Harry W. Smedes
1967, Open-File Report 67-203
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Page 5854, results 146326 - 146350
Publication Extents
Not all publications have extents, not all extents are completely accurateHolly C. Wagner
1967, Open-File Report 67-266
R.S. Saunders, T.A. Mutch
1967, Open-File Report 68-197
Ellipse III-9-5 is in a level area between Mare Cognitum and Oceanus Procellarum, approximately 125 km southeast of the crater Lansberg. Mare material within the map area is covered with a greater number of subdued craters than typical smooth mare. ...
Jerry Harbour
1967, Open-File Report 68-118
Ellipse III-12-1 is in the northwestern part of the Flamsteed P ring, about 35 km north-northeast of the crater Flamsteed E. The area is a moderately cratered, undulating mare plain. ...
Mareta West, P. Jan Cannon
1967, Open-File Report 68-321
Ellipse III-11-8 is in southeast Oceanus Procellarum, south of the craters Kepler and Encke. ...
N.J. Trask
1967, Open-File Report 68-270
This map is one of series showing the geology of potential early Apollo landing sites. It was prepared largely from high-resolution photographs taken by Lunar Orbiters II and V. ...
Frank Joseph Kleinhampl, Joseph I. Ziony
1967, Open-File Report 67-129
Water Resources Division, U.S. Geological Survey
1967, Open-File Report 67-232
No abstract available....
Howard D. Zeller
1967, Open-File Report 68-337
No abstract available. ...
Howard D. Zeller
1967, Open-File Report 68-338
No abstract available. ...
Water Resources Division, U.S. Geological Survey
1967, Open-File Report 67-252
No abstract available....
Water Resources Division, U.S. Geological Survey
1967, Open-File Report 67-233
No abstract available....
M. H. Carr
1967, Open-File Report 68-32
Site II P-2, on the southern edge of Mare Tranquillitatis, is in an area transitional between mare and terra. Mare or mare-like material predominate; typical upland terrain occurs locally, but is more extensive south and west of the site. A distinctive feature of the site is the exceptional smoothness and...
L.B. Laird, K.L. Walters
1967, Open-File Report 67-142
G.C. Doty
1967, Open-File Report 67-84
M. E. Davis, E. R. Leggat
1967, Open-File Report 67-79
The Hueco Bolson, as defined in this report, is in the extreme western part of Texas and includes that part of El Paso County between the Franklin and Hueco Mountains north of the Rio Grande....
R. D. Carroll, D.L. Coffin, J. R. Ege, F.A. Welder
1967, Open-File Report 67-38
Analysis of geologic, hydrologic , and geophysical data obtained in and around Yellow Creek core hole No. 1, Rio Blanco County, Colorado, indicate a 1,615-foot section of oil shale was penetrated by the hole. Geophysical log data indicate the presence of 25 gallons per ton shale for a thickness of...
F.E. Clarke, Ivan Barnes
1967, Open-File Report 67-45
R.W. Clement
1967, Open-File Report 67-46
D.E. Click, B. N. Aldridge
1967, Open-File Report 67-47
Alberto Condes de la Torre
1967, Open-File Report 67-66
J.J. Cook
1967, Open-File Report 67-67
W.P. Cross
1967, Open-File Report 67-69
E. G. Crosthwaite
1967, Open-File Report 67-70
E.J. Crosthwaite, M.J. Mundorff, E.H. Walker
1967, Open-File Report 67-71
The lower Henrys Fork region includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River in eastern Idaho. The northwestern and western parts of the area are part of the Snake River lava plain. The central part of the area is occupied by...