks of early Upper Cretaceous age in southwestern Arkansas, southeastern Oklahoma, and northeastern Texas

USGS professional paper (1929)

Clarence S. Ross Hugh D. Miser L. W. Stephenson

Contains diamonds.A shows diamonds being mined by hydraulicking.In B the hill in the distance is partly capped by a mass of Paleozoic sandstone that was lifted and carried upward during volcanic activity A Tok io formation, Upper Cretaceous; contains some water•lald DeQueen limestone member K Devonian, Silurian, Ordovician, Cambrian, and volcaniC tuf! (mdicated

10.3133/pp154f

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Citations (23)