Gerald Martin Richmond
1969, Open-File Report 69-222
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Publication Extents
Not all publications have extents, not all extents are completely accurateGeorge Plafker
1969, Professional Paper 543-I
The March 27, 1964, earthquake was accomp anied by crustal deformation-including warping, horizontal distortion, and faulting-over probably more than 110,000 square miles of land and sea bottom in south-central Alaska. Regional uplift and subsidence occurred mainly in two nearly parallel elongate zones, together about 600 miles long and as much...
H. W. Anderson Jr.
1969, Open-File Report 69-8
C.F. Galliher, J.E. Hull
1969, Open-File Report 69-100
Roger B. Colton
1969, Geologic Quadrangle 782
W.C. Overstreet, Elno Rasainen, M.A. Fourati, K.H. Shahwan, Ibrahim Baradja
1969, Open-File Report 69-190
No abstract available....
F. J. Frank, A.B. Harris
1969, Open-File Report 69-95
Crater Lake National Park is on the crest of the Cascade Range in southwestern Oregon. Except for small areas of glacial deposits, the area is underlain by volcanic rocks of Tertiary and Quaternary age. The principal rock types are andesitic and basaltic lavas, pumiceous volcanic flow breccias, tuffs, and airborne...
K. V. Wilson, James W. Hudson
1969, Hydrologic Atlas 407
No abstract available....
B.D. Tschudy
1969, Professional Paper 643-A
D.H. Carpenter, R.H. Simmons
1969, Open-File Report 69-32
No abstract available....
D. L. Stevens, Robert B. Forbes, D. B. Hawkins
1969, Open-File Report 69-266
Gold analysis of grab and auger samples of bedrock taken along the new Ester Dome Road reveals that this road cuts several mineralized zones characterized by anomalous concentrations of gold. The results of a magnetometer traverse along this road indicate that the negative magnetic anomalies along the traverse may be...
C.A. Repenning, M. E. Cooley, J. P. Akers
1969, Professional Paper 521-B
No abstract available....
G. E. Ulrich
1969, IMAP 604
Lunar surface materials are classed into units on the basis of visual observations and data from telescopic and Lunar Orbiter photographs. Each unit has a distinctive range of physical...
George Plafker, E.M. MacKevett Jr.
1969, Open-File Report 69-208
Betsy A. Weld, Margaret S. Griffin, George W. Brett
1969, Circular 568
R.P. Novitzki, Wayne A. Van Voast, L.A. Jerabek
1969, Hydrologic Atlas 320
Glacial drift and Cretaceous sedimentary rocks are the major aquifers in the Yellow Medicine River watershed unit. The Yellow Medicine and Minnesota Rivers are the major sources of surface water. For physiographic regions – Upland Plain, Slope, Lowland Plain, and Minnesota River Flood Plain – influence surface drainage, and the flow...
R.J. Pickering
1969, Professional Paper 433-H
Roman T. Mycyk, Gerald L. Walter
1969, Hydrologic Atlas 303
R. C. Newcomb
1969, Professional Paper 383-C
No abstract available....
J.F. McCauley
1969, IMAP 586
This map is one of a series prepared from photographs transmitted by Ranger IX (Jet Propulsion Lab.,...
S. G. Brown, Herbert H. Schumann
1969, Water Supply Paper 1859-F
The Willcox basin is an area of interior drainage in the northern part of Sulphur Springs Valley, Cochise and Graham Counties, Ariz. The basin comprises about 1,500 square miles, of which the valley floor occupies about 950 square miles. The basin probably formed during middle and late Tertiary time, when...
S.R. Titley, N.J. Trask
1969, IMAP 623
D. H. Whitebread
1969, IMAP 578
E.M. Miller
1969, Hydrologic Atlas 410
No abstract available....
George Vincent Cohee, Robert Glenn Bates, W.B. Wright
1969, Bulletin 1274-A
No abstract available....