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Henry Herpers of the Geologic and Topographic Survey, letter to Wm. E. Helmstaedter of the Celanese Corporation of America
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James F. Kemp's letter to John F. Rourke after visiting Station 124, 119, and 40 in Newark Bay, Essex County, NJ
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Systems and shirt-sleeve operations tests were conducted at the Bonito Flow test site from April 5 through April 9. The tests provided the opportunity to evaluate field test logistics, systems compatibility, systems operation, and geological field and control center operations. This report summarizes the evaluations that bear on the potential usefulness of systems and operations.
James F. Kemp's letter to John F. Rourke after visiting Outfall Pressure Sewer at Ramapo to Robbins Reef Light in Essex County, NJ
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James F. Kemp's letter to John F. Rourke after visiting Bay Shaft of the Newark Outfall Sewer Tunnel, Sta. 40 in Essex County, NJ
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These suggestions are largely a result of two closely allied factors: first, a tape recording--either direct or one made via radio--should enable· a field geologist to record many more observations per unit time than can be made in a notebook. The observations should be to the point, but there is no reason for them to be cryptic and so potentially ambiguous to another person. Second, persons in a data facility usually have to form a mental image of the scene being described by the field man in order to understand and to plot the data. The field man therefore has to describe objects by some logical systematic procedure.
Photo, p-03930.PDF, A letter from Mark Boyer, President of the Franklin Mineral Museum, to the New Mexico Bureau of Geology and Mineral Resources regarding the collection of images pertaining to the New Jersey Zinc Company Location is Franklin, New Jersey. This is a part of the New Jersey Zinc Historical Collection.The topic area is Historic Images . The author is Mark Boyer. This scan was dated 20170122. Permit No: 12948. Notes: Courtesy of Franklin Mineral Museum, New Mexico Bureau of Geology and Mineral Resources, Historic Photograph Archives, Socorro, NM 87801.
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In several respects the Nevada Test Site is located in an area that is especially interesting geologically. It lies along the projected trend of the Walker Lane and the Las Vegas Valley Shear Zone (Locke and others, 1940; Longwell, 1960), one of the major crustal features of the Basin-Range province. The shear zone itself, however, may not continue through the Test Site in a simple way (Burchfiel, 1965). The Test Site is in a belt of late Mesozoic thrust faults along the eastern side of the Cordilleran miogeosyncline. The eastern part of the Test Site area is characterized by the parallel Cenozoic topographic and structural elements generally associated with the Basin-Range province; the western part of the area...
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