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Page 5311, results 132751 - 132775

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Geochemistry of the Mattole River in Northern California
Vance C. Kennedy, Ronald L. Malcolm
1977, Open-File Report 78-205
The chemical composition of streams can vary greatly with changing discharge during storm runoff. These chemical changes are related to the pathways of various water parcels from the time they fall as rain until they enter the stream, and to the interactions between water and sediment during transport downstream. In...
Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma
Joseph J. D’Lugosz, Roger G. McClaflin
1977, Open-File Report 77-487
Most of the data presented in this report were collected by the U.S. Geological Survey as part of a study of the geohydrology of the Vamoosa aquifer, in east-central Oklahoma, in cooperation with the Oklahoma Geological Survey. Some of the data listed in the tables were collected by Bingham and...
Interpretation of Landsat images: Oman
Maurice J. Grolier
1977, Open-File Report 77-296
The part of northern Oman shown on this mosaic of two Landsat images extends from Ras al Hadd in the east to the village of Wudam Alwa on the coast of the Gulf of Oman. The mosaic consists of two Landsat images printed in false color on Cibachrome material. The three major physiographic...
Late Pleistocene and Recent geology of the Housatonic River region in northwestern Connecticut
George C. Kelley
1977, Open-File Report 77-545
An investigation of Late Pleistocene and Recent surficial deposits in western Connecticut and adjacent areas was undertaken, to determine characteristics of Wisconsin glaciation and the history and chronology of deglaciation in part of the finely dissected New England Uplands. The study area lies along the midreach of the Housatonic River...
Appraisal of the water resources of Death Valley, California-Nevada
Glenn Allen Miller
1977, Open-File Report 77-728
The hydrologic system in Death Valley is probably in a steady-state condition--that is, recharge and discharge are equal, and net changes in the quantity of ground water in storage are not occurring. Recharge to ground water in the valley is derived from interbasin underflow and from local precipitation. The two...
Analysis of runoff from small drainage basins in Wyoming
Gordon S. Craig, James G. Rankl
1977, Open-File Report 77-727
A flood-hydrograph study has defined the magnitude and frequency of flood volumes and flood peaks that can be expected from drainage basins smaller than 11 square miles in the plains and valley areas of Wyoming. Rainfall and runoff data, collected for 9 years on a seasonal basis (April through September),...