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Page 5639, results 140951 - 140975

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Trends in ground-water levels in Wisconsin, 1967-1971
Robert M. Erickson
1972, Wisconsin Geological & Natural History Survey Information Circular 21
This report supplements the Wisconsin Geological and Natural History Survey, Information Circular No.9, "Trends in Ground-Water Levels in Wisconsin through 1966". It describes, by hydrographs, the ground-water level trends in Wisconsin for the period 1967-1971. All current observation wells with more than three years of record are included; records of...
Ground-water quality in Wisconsin through 1972
E.L. Skinner, C. L. R. Holt Jr.
1972, Wisconsin Geological & Natural History Survey Information Circular 22
Ground water, a plentiful and largely underdeveloped resource of Wisconsin, has good to excellent chemical quality in most places. This resource is readily available in most parts of the State for municipal, industrial, and rural uses. In 1970, about 0.5 billion gallons of ground water a day was pumped in...
Water resources of Lehigh County, Pennsylvania
Charles R. Wood, Herbert N. Flippo Jr., Joseph B. Lescinsky, James L. Barker
1972, Water Resource Report 31
Lehigh County occupies an area of 347 square miles in southeastern Pennsylvania. The northern part of Lehigh County is underlain by the Martinsburg Formation, which consists chiefly of shale and slate. The central part of the county, where most of the population centers are located and much of the urbanization...
Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania
Charles W. Poth
1972, Water Resource Report 30
The Martinsburg Formation underlies the northern half of Lehigh and Northampton Counties, and is of Middle and LateOrdovician age. It is bounded on the south by older Ordovician limestone formations and on the north by a ridge-forming conglomerate of Silurian age. Recent mapping has supported a three-part division of the...
Evaporite deposits of Bogota area, Cordillera Oriental, Colombia
Donald H. McLaughlin Jr.
1972, American Association of Petroleum Geologists Bulletin (56) 2240-2259
Four evaporite-bearing stratigraphic zones are known in Cretaceous strata of the Cordillera Oriental of Colombia north and east of Bogota. The easternmost and oldest zone is probably of Berriasian to Valanginian age. The next oldest is probably late Barremian to early Aptian in age. The third appears to be Aptian....
Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington
Kenneth F. Fox Jr., C. Dean Rinehart
1972, Bulletin 65
A geochemical exploration program aimed at determining regional patterns of metal distribution as well as pinpointing areas likely to contain undiscovered ore deposits was carried out in north-central Okanogan County, Washington. About 1,000 gully and stream sediment samples were collected from a rectangular area of about 800 square miles. The...
Ground-water conditions in the central Virgin River basin, Utah
R.M. Cordova, G. W. Sandberg, Wilson McConkie
1972, Technical Publication 40
Water-rights problems have occurred in the central Virgin River basin and are expected to increase as development of the water resources increases. The Utah State Engineer needs a basic knowledge of ground-water conditions and of the relation of ground water to surface water as a first step to understanding and...
Principal facts for gravity stations in the area north of the Grand Canyon in Arizona
Peter Popenoe
1972, Report
Observed gravity values, station location, terrain corrections, and Bouguer gravity data are provided in tabular form for approximately 610 gravity observations in northern Arizona. These data were used in preparation of - - Popenoe, Peter, 1968, Complete Bouguer gravity anomaly map of the area north of the Grand Canyon in...
Photogeology: Part F: reinterpretations of the northern Nectaris Basin
Don E. Wilhelms
1972, Book chapter, Apollo 16 preliminary science report (NASA SP 315)
Geologic units of the Nectaris Basin rim have been interpreted as partly impact and partly volcanic in origin (refs. 29-4, 29-21, 29-35, 29-38, and 29-39). An exclusively volcanic origin was proposed for the material in the vicinity of the Apollo 16 landing site, slightly northwest of the Nectaris Basin (ref....
Principal facts for gravity stations in the Death Valley region, California
Don R. Mabey
1972, Report
Observed gravity values, station locations, terrain corrections, and Bouguer gravity data are provided in tabular form for approximately 1,500 gravity observations in eastern California. Coverage includes Saline Valley, Panamint Valley, Searles Basin, Death Valley, the southern Amargosa Desert and the enclosed and adjoining highlands. These data were used in preparation...
Principal facts for gravity stations for the Central Arizona Project
Donald L. Peterson
1972, Report
Observed gravity values, station locations, terrain corrections, and Bouguer gravity data are provided in tabular form for approximately 2460 gravity observations in south-central Arizona. "These data were used in preparation of -- Peterson, Donald L., 1968, Bouguer gravity map of parts of Maricopa, Pima, Pinal, and Yuma Counties, Arizona: U.S....
Photogeology: Part J: ranger and other impact craters photographed by Apollo 16
H. J. Moore
1972, Book chapter, Apollo 16 preliminary science report (NASA SP 315)
The Apollo 16 crew photographed an unusual variety of impact craters, including the two craters produced by the impacts of Ranger 7 and 9 spacecraft, small craters produced by boulders as they bounced downslope, craters with marked bilateral symmetry, and primary craters with a wide range of morphologies and sizes....
Photogeology: Part L: crater morphometry
Richard J. Pike
1972, Book chapter, Apollo 16 preliminary science report (NASA SP 315)
Morphometric analysis of lunar craters (ref. 29-75) complements the more traditional photointerpretive study of crater morphology. These two indirect approaches to the scientific investigation of lunar craters continue to be productive because the preferred alternative method, direct field examination of specific large craters, is not being undertaken in the current...
Preliminary examination of lunar samples: Part A: a petrographic and chemical description of samples from the lunar highlands
The Lunar Sample Preliminary Examination Team
1972, Book chapter, Apollo 16 preliminary science report (NASA SP 315)
More than four-fifths of the surface of the Moon consists of a profoundly cratered irregular surface designated terra or highlands by analogy with the terrestrial continents. These terra regions have much higher albedos than the physiographically lower and much smoother mare regions. The difference in albedo can now be ascribed...
Photogeology: Part S: mare ridges and arches in southern Oceanus Procellarum
George W. Colton, Keith A. Howard, Henry J. Moore
1972, Book chapter, Apollo 16 preliminary science report (NASA SP 315)
Low-relief mare features such as ridges and arches are best studied by using stereoscopic photographs taken at low Sun angles. Apollo 16 metric camera photography of the southern Oceanus Procellarum east of Letronne Crater reveals a diversity of subtle features (fig. 29-125) and adds significantly to an understanding of the...