Norman L. Hatch Jr., Rolfe S. Stanley
1973, Open-File Report 73-101
Search Results
184314 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 6199, results 154951 - 154975
Publication Extents
Not all publications have extents, not all extents are completely accurateJ. W. Warner
1973, Open-File Report 72-442
W. R. Osterkamp
1973, IMAP 844-E
No abstract available....
Joseph C. Clark, Jan D. Rietman
1973, Professional Paper 783
No abstract available....
D.H. Richter, N.A. Matson Jr., H. R. Schmoll
1973, IMAP 807
G.M. Richmond
1973, IMAP 639
G.M. Richmond
1973, IMAP 644
G. W. Walker
1973, IMAP 727
Warren Lee Peterson
1973, Geologic Quadrangle 1076
Arthur A. Baker
1973, Geologic Quadrangle 1103
K. A. Sargent, P. P. Orkild
1973, IMAP 754
Louis Pavlides
1973, Geologic Quadrangle 1094
D. H. Scott, R. E. Eggleton
1973, IMAP 805
The Rumker quadrangle, in the northwest quadrant of the Moon, is adjacent to the western rim of the multi-ring Imbrium basin and to Sinus <span class="SpellingError...
W. G. Pierce, W. H. Nelson, H.J. Prostka
1973, IMAP 816
R. W. Mower
1973, IMAP 766-K
The concentration of dissolved solids in water from the principal aquifer ranges from about 100 mg/l (milligrams per liter) to as much as 800 mg/l. Water containing the least dissolved solids occurs in an arcuate, mile-wide band along the southern border of the Sugar House quadrangle. Water containing the most...
G.M. Richmond
1973, IMAP 645
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,...
Bruce Bryant, Glenn R. Scott, Robert D. Miller
1973, Geologic Quadrangle 1073
R. B. Morton
1973, IMAP 738
No abstract available....
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...
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...
L. M. Shown
1973, IMAP 848-A
No abstract available....
H. E. Simpson
1973, IMAP 761-D
H. E. Simpson
1973, IMAP 761-E
No abstract available....
Richard Van Horn
1973, IMAP 766-G
No abstract available....