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Modeling the dynamics of lahars that originate as landslides on the west side of Mount Rainier, Washington

George, David L., Iverson, Richard M., Cannon, Charles M.·2022·Open-File Report
DOI 10.3133/ofr20211118
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Research works printed but not linked: 35

  1. Allstadt, K., 2013, Extracting source characteristics and dynamics of the August 2010 Mount Meager landslide from broadband seismograms: Journal of Geophysical Research, v. 118, no. 3, p. 1472-1490, https://doi.org/10.1002/ jgrf.20110. · DOI
  2. Berger, M.J., and Colella, P., 1989, Local adaptive mesh refinement for shock hydrodynamics: Journal of Computational Physics, v. 82, no. 1, p. 64-84, https://doi.org/10.1016/0021-9991(89)90035-1. · DOI
  3. Berger, M.J., and Oliger, J., 1984, Adaptive mesh refinement for hyperbolic partial differential equations: Journal of Computational Physics, v. 53, no. 3, p. 484-512, https://doi.org/10.1016/0021-9991(84)90073-1. · DOI
  4. Berger, M.J., George, D.L., LeVeque, R.J., and Mandli, K.T., 2011, The GeoClaw software for depth-averaged flows with adaptive refinement: Advances in Water Resources, v. 34, no. 9, p. 1195-1206, https://doi.org/10.1016/ j.advwatres.2011.02.016. · DOI
  5. Crandell, D.R., and Waldron, H.H., 1956, A recent volcanic mudflow of exceptional dimensions from Mount Rainier, Washington: American Journal of Science, v. 254, p. 349-362, https://doi.org/10.2475/ajs.254.6.349. · DOI
  6. Crandell, D.R., 1971, Postglacial lahars from Mount Rainier volcano, Washington: U.S. Geological Survey Professional Paper 677, 75 p., https://doi.org/10.3133/pp677. · DOI
  7. Czuba, J.A., Olsen, T.D., Czuba, C.R., Magirl, C.S., and Gish, C.C., 2012, Changes in sediment volume in Alder Lake, Nisqually River Basin, Washington, 1945-2011: U.S. Geological Survey Open-File Report 2012-1068, 30 p., https://doi.org/10.3133/ofr20121068. · DOI
  8. Finn, C.A., Sisson, T.W., and Deszcz-Pan, M., 2001, Aerogeo- physical measurements of collapse-prone hydrothermally altered zones at Mount Rainier volcano: Nature, v. 409, p. 600-609, https://doi.org/10.1038/35054533. · DOI
  9. George, D.L., 2006, Finite volume methods and adaptive refinement for tsunami propagation and inundation: Seattle, University of Washington, Ph.D. dissertation, 167 p.
  10. George, D.L., 2008, Augmented Riemann solvers for the shallow water equations over variable topography with steady states and inundation: Journal of Computational Physics, v. 227, no. 6, p. 3089-3113, https://doi.org/ 10.1016/j.jcp.2007.10.027. · DOI
  11. George, D.L., 2011, Adaptive finite volume methods with well-balanced Riemann solvers for modeling floods in rugged terrain-Application to the Malpasset dam-break flood (France, 1959): International Journal for Numerical Methods in Fluids, v. 66, no. 8, p. 1000-1018, https://doi.org/10.1002/fld.2298. · DOI
  12. George, D.L. and Iverson, R.M., 2014, A depth-averaged debris-flow model that includes the effects of evolving dilatancy-II. Numerical predictions and experimental tests: Proceedings of the Royal Society A, v. 470, no. 2170, 31 p., https://doi.org/10.1098/rspa.2013.0820. · DOI
  13. George, D.L., Iverson, R.M., and Cannon, C.M., 2017, New methodology for computing tsunami generation by subaerial landslides-Application to the 2015 Tyndall Glacier landslide, Alaska: Geophysical Research Letters, v. 44, no. 14, p. 7276-7284, https://doi.org/10.1002/ 2017GL074341. · DOI
  14. Guthrie, R.H., Friele, P., Allstadt, K., Roberts, N., Evans, S.G., Delaney, K.B., Roche, D., and Clague, J.J., 2012, The 6 August 2010 Mount Meager rock slide-debris flow, Coast Mountains, British Columbia-Characteristics, dynamics, and implications for hazard and risk assessment: Natural Hazards and Earth System Sciences, v. 12, no. 5, p. 1277-1294, https://doi.org/10.5194/nhess-12-1277-2012. · DOI
  15. Hoblitt, R.P., Walder, J.S., Driedger, C.L., Scott, K.M., Pringle, P.T., and Vallance, J.W., 1998, Volcano hazards from Mount Rainier, Washington, revised 1998: U.S. Geological Survey Open-File Report 98-428, 11 p., https://doi.org/10.3133/ofr98428. · DOI
  16. Iverson, R.M., and George, D.L., 2014, A depth-averaged debris-flow model that includes the effects of evolving dilatancy-I. Physical basis: Proceedings of the Royal Society A, v. 470, no. 2170, 31 p., https://doi.org/10.1098/ rspa.2013.0819. · DOI
  17. Iverson, R.M., and George, D.L., 2016, Modelling landslide liquefaction, mobility bifurcation and the dynamics of the 2014 Oso disaster: Geotechnique, v. 66, no. 3, p. 175-187, https://doi.org/10.1680/jgeot.15.LM.004. · DOI
  18. Iverson, R.M., George, D.L., Allstadt, K., Reid, M.E., Collins, B.D., Vallance, J.W., Schilling, S.P., Godt, J.W., Cannon, C.M., Magirl, C.S., Baum, R.L., Coe, J.A., Schulz, W.H., and Bower, J.B., 2015, Landslide mobility and hazards-Implications of the 2014 Oso disaster: Earth and Planetary Science Letters, v. 412, p. 197-208, https://doi. org/10.1016/j.epsl.2014.12.020. · DOI
  19. Iverson, R.M., Logan, M., LaHusen, R.G., and Berti, M., 2010, The perfect debris flow?-Aggregated results from 28 large-scale experiments: Journal of Geophysical Research Earth Surface, v. 115, no. F3, article F03005, 29 p., https://doi.org/10.1029/2009JF001514. · DOI
  20. Iverson, R.M., Schilling, S.P., and Vallance, J.W., 1998, Objec- tive delineation of lahar-inundation hazard zones: Geologi- cal Society of America Bulletin, v. 110, no. 8, p. 972-984, https://doi.org/10.1130/0016-7606(1998)110%3C0972:OD OLIH%3E2.3.CO;2. Iverson, R.M., George, D.L., and Logan, M., 2016, Debris flow runup on vertical barriers and adverse slopes: Journal of Geophysical Research Earth Surface, v. 121, no. 12, p. 2333-2357, https://doi.org/10.1002/2016JF003933. · DOI
  21. Jaboyedoff, M., Carrea, D., Derron, M.H., Oppikofer, T., Penna, I.M., and Rudaz, B., 2020, A review of methods used to estimate initial landslide failure surface depths and volumes: Engineering Geology, v. 267, article 105478, 18 p., https://doi.org/10.1016/j.enggeo.2020.105478. · DOI
  22. Jefferies, M., and Been, K., 2016, Soil liquefaction-A critical state approach (2d ed.): Boca Raton, Fla., CRC Press, 712 p.
  23. LeVeque, R.J., 2002, Finite volume methods for hyperbolic problems: Cambridge Texts in Applied