Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana
Joseph W. Lang
1972, Water Supply Paper 1899-M
Fresh water in abundance is contained in large artesian reservoirs in sand and gravel deposits of Tertiary and Quaternary ages in the Pearl River basin, a watershed of 8,760 square miles. Shallow, water-table reservoirs occur in Quarternary deposits (Pleistocene and Holocene) that blanket most of the uplands in .the southern...
The ground-water system in southeastern Laramie County, Wyoming
Marvin A. Crist, William B. Borchert
1972, Open-File Report 72-80
Increased development of irrigation wells in southeastern Laramie County, Wyo., has caused concern about the quantity of water available. Ground water from approximately 230 large-capacity wells is used to irrigate most of the 18,165 acres under irrigation. The purpose of this study is to provide more knowledge about the character...
Generalized subsurface geology of the water-bearing deposits, northern San Joaquin Valley, California
W. R. Hotchkiss
1972, Open-File Report 73-119
The study area includes about 5,000 square miles of the northern part of the San Joaquin Valley, a broad structural trough drained by the San Joaquin River. Fresh ground water is mostly in unconsolidated deposits derived from the Coast Ranges on the west and the Sierra Nevada on the east.....
Annual water-resources review, White Sands Missile Range: 1971
R. R. Cruz
1972, Report
This report presents water-resource information that was collected at White Sands Missile Range during 1971 and early 1972 by personnel of the U.S. Geological Survey, Water Resources Division. Data on ground-water pumpage and resulting water-level fluctuation, chemical quality, percipitation, and surface-water runoff are summarized in the report. The data were...
Selected fluvial monazite deposits in the southeastern United States
William C. Overstreet, A. M. White, P. K. Theobald, D. W. Caldwell
1971, Open-File Report 71-222
Farther southwest in Georgia, around Griffin and Zebullon, along streams tributary to the Flint River in the monazite belt the flood plains are generally small and discontinuous, and only about 1 percent of the sediment is gravel. The area between Griffin, Zebullon, and the Flint River is underlain by biotite...
Water resources of the upper White River basin, east-central Indiana
L. W. Cable, J. F. Daniel, R. J. Wolf, C. H. Tate
1971, Water Supply Paper 1999-C
Ground-water discharge to the streams sustains year-round streamflow in the upper White River basin. This discharge, referred to as ground-water runoff or base runoff, is considered to be an index to the amount of g ound water available for development. A comparison of the variations of groundwater runoff and aquifer...
Annual water-resources review, White Sands Missile Range, 1970, a basic-data report
J.A. Basler
1971, Open-File Report 71-15
Deformation of lee-side laminae in eolian dunes
Edwin D. McKee, John R. Douglass, Suzanne Rittenhouse
1971, Bulletin of the Geological Society of America (82) 359-378
Processes responsible for structures in sand dunes consist of (l) primary deposition by saltation and creep and by settling from suspension, (2) redeposition accompanying avalanching, and (3) penecontemporaneous erosion. Characteristics of dune structures were examined in the field by introducing marker beds of magnetite at times of sand deposition, thus...
Glacial marine sediments in the precambrian Gowganda formation at Whitefish Falls, Ontario (Canada)
D. A. Lindsey
1971, Palaeogeography, Palaeoclimatology, Palaeoecology (9) 7-25
Study of a well-exposed section of the Gowganda Formation at Whitefish Falls, Ontario, suggests criteria for the recognition of glacial marine sediments. Thickness of hundreds of feet, lateral continuity, faint internal stratification, sorted lenses of sandstone and conglomerate, and dropstones characterize much of the tillite. Thickness of hundreds of feet,...
Water supply well SRC-2, Stallion Range Center, White Sands Missile Range, Socorro County, New Mexico
F. P. Lyford
1970, Open-File Report 70-202
No abstract available....
Silica sand deposits in the Monrovia area, Liberia
Sam Rosenblum, S.P. Srivastava
1970, Open-File Report 70-280
Thin surficial deposits of white silica sand occupy much of the flat coastal area of Liberia from Monrovia to Buchanan 100 km southeast; most of the sand is of good quality for glass manufacture. A lagoonal mode of origin is suggested for these essentially monomineralic deposits. Based on the average...
