Kenneth I. Darmer, Lloyd A. Wagner
1973, Hydrologic Atlas 519
Search Results
165683 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 5586, results 139626 - 139650
Publication Extents
Not all publications have extents, not all extents are completely accurateS. M. Hindall, Earl L. Skinner
1973, Hydrologic Atlas 453
The purpose of this report is to describe the physical environment, availability, characteristics, distribution, movement, and quailty of water in the Pecatonica-Sugar River basin. In addition, water use and water problems are summarized to give an understanding of man's management of water within the basin....
Howard E. Allen, Allen W. Noehre
1973, Hydrologic Atlas 495
Arthur L. Putnam, K.L. Lindskov
1973, Water-Resources Investigations Report 73-12
C.R. Showen, O.O. Williams
1973, Water-Resources Investigations Report 73-23
J.W. Cagle
1973, IMAP 763
The bedrock surface in Iowa is covered nearly everywhere by unconsolidated deposits of glacial drift and alluvium which range in thickness from less than 1 foot to more than 400 feet, and from less than 1 foot to about 60 feet, respectively. The bedrock surface is the result of a...
H. R. Schmoll, Ernest Dobrovolny
1973, IMAP 787-C
R. W. Mower
1973, IMAP 766-H
Saturated Quaternary deposits in the Sugar Horse quadrangle supply significant quantities of water to wells from which water is withdrawn for domestic, municipal, industrial, and irrigation uses. The deposits consist of clay, silt, sand, and gravel; individual beds range from a few inches to several tens of feet thick. The...
N.M. Denson, W. R. Keefer, G. H. Horn
1973, IMAP 848-C
No abstract available....
D. J. Easterbrook
1973, IMAP 854-A
R. W. Mower, Richard Van Horn
1973, IMAP 766-I
The depth to ground water in shallow aquifers in the Sugar Horse quadrangle ranges from zero in areas of springs and seeps to more than 10 feet beneath most of the area shown on the map. The depth to water differs from place to place because of irregular topography, and...
Water Resources Division, U.S. Geological Survey, Liberian Geological Survey
1973, IMAP 778-A
D. J. Gable
1973, IMAP 792-A
No abstract available....
J. O. Maberry
1973, IMAP 770-M
No abstract available....
R. W. Mower
1973, IMAP 766-L
The potentiometric surface is an imaginary surface representing the static head of ground water and defined by the levels to which ground water would rise in tightly cased wells. The potentiometric surface of the principal aquifer within the area of the Sugar House quadrangle ranges from about 20 feet above,...
R. B. Morton
1973, IMAP 738
No abstract available....
Paul L. Williams, Harry R. Covington
1973, IMAP 591-O
This map is intended as a guide for those who enjoy outdoor recreation in magnificent scenic settings.The Salina quadrangle lies in the heart of the Colorado Plateau, a sparsely populated land of unique and outstanding scenic beauty. The eastern half of the quadrangle is a great desert, partly blanketed by...
R. D. Miller
1973, IMAP 852-A
D. J. Gable
1973, IMAP 792-C
No abstract available....
M. M. Clark
1973, IMAP 741
No abstract available....
W. H. Monroe
1973, IMAP 751
J. R. Keith, J. O. Maberry
1973, IMAP 770-N
No abstract available....
Liberian Geological Survey
1973, IMAP 772-A
J.F. McCauley
1973, IMAP 740
The Grimaldi quadrangle lies at the southwest margin of Oceanus Procellarum about 1,000 km east of Orientale, the youngest of the lunar multi-ringed basins. The distal ends of the...
B.H. Kent
1973, IMAP 743