1972, IMAP 591-C
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateW. J. Hail Jr.
1972, IMAP 698
Bruce Bryant
1972, IMAP 785-A
I. J. Witkind
1972, IMAP 781-A
R.R. Burchett, V. H. Dreeszen, E.C. Reed, G.E. Prichard
1972, IMAP 729
Bruce Bryant
1972, IMAP 785-G
Larry D. Harris
1972, IMAP 767-C
No abstract available....
R. V. Sharp
1972, IMAP 675
No abstract available....
D.W. Rankin, G.H. Espenshade, R. B. Neuman
1972, IMAP 709-A
Glenn R. Scott
1972, IMAP 790-C
Formations that contain clays having swelling pressures higher than 2,500 pounds per square foot (as measured by the Potential Volume Change meter) are listed in order of decreasing swelling pressure: Denver Formation, Pierre Shale, Laramie Formation, Green Mountain Conglomerate, Fox Hills Sandstone, and Arapahoe Formation. Some landslides derived from these...
D.E. Wilhelms
1972, IMAP 722
The distribution of major physiographic provinces and geologic units of the Tarantius quadrangle is determined by the five intersecting circular multi-ringed mare basins. Three basins, i<span...
R.E. Hansen
1972, IMAP 717
L.A. Weiss
1972, IMAP 784-Q
R.R. Compton
1972, IMAP 672
G. R. Scott
1972, IMAP 790-A
G. R. Scott
1972, IMAP 790-F
No abstract available....
G. R. Scott
1972, IMAP 790-E
G. R. Scott
1972, IMAP 790-D
No abstract available....
1972, IMAP 591-E
In general, long freeze-free periods occur at low elevations, and short freeze-free periods occur at high elevations. But some valley floors have shorter freeze-free seasons than the glancing foothills because air cooled at high elevations flows downward and is trapped in the valleys. This temperature pattern occurs in the western...
B. A. Morgan
1972, IMAP 724
I. J. Witkind
1972, IMAP 781-E
No abstract available....
1972, IMAP 591-D
No abstract available....
W. H. Langer
1972, IMAP 784-E
G. R. Scott
1972, IMAP 790-B
No abstract available....
Paul L. Williams
1972, IMAP 591-L
The term “landslide” is broadly defined as any “downward and outward movement of slope-forming materials composed of natural rock, soils, artificial fills, or combinations of these materials. The moving mass may proceed by any one of three principal types of movement: falling, sliding, or flossing, or by their combinations” (Varnes,...