Publications
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The physics of debris flows — A conceptual assessment
Debris flows exhibit conspicuous dynamic interactions among their solid and fluid constituents. Key features of the interactions are neglected in traditional theories that treat debris flows as viscoplastic continua or as uniformly dispersed grain flows, but improved understanding of grain-grain and fluid-grain interactions has emerged from recent experimental and theoretical research. Grain-flow
Authors
Richard M. Iverson, Roger P. Denlinger
Unreinforced masonry buildings
No abstract available.
An interview with Otto Nuttli
No abstract available.
A chronology of U.S. Geological Survey hazards warnings: 1976-1986
No abstract available.
Authors
Paula L. Gori, Clement F. Shearer
Debris flow/avalanches: Process, recognition, and mitigation
No abstract available.
Authors
John E. Costa, G. F. Wieczorek
A detailed chronology of the most recent eruption period at Mount Hood, Oregon
The most recent eruptive period of Mount Hood volcano, the Old Maid eruptive period, was characterized by volcano-hydrologic events (hydrologic events initiated by volcanic activity) which resulted in extensive lahar inundation in the White, Sandy, and Zigzag River drainages and produced a lithic pyroclastic flow which traveled at least 9 km down the White River from the vent area at Crater Rock.
Authors
Kenneth A. Cameron, P. T. Pringle
Flood power
No abstract available.