Test wells T-15, T-16, T-17, T-18, and Rc-3, White Sands Missile Range, Dona Ana and Socorro Counties, New Mexico
F. P. Lyford
1970, Open-File Report 70-201
Electrical-analog-model study of water resources of the Columbus area, Bartholomew County, Indiana
Frank A. Watkins, J. E. Heisel
1970, Water Supply Paper 1981
The Columbus study area is in part of a glacial outwash sand and gravel aquifer that was deposited in a preglacial bedrock valley. The study area extends from the north line of Bartholomew County to the south county line and includes a small part of Jackson County south of Sand...
Stratigraphic test well T-14, Post Area, White Sands Missile Range, Dona Ana County, New Mexico
G.C. Doty, J.B. Cooper
1970, Open-File Report 70-113
Summary records of supply wells and test wells in the Post Headquarters are, White Sands Missile Range, New Mexico
J.B. Cooper
1970, Open-File Report 70-89
Annual water-resources review, White Sands Missile Range, 1969--a basic data report
F.E. Busch
1970, Open-File Report 70-49
Reconnaissance geology of the Wadi Wassat quadrangle, Kingdom of Saudi Arabia
William C. Overstreet, Darwin L. Rossman
1970, Open-File Report 70-248
The Wadi Wassat quadrangle covers an area of 2926 sq km in the southwestern part of the Kingdom of Saudi Arabia. The west half of the quadrangle is underlain by crystalline rocks of the Arabian Shield, but in the eastern half of the quadrangle the Precambrian rocks are covered by...
Estimated mean-annual runoff at Post Headquarters area, White Sands Missile Range, New Mexico
A. G. Scott
1970, Open-File Report 70-297
Nature and origin of early and late cherts in the Leadville Limestone, Colorado
Norman G. Banks
1970, Bulletin of the Geological Society of America (81) 3033-3048
Two generations of chert have been observed in the Mississippian Leadville Limestone of west-central Colorado: (1) an early chert inferred to have precipitated from hypersaline marine waters of high pH after those waters seeped into carbonate muds prior to final burial and lithification of the carbonate; and (2) a late...
Summary records of supply wells and test wells in the Post Headquarters area, White Sands Missile Range, New Mexico
James B. Cooper
1970, Report
No abstract available....
Missile impacts as sources of seismic energy on the moon
G.V. Latham, W.G. McDonald, H. J. Moore
1970, Science (168) 242-245
Seismic signals recorded from impacts of missiles at the White Sands Missile Range are radically different from the signal recorded from the Apollo 12 lunar module impact. This implies that lunar structure to depths of at least 10 to 20 kilometers is quite different from the typical structure of the...
Geophysical surveys for ground water at White Sands Missile Range, New Mexico
Adel A. R. Zohdy, D. B. Jackson, R.E. Mattick, D. L. Peterson
1969, Open-File Report 69-326
Sedimentary rocks of the coast of Liberia
Richard William White
1969, Open-File Report 69-318
Two basins containing sedimentary rocks o# probable Cretaceous age have been recognized near the coast of Liberia in the area between Monrovia and Buchanan; geophysical evidence suggests that similar though larger basins exist on the adjacent continental shelf. The oldest sedimentary unit recognized, the Paynesville Sandstone of possible early to...
Test wells SMR-4 and SMR-4, White Sands Missile Range, Dona Ana County, New Mexico
G.C. Doty
1969, Open-File Report 69-78
Glacial sedimentology of the Precambrian Gowganda Formation, Ontario, Canada
David A. Lindsey
1969, GSA Bulletin (80) 1685-1702
The Gowganda Formation is part of the thick Huronián sequence of Precambrian sedimentary rocks that crop out in central Ontario from Lake Superior to Quebec. Although it has long been considered to be glacial, recent work on submarine slump and turbidite deposits has reopened the question of its origin. This...