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Page 4831, results 120751 - 120775

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Not all publications have extents, not all extents are completely accurate
Users manual for a one-dimensional Lagrangian transport model
D. H. Schoellhamer, H.E. Jobson
1986, Water-Resources Investigations Report 86-4145
A Users Manual for the Lagrangian Transport Model (LTM) is presented. The LTM uses Lagrangian calculations that are based on a reference frame moving with the river flow. The Lagrangian reference frame eliminates the need to numerically solve the convective term of the convection-diffusion equation and provides significant numerical advantages...
Results of exploratory drilling for water in Waihanau Valley, Molokai, Hawaii
K. J. Takasaki
1986, Water-Resources Investigations Report 85-4332
Three exploratory wells, located in lower Waihanau Valley on Molokai, were drilled and tested for their yields during the period May to October 1983. The first well, 582 ft deep, tapped the main water body in a basaltic aquifer intruded by scattered near-parallel volcanic dikes. Water in this water body...
Preliminary delineation and description of the regional aquifers of Tennessee -- Highland Rim aquifer system
J. V. Brahana, M. W. Bradley
1986, Water-Resources Investigations Report 82-4054
The Highland Rim aquifer system in Tennessee is primarily composed of Mississippian carbonates and occurs west of the Valley and Ridge Province. It crops out in the Highland Rim and the Sequatchie Valley. It has been removed by erosion from the Central Basin. Groundwater in the Highland Rim aquifer system...
Preliminary delineation and description of the regional aquifers of Tennessee– The Cretaceous aquifer system of west-Tennessee
J. V. Brahana, Dolores Mulderink, M. W. Bradley
1986, Water-Resources Investigations Report 83-4039
The Cretaceous aquifer in Tennessee is composed of sand and clay of Cretaceous age. The aquifer occurs in west Tennessee from the Mississippi River east to the Tennessee River. Groundwater in the Cretaceous aquifer is recharged at outcrops and through overlying permeable deposits. The overlying Porter 's Creek clay acts...
Preliminary delineation and description of the regional aquifers of Tennessee– Tertiary aquifer system
J. V. Brahana, M. W. Bradley, Dolores Mulderink
1986, Water-Resources Investigations Report 83-4011
The Tertiary aquifer system in Tennessee is composed of sands and clays of Quaternary and Tertiary age. The aquifer system occurs in west Tennessee from the Mississippi River east to the outcrop of the Porters Creek Clay. Groundwater in the Tertiary aquifer system is recharged at outcrops and through overlying...
Summary geochemical maps for samples of rock, stream sediment, and nonmagnetic heavy-mineral concentrate, Cypress Roadless Area, Kern County, California
M.A. Chaffee, D.L. Fey, R. H. Hill, S. J. Sutley
1986, Miscellaneous Field Studies Map 1532-B
The Cypress Roadless Area comprises approximately 3 square miles (1,949 acres) of Sequoia National Forest, Kern County, California. The area is at the southern end of the Sierra Nevada, approximately 30 miles east-northeast of Bakersfield, and 2.5 miles and 3.5 miles south-southeast of the communities of Bodfish and Lake Isabella,...
Water quality of Rhode Island streams
J. C. Briggs, J.S. Feiffer
1986, Water-Resources Investigations Report 84-4367
Water quality data collected from November 1979 through September 1983 at five stream stations within Rhode Island and one in Massachusetts show that concentrations of the common constituents were low. Mean water hardness at all sites was in the ' soft ' category. Sodium concentrations were less than 20 mg/L...
Liquefaction susceptibility in the San Bernardino Valley and vicinity, Southern California; a preliminary evaluation
J. C. Matti, S. E. Carson
1986, Open-File Report 86-562
This report discusses earthquake-induced liquefaction susceptibility of alluvial sediments in the San Bernardino valley and vicinity, southern California. The study includes maps that zone the region into areas having high to low susceptibility for each of three scenario earthquakes: a Ms=8.0 earthquake on the San Andreas fault, a Ms=7.0 earthquake...