Skip to main content
U.S. flag

An official website of the United States government

Dot gov

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Https

Secure .gov websites use HTTPS
A lock ( ) or https:// means you’ve safely connected to the .gov website. Share sensitive information only on official, secure websites.

Search Results

165505 results.

Alternate formats: RIS file of the first 3000 search results  |  Download all results as CSV | TSV | Excel  |  RSS feed based on this search  |  JSON version of this page of results

Page 6071, results 151751 - 151775

Show results on a map

Publication Extents

Not all publications have extents, not all extents are completely accurate
Floods in New York, magnitude and frequency
F. Luman Robison
1961, Circular 454
This report presents a practical means of predicting the probable magnitude of floods on streams in New York State. Because of the limited amount of data on small drainage basins this method is not applicable to sites where the drainage area is less than 10 square miles or to streams...
Ground water in the alluvium of Beaver Creek basin, Oklahoma
D.L. Hart Jr.
1961, Open-File Report 61-59
Beaver Creek is an 857 square-mile area in south-central Oklahoma. The tributaries head at an altitude as high as 1,400 feet and the mouth of Beaver Creek is at an altitude of 804 feet. Alluvial material has been deposited along all the major streams in the basin. The alluvium contains...
Floods in Pennsylvania, frequency and magnitude
W. F. Busch, E.C. Shaw
1961, Open-File Report 61-28
This report outlines a method of determining the magnitude of floods having frequencies up to 50 years for any stream in Pennsylvania except regulated streams and streams whose drainage basins are smaller than 10 square miles. On the main stems of the Schuylkill, Delaware, Susquehanna, and Chemung Rivers the magnitude...
Ground water in the alluvium of Elk Creek basin, Oklahoma
J.R. Hollowell
1961, Open-File Report 61-65
Elk Creek basin comprises 584 square miles in Washita, Beckman, and Kiowa Counties. The basin is typical of southwestern Oklahoma with nearly level plains broken by gentle rolling hills and low escarpments, except for the extreme southern part, where seven granite and gabbroic knobs and ridges of the Wichita Mountains...
Ground water in the vicinity of Roosevelt, Oklahoma
J.R. Hollowell
1961, Open-File Report 61-67
The principal source of additional ground-water supply in the Roosevelt area of west-central Kiowa County is from alluvial deposits. Ground water can be obtained in varying amounts from the red beds of Permian age, but yields of wells are small and the water is of poor quality at most places. Roosevelt's...