Computations of total sediment discharge, Niobrara River near Cody, Nebraska
Bruce R. Colby, C. H. Hembree
1955, Water Supply Paper 1357
A natural chute in the Niobrara River near Cody, Nebr., constricts the flow of the river except at high stages to a narrow channel in which the turbulence is sufficient to suspend nearly the total sediment discharge. Because much of the flow originates in the sandhills area of Nebraska, the...
Ground-water resources of the Middle Loup division of the lower Platte River basin, Nebraska, with a section on Chemical quality of the ground water
Delbert Wayne Brown, Frank Hays Rainwater
1955, Water Supply Paper 1258
The Middle Loup division of the lower Platte River basin is an area of 650 square miles which includes the Middle Loup River valley from the confluence of the Middle and North Loup Rivers in Howard County, Nebr., to the site of the diversion dam that the U. S. Bureau...
Floods of April 1952 in the Missouri River basin
J. V. B. Wells
1955, Water Supply Paper 1260-B
The floods of April 1952 in the Milk River basin, along the Missouri River from the mouth of the Little Missouri River to the mouth of the Kansas River, and for scattered tributaries of the Missouri River in North and South Dakota were the greatest ever observed. The damage amounted...
Floods of 1952 in the basins of the upper Mississippi River and Red River of the North
J. V. B. Wells
1955, Water Supply Paper 1260-C
The flood of April 1952 on the Mississippi River between the Minnesota and Des Moines Rivers established many record-high stages. In the Minnesota River basin, the floods of April 1952 exceeded those of 1951 in many locations but generally were smaller than those of 1881. The timing of flows on...
Pleistocene geology of the southwestern Wind River Mountains, Wyoming
G.W. Holmes, J.H. Moss
1955, GSA Bulletin (66) 629-654
Patches of Buffalo till record the earliest glaciation in the southwestern Wind River Mountains. In places, these rest in youthful valleys cut in high gravel terrace. Two other younger and lower terraces are both topographically and stratigraphically associated with Buffalo till, which may indicate that the Buffalo advance was compound....
Geology of the Huron River pitchblende occurrence, Baraga County, Michigan
R.C. Vickers
1955, Trace Elements Investigations 303
Small quantities of uranium-bearing minerals were discovered by a geologist of the Jones and Laughlin Ore Company during the summer of 1949 along the East Branch of the Huron River, sec. 1, T. 51 N., R. 30 W., Baraga County, Mich. Subsequent diamond drilling of the prospect by the Jones...
Sediment investigations of the Platte River near Overton, Nebraska
C.D. Albert, H.P. Guy
1955, Report
This report contains results of sediment-transport investigations on the Platte River near Overton,. Nebr. from January 1950 to September 1953. The basic data of suspended-sediment studies, results of bed-material analyses, and determinations of water-surface slopes from staff readings are given. The data indicate that a reliable determination of suspended sediment, hence...
Floods of November-December 1950 in western Nevada
J. V. B. Wells
1954, Water Supply Paper 1137-H
Record-breaking floods in the Walker, Carson, and Truckee River basins during November and December 1950 resulted from a rapid sequence of storms and unseasonably high temperatures that melted most of the early snow cover. During the period November 13 to December 8, 1950, total precipitation ranged from about 5 inches...
First Fourteen Years of Lake Mead
Harold E. Thomas
1954, Circular 346
This circular summarizes the results of recent studies of Lake Mead and its environs. Area-capacity tables, prepared on the basis of a hydrographic survey of the lake in 1948-49, show that the capacity of the reservoir was reduced 4.9 percent during the first 14 years after Hoover Dam was completed,...
Floods in Devils and Pecos River basins of Texas, June 27-28, 1954 - miscellaneous data
S.D. Breeding
1954, Open-File Report 54-27
Record-breaking floods occurred June 27, 28, 1954, in the Devils and lower Pecos Rivers and in some tributaries to those streams, caused by heavy rainfall of June 26-28. At the time of the flood the geological Survey was not operating a gaging station in the Devils River basin or in...
Floods of November-December 1950 in the Central Valley basin, California
C. G. Paulsen
1953, Water Supply Paper 1137-F
The flood of November-December 1950 in the Central Valley basin was the greatest in most parts of the basin since the turn of the century and probably was exceeded in the lower San Joaquin River basin only by the historic flood of 1862. In respect to monetary loss, the 1950...
Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon
Wilbur Douglas Simons
1953, Water Supply Paper 1220
The Columbia River is the largest stream in western United States. Above The Dalles, Oregon, it drains an area of 237,000 square miles, of which 39,000 square miles is in Canada. This area is largely mountainous and lies between the Rocky Mountains and the Cascade Range. The Kootenai, Pend Oreille,...
