Richard M. Iverson
My USGS career has focused mostly on evaluating and modeling the dynamics and hazards of landslides and debris flows, with a secondary focus on the dynamics of volcanic extrusions. Part of my work involved design, development, and utilization of the USGS debris-flow flume, a unique, large-scale experimental facility at the H.J. Andrews Experimental Forest near Blue River, Oregon.
Career Highlights
A written account of some career highlights was published in 2020 in Perspectives of Earth and Space Scientists. An oral history interview recounting some of my career highlights is archived at Oregon State University.
Professional Experience
Senior Research Hydrologist, USGS Cascades Volcano Observatory
Adjunct Professor, University of Washington and Portland State University
Education and Certifications
Stanford University, Ph.D., 1984, Applied Earth Sciences
Stanford University, M.S., 1981, Hydrology
Stanford University, M.S., 1980, Applied Earth Sciences
Iowa State University, B.S., 1977, Geology major, Mathematics and Physics minors
Honors and Awards
Fellow, American Geophysical Union (AGU) and Geological Society of America (GSA)
E.B. Burwell Award, GSA, 1991
Kirk Bryan Award, GSA, 2001
Richard H. Jahns Distinguished Lecturer, GSA, 2005
Langbein Lecturer, AGU, 2006
U.S. Department of the Interior Distinguished Service Award, 2019
Science and Products
My research career, including information about the debris flow experimental flume facility, is docuymented in this memoir.
Landslide disparities, flume discoveries, and Oso despair
When models meet managers: Examples from geomorphology
Gravity-driven mass flows
How should mathematical models of geomorphic processes be judged?
The debris-flow rheology myth
Surge dynamics coupled to pore-pressure evolution in debris flows
Mechanics of debris flows and debris-laden flash floods
Volcano hazards in the Three Sisters region, Oregon
Distributed shear of subglacial till due to Coulomb slip
Flow of variably fluidized granular masses across three-dimensional terrain 2. Numerical predictions and experimental tests
New views of granular mass flows
Flow of variably fluidized granular masses across three-dimensional terrain I. Coulomb mixture theory
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
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- Publications
My research career, including information about the debris flow experimental flume facility, is docuymented in this memoir.
Landslide disparities, flume discoveries, and Oso despair
Landslide dynamics is the branch of science that seeks to understand the motion of landslides by applying Newton's laws. This memoir focusses on a 40‐year effort to understand motion of highly mobile—and highly lethal—landslides such as debris avalanches and debris flows. A major component of this work entailed development and operation of the U.S. Geological Survey debris flow flume, a unique, laAuthorsRichard M. IversonFilter Total Items: 118When models meet managers: Examples from geomorphology
No abstract available.AuthorsPeter R. Wilcock, John C. Schmidt, M. Gordon Wolman, William E. Dietrich, DeWitt Dominick, Martin W. Doyle, Gordon E. Grant, Richard M. Iverson, David R. Montgomery, Thomas C. Pierson, Steven P. Schilling, Raymond C. WilsonGravity-driven mass flows
Gravity-driven mass flows, also known as sediment gravity flows, include a spectrum of phenomena in which more-or-less coherent mixtures of grains and intergranular fluid flow down slopes. At one end of this spectrum are dilute flows in which momentum is transferred mostly by fluid forces and sediment is largely a passive cargo that increases the effective fluid density. These dilute mass flows arAuthorsRichard M. IversonHow should mathematical models of geomorphic processes be judged?
No abstract available.AuthorsRichard M. IversonThe debris-flow rheology myth
Models that employ a fixed rheology cannot yield accurate interpretations or predictions of debris-flow motion, because the evolving behavior of debris flows is too complex to be represented by any rheological equation that uniquely relates stress and strain rate. Field observations and experimental data indicate that debris behavior can vary from nearly rigid to highly fluid as a consequence of tAuthorsR. M. IversonSurge dynamics coupled to pore-pressure evolution in debris flows
Temporally and spatially varying pore-fluid pressures exert strong controls on debris-flow motion by mediating internal and basal friction at grain contacts. We analyze these effects by deriving a one-dimensional model of pore-pressure diffusion explicitly coupled to changes in debris-flow thickness. The new pore-pressure equation is combined with Iverson's (1997) extension of the depth-averaged SAuthorsS.B. Savage, R. M. IversonMechanics of debris flows and debris-laden flash floods
A new mathematical model developed to predict behavior of debris flows and avalanches also holds promise for predicting behavior of debris-laden flash floods. The model assumes that debris flows behave as mixtures of interacting Newtonian fluids and Coulomb solids. Solid and fluid constituents obey three-dimensional mass and momentum balances, which are summed and depth-integrated to yield equatioAuthorsRichard M. Iverson, Roger P. DenlingerVolcano hazards in the Three Sisters region, Oregon
Three Sisters is one of three potentially active volcanic centers that lie close to rapidly growing communities and resort areas in Central Oregon. Two types of volcanoes exist in the Three Sisters region and each poses distinct hazards to people and property. South Sister, Middle Sister, and Broken Top, major composite volcanoes clustered near the center of the region, have erupted repeatedly oveAuthorsWilliam E. Scott, R. M. Iverson, S. P. Schilling, B.J. FisherDistributed shear of subglacial till due to Coulomb slip
In most models of the flow of glaciers on till beds, it has been assumed that till behaves as a viscoplastic fluid, despite contradictory evidence from laboratory studies. In accord with this assumption, displacement profiles measured in subglacial till have been fitted with viscoplastic models by estimating the stress distribution. Here we present a model that illustrates how observed displacemenAuthorsNeal R. Iverson, Richard M. IversonFlow of variably fluidized granular masses across three-dimensional terrain 2. Numerical predictions and experimental tests
Numerical solutions of the equations describing flow of variably fluidized Coulomb mixtures predict key features of dry granular avalanches and water-saturated debris flows measured in physical experiments. These features include time-dependent speeds, depths, and widths of flows as well as the geometry of resulting deposits. Threedimensional (3-D) boundary surfaces strongly influence flow dynamicAuthorsR.P. Denlinger, R. M. IversonNew views of granular mass flows
Concentrated grain-fluid mixtures in rock avalanches, debris flows, and pyroclastic flows do not behave as simple materials with fixed rheologies. Instead, rheology evolves as mixture agitation, grain concentration, and fluid-pressure change during flow initiation, transit, and deposition. Throughout a flow, however, normal forces on planes parallel to the free upper surface approximately balanceAuthorsR. M. Iverson, J. W. VallanceFlow of variably fluidized granular masses across three-dimensional terrain I. Coulomb mixture theory
Rock avalanches, debris flows, and related phenomena consist of grain-fluid mixtures that move across three-dimensional terrain. In all these phenomena the same basic forces, govern motion, but differing mixture compositions, initial conditions, and boundary conditions yield varied dynamics and deposits. To predict motion of diverse grain-fluid masses from initiation to deposition, we develop a deAuthorsR. M. Iverson, R.P. DenlingerNon-USGS Publications**
Iverson, R.M., 1980, Processes of accelerated pluvial erosion on desert hillslopes modified by vehicular traffic: Earth Surface Processes, v. 5, no. 4, p. 369‑388.Iverson, R.M., Hinckley, B.S., Webb, R.H., and Hallet, B., 1981, Physical effects of vehicular disturbances on arid landscapes: Science, v. 212, no. 4497, p. 915‑917.Hinckley, B.S., Iverson, R.M., and Hallet, B., 1983, Accelerated water erosion in ORV‑use areas: Environmental Effects of Off-road Vehicles: Impacts and Management in Arid Regions, R.H. Webb and H.G. Wilshire, eds., Springer‑Verlag, New York, p. 81‑94.Elvidge, C.D., and Iverson, R.M., 1983, Regeneration of desert pavement and desert varnish: Environmental Effects of Off-road Vehicles: Impacts and Management in Arid regions, R.H. Webb and H.G. Wilshire, eds., Springer‑Verlag, New York, p. 225‑241.Iverson, R.M., 1983, Discussion of "A model for creeping flow in landslides" by W.Z. Savage and A.F. Chleborad: Bulletin of the Association of Engineering Geologists, v. 20, no. 4, p. 455‑459.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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