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Page 5946, results 148626 - 148650

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Water resources of the Satus Creek Basin, Yakima Indian Reservation, Washington
M.J. Mundorff, Mac Nish, D.R. Cline
1976, Open-File Report 76-685
The Satus Creek basin lies on the east flank of the Cascade Range in south-central Washington. The basin is entirely within the Yakima Indian Reservation and is bordered and drained on the east by the Yakima River.Average annual precipitation ranges from about 35 inches in the western upland to less...
Geologic map of the Oxia Palus Quadrangle of Mars
D.E. Wilhelms
1976, IMAP 895
The Oxia Palus quadrangle contains three distinct geologic provinces: (1) an elevated cratered plateau that occupies three-fourths of the quadrangle and is similar to much of the southern hemisphere of Mars; (2) the low, relatively featureless Chryse Planitia in the northwest corner; and (3) a complex province of chaotic terrain...
Teton Dam flood of June 1976, Deer Parks quadrangle, Idaho
Herman A. Ray, C. Michael Bennett, Andrew W. Records
1976, Hydrologic Atlas 571
The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The...
Organic carbon and nitrogen concentrations and annual organic carbon load of six selected rivers of the United States
Ronald L. Malcolm, W. H. Durum
1976, Water Supply Paper 1817-F
The organic carbon load during 1969-70 of each of the six rivers in this study is substantial. The 3.4-billion-kilogram (3.7-million-ton) and 47-million-kilogram (52-thousandton) annual organic carbon loads of the Mississippi River and the Brazos River (Tex.), respectively, were approximately equally distributed between dissolved and suspended phases, whereas the 725-million-kilogram (79.8-million-ton)...
Teton Dam flood of June 1976, Moreland quadrangle, Idaho
Larry L. Hubbard, John H. Bartells
1976, Hydrologic Atlas 580
The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The...
Teton Dam flood of June 1976, Firth quadrangle, Idaho
Larry L. Hubbard, John H. Bartells
1976, Hydrologic Atlas 577
The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The...
Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho
Joe A. Moreland, Harold R. Seitz, Albert Mario LaSala
1976, Open-File Report 76-673
Approximately 3,100 drain wells injects irrigation waste water, urban runoff, septic-tank effluent, and industrial waste water into the Snake Plain aquifer in Minidoka, Gooding, Jerome, and Lincoln Counties, Idaho. About 29,000 acre-feet of irrigation waste water, 100 acre-feet of urban runoff, 400 acre-feet of septic-tank effluent, and 1,000 acre-feet of...
Quality-of-water data, Palm Beach County, Florida, 1970-1975
Wesley L. Miller, Arthur C. Lietz
1976, Open-File Report 76-784
One of the most pressing problems of Palm Beach County, Florida, is the present and potential contamination of the surface and ground-water resources. The canals which dissect the urban and agricultural areas are convenient receptacles for storm-water runoff, sewage effluent, and agricultural wastes. Contaminants in the canals may enter the...
Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington
Dee Molenaar
1976, Open-File Report 76-808
On the Yakima Indian Reservation, Washington, only about 5 percent of the Satus Creek basin--in the relatively flat eastern lowland adjacent to and including part of the Yakima River lowland--is agriculturally developed, mostly through irrigation. Because the basin 's streams do not contain adequate water for irrigation, most irrigation is...
Water resources of the Bighorn basin, northwestern Wyoming
Marlin E. Lowry, H. W. Lowham, Gregory C. Lines
1976, Hydrologic Atlas 512
This 2-sheet map report includes the part of the Bighorn Basin and adjacent mountains in northwestern Wyoming. Water-bearing properties of the geologic units are summarized. The hydrogeologic map illustrates the distribution of wells in the different units and gives basic data on the yields of wells, depth of wells, depth...
Floodflow characteristics at proposed bridge site on Fishkill Creek, Fishkill, New York
Thomas J. Zembrzuski, Bernard Dunn
1976, Open-File Report 76-595
An evaluation of floodflow characteristics of Fishkill Creek at the proposed bridge site at Fishkill, N.Y., was made for the 50- and 100-year floods. The flood-frequency analysis revealed that the magnitude of the 50- and 100-year floods are 8,000 cubic feet per second (cfs) and 10,000 cfs, respectively. The normal...
Probable maximum flood at Lake Chippewa near Winter, Wisconsin
William R. Krug
1976, Open-File Report 76-800
The probable maximum flood was computed for Lake Chippewa, Wisconsin, and routed through the lake to determine maximum lake stage. The peak discharge of the probable maximum flood at Lake Chippewa was computed to be about 75,000 cubic feet per second, primarily caused by rainfall on the lake. A secondary...