Publications
Filter Total Items: 883
Summit Lake landslide and geomorphic history of Summit Lake basin, northwestern Nevada
The Summit Lake landslide, northwestern Nevada, composed of Early Miocene pyroclastic debris, Ashdown Tuff, and basalt and rhyolite of the Black Rock Range, blocked the upper Soldier Creek-Snow Creek drainage and impounded Summit Lake sometimes prior to 7840 yr B.P. The slide covers 8.2 km2 and has geomorphic features characteristic of long run-out landslides, such as lobate form, longitudinal and
Authors
B. Brandon Curry, W.N. Melhorn
Landslides: Extent and economic significance in the United States
No abstract available.
Authors
E. E. Brabb
Landslide classification for identification of mud flows and other landslides
No abstract available.
Authors
R. H. Campbell, R. W. Fleming, D.J. Prior, D. J. Nichols, D. J. Varnes, M. A. Hampton, D.A. Sangrey, E. E. Brabb
Maps showing landslide features and related ground deformation in the Woodlawn area of the Manoa Valley, City and County of Honolulu, Hawaii
No abstract available.
Authors
Rex L. Baum, Robert W. Fleming, Stephen D. Ellen
Transformation of dilative and contractive landslide debris into debris flows-An example from Marin County, California
The severe rainstorm of January 3, 4 and 5, 1982, in the San Francisco Bay area, California, produced numerous landslides, many of which transformed into damaging debris flows. The process of transformation was studied in detail at one site where only part of a landslide mobilized into several episodes of debris flow. The focus of our investigation was to learn whether the landslide debris dilated
Authors
R. W. Fleming, S. D. Ellen, M.A. Algus
Structures associated with strike-slip faults that bound landslide elements
Large landslides are bounded on their flanks and on elements within the landslides by structures analogous to strike-slip faults. We observed the formation of thwse strike-slip faults and associated structures at two large landslides in central Utah during 1983-1985. The strike-slip faults in landslides are nearly vertical but locally may dip a few degrees toward or away from the moving ground. Fa
Authors
R. W. Fleming, A. M. Johnson
Statistical analysis of factors affecting landslide distribution in the new Madrid seismic zone, Tennessee and Kentucky
More than 220 large landslides along the bluffs bordering the Mississippi alluvial plain between Cairo, Ill., and Memphis, Tenn., are analyzed by discriminant analysis and multiple linear regression to determine the relative effects of slope height and steepness, stratigraphic variation, slope aspect, and proximity to the hypocenters of the 1811-12 New Madrid, Mo., earthquakes on the distribution
Authors
R. W. Jibson, D. K. Keefer
Landslide deposits in the Duchesne 30' x 60' Quadrangle, Utah
No abstract available.
Authors
R. B. Colton, Bruce Bryant
Landslides and debris flows in Ephraim Canyon, central Utah
No abstract available.
Authors
Rex L. Baum, Robert W. Fleming