Floods of May-July 1950 in southeastern Nebraska
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1137-D
Four floods occurred in southeast Nebraska during the period of May to July 1950. Two of these were the greatest known in the State if the size of the drainage areas is considered, and the other two were not so spectacular but were of notable size and of possible hydrologic...
Floods of 1950 in the upper Mississippi River and Lake Superior basins in Minnesota
C. G. Paulsen
1953, Water Supply Paper 1137-G
In areal coverage and magnitude of peak discharge the floods of April-May 1950 in the Missouri River Basin in North and South Dakota were unprecedented in the area. These floods were characterized by an extremely late spring breakup of ice, by great flood peaks resulting from snow melt, and by...
Geology of the Knife River area, North Dakota
William Edward Benson
1953, Open-File Report 53-21
The Knife River area, consisting of six 15-minute quadrangles, includes the lower half of the Knife River valley in west-central North Dakota. The area, in the center of the Williston Basin, is underlain by the Tongue River member of the Fort Union formation (Paleocene) and the Golden Valley formation (Eocene)....
Floods of 1950 in the Red River of the North and Winnipeg River basins
Water Resources Division, U.S. Geological Survey
1952, Water Supply Paper 1137-B
The floods of April-July 1950 in the Red River of the North and Winnipeg River Basins were the largest that have occurred in several decades and caused the greatest damage that the flooded area has ever sustained. Five lives were lost in the United States, owing to causes directly connected...
Flood of August 1950 in the Waimea area, Kauai, Hawaii
R.K. Chun
1952, Water Supply Paper 1137-C
On August 15-18, 1950, Waimea River on the island of Kauai, T. H., had one of the severest floods in its history as a result of torrential rains, caused by a storm associated with the only typhoon ever recorded in the proximity of the Hawaiian Archipelego. At one rainfall station...
Pegmatites of the Crystal Mountain district, Larimer County, Colorado
William R. Thurston
1952, Trace Elements Investigations 139
The Front Range of Colorado is composed chiefly of schists of the pre-Cambrian Idaho Springs formation which have been intruded by a variety of granitic batholiths. In the Crystal Mountain district the Mount Olympus granite, a satellite of the Longs Peak batholith, forms sills and essentially concordant multiple intrusions in...
Missouri River basin floods of April-May 1950 in North and South Dakota
Roy Edwin Oltman
1951, Water Supply Paper 1137-A
In area coverage and magnitude of peak discharge the floods of April-May 1950 in the Missouri River Basin in North and South Dakota were unprecedented in the area. These floods were characterized by an extremely late spring breakup of ice, by great flood peaks resulting from snow melt, and by...
Flood of August 4-5, 1943, in central West Virginia, with a summary of flood stages and discharges in West Virginia
Harlan Mercer Erskine
1951, Water Supply Paper 1134-A
During the night of August 4-5, 1943, a violent, thunderstorm of unusual intensity occurred in parts of Braxton, Calhoun, Gilmer, Ritchie, and Wirt Counties in the Little Kanawha River Basin in central West Virginia. Precipitation amounted to as much as 15 inches in 2 hours in some sections. As a...
The relation of river stages to ground-water levels at Pittsburgh, Pennsylvania
D. W. Van Tuyl
1951, Open-File Report 51-167
No abstract available....
Ground water in the Jordan Valley, Utah
G.H. Taylor, R.M. Leggette
1949, Water Supply Paper 1029
The Jordan Valley is a small part of a larger area that during the glacial epoch was covered by an ancient lake known as Lake Bonneville. The Jordan River, the natural drainage path from Utah Lake, flows northward through the center of the valley and empties into Great Salt Lake....
Texas floods of 1940
Seth D. Breeding
1948, Water Supply Paper 1046
Floods occurred in Texas during, June, July, and November 1940 that exceeded known stages on many small streams and at a few places on the larger streams. Stages at several stream-gaging stations exceeded the maximum known at those places since the collection of daily records began. A storm, haying its...
Major Texas floods of 1936
Tate Dalrymple
1947, Water Supply Paper 816
In 1936 floods occurred in parts of Texas during two periods one about July 1 and the other in the later portion of September which were marked by record-breaking or outstanding stages and discharges on some of the larger rivers. ...
Geologic features of the Connecticut Valley, Massachusetts as related to recent floods
Richard Henry Jahns
1947, Water Supply Paper 996
This report gives the results of a geologic study of certain features that bear upon the recent flood behavior of rivers flowing in the Massachusetts part of the Connecticut Valley. It is in part an outline of the physiographic history of the Connecticut River, a 'history that is treated in...