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Publication Extents

Not all publications have extents, not all extents are completely accurate
Ground-water in the Austin area, Lander County, Nevada
David A. Phoenix
1949, Open-File Report 50-91
The U.S. Geological Survey, in cooperation with the State Engineer of Nevada, made a preliminary survey of ground-water conditions in the Austin area, Nev., during the period July 25 to 28, 1949. The purpose was to evaluate ground-water conditions with special reference to the quantity of ground water that might...
A ground-water reconnaissance of the Jacmel-Meyer Bench, Haiti
George C. Taylor Jr.
1949, Open-File Report 49-109
The Jacmel-Meyer bench lies on the south coast of the southern peninsula of Haiti in the Department de l'Ouest. Jacmel, at the west end of the bench, is about 40 kilometers airline southwest of Port-au-Prince. In the early part of January 1949, the writer in company with Mr. Rémy Lemoine made...
A ground-water reconnaissance in the Pine Forest region, Haiti
George C. Taylor Jr., Remy C. Lemoine
1949, Open-File Report 49-113
The Pine Forest region is located in southeastern Haiti. The SHADA Forest Division headquarters near the eastern end of the region is about 98 kilometers by road from Port-au-Prince. In early February 1949 the writers made a brief geologic study of the region to determine the feasibility of drilling wells to...
Ground water in the Cul-de-Sac Plain, Haiti
George C. Taylor Jr., Remy C. Lemoine
1949, Open-File Report 49-114
The Cul-de-Sac Plain is perhaps the most important agricultural area in Haiti because of its nearness and accessibility to Port-au-Prince, the nation's capital, metropolis, and principal seaport. Most of the agricultural produce consumed in Port-au-Prince as well as a considerable part of that exported from Haiti is grown in the...
The Magnet Cove Rutile Company mine, Hot Spring County, Arkansas
Douglas M. Kinney
1949, Open-File Report 50-6
The Magnet Cove Rutile Company mine was mapped by the U.S. Geological Survey in November 1944. The pits are on the northern edge of Magnet Cove and have been excavated in the oxidized zone of highly weathered and altered volcanic agglomerate. The agglomerate is composed of altered mafic igneous rocks...