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Page 3575, results 89351 - 89375

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Ground-water geochemistry of Kwajalein Island, Republic of the Marshall Islands, 1991
Gordon W. Tribble
1997, Water-Resources Investigations Report 97-4184
Ground water on Kwajalein Island is an important source of drinking water, particularly during periods of low rainfall. Fresh ground water is found as a thin lens underlain by saltwater. The concentration of dissolved ions increases with depth below the water table and proximity to the shoreline as high-salinity seawater...
NAWQA, National Water-Quality Assessment Program; Allegheny-Monongahela River Basin
Steven D. McAuley, Juliane B. Brown, James I. Sams III
1997, Open-File Report 97-246
Surface-water and ground-water quality and aquatic life can be significantly affected by the following principal issues identified in the Allegheny-Monongahela River Basin:Contaminants common to surface and under-ground coal mine discharge such as acidity, iron, aluminum, manganese, and sulfate.Volatile organic compounds (VOC’s), pesti-cides, and nutrients from increased urbanization.Runoff and loading of...
Deep structure of Medicine Lake volcano, California
J.R.R. Ritter, J.R. Evans
1997, Tectonophysics (275) 221-241
Medicine Lake volcano (MLV) in northeastern California is the largest-volume volcano in the Cascade Range. The upper-crustal structure of this Quaternary shield volcano is well known from previous geological and geophysical investigations. In 1981, the U.S. Geological Survey conducted a teleseismic tomography experiment on MLV to explore its deeper structure....
Analysis of borehole televiewer measurements in the Vorotilov drillhole, Russia - First results
K. Huber, K. Fuchs, J. Palmer, F. Roth, B.N. Khakhaev, L. E. Van-Kin, L.A. Pevzner, S. Hickman, Daniel Moos, Mark D. Zoback, D. Schmitt
1997, Tectonophysics (275) 261-272
In the Eurasian part of the World Stress Map almost the whole region east of the Tornquist-Teisseyre line is terra incognita. The closure of this information gap is of fundamental importance to the understanding of the geodynamics of the Eurasian continent. A detailed analysis of stress-induced wellbore breakouts has been...
Southern Laurentide ice lobes were created by ice streams: Des Moines Lobe in Minnesota, USA
C. J. Patterson
1997, Sedimentary Geology (111) 249-261
Regional mapping in southern Minnesota has illuminated a suite of landforms developed by the Des Moines Lobe that delimit the position of the lobe at its maximum and at lesser readvances. The ice lobe repeatedly advanced, discharged its subglacial water, and subsequently stagnated. Recent glaciological research on Antarctic ice streams...
Reinterpretation of the peninsular Florida Oligocene: An integrated stratigraphic approach
G. Lynn Wingard, T.M. Scott, Lucy E. Edwards, S.D. Weedman, K. R. Simmons
1997, Sedimentary Geology (108) 207-228
A very thick (> 300 m) nearly continuous Oligocene section exists in southern peninsular Florida, as revealed by lithostratigraphic, biostratigraphic (mollusks and dinocysts), chronostratigraphic (Sr isotopes) and petrographic analyses of twelve cores and two quarries. The Oligocene deposits in the subsurface of southern Florida are the thickest documented in the...
Slope-apron deposition in an Ordovician arc-related setting: The Vuelta de Las Tolas Member (Suri Formation), Famatina Basin, northwest Argentina
M.G. Mangano, L.A. Buatois
1997, Sedimentary Geology (109) 155-180
The Ordovician Suri Formation is part of the infill of the Famatina Basin of northwest Argentina, which formed in an active setting along the western margin of early Paleozoic Gondwana. The lower part of this formation, the Vuelta de Las Tolas Member, records sedimentation on a slope apron formed in...
Correlation of Miocene sequences and hydrogeologic units, New Jersey Coastal Plain
P. J. Sugarman, K.G. Miller
1997, Sedimentary Geology (108) 3-18
We have developed a Miocene sequence stratigraphic framework using data from recently drilled boreholes in the New Jersey Coastal Plain. Sequences are shallowing upward, unconformity-bounded units; fine-grained shelf and prodelta sediments grade upward to delta front and shallow-marine sands, corresponding to confining bed-aquifer couplets. By dating Miocene sequences using Sr-isotope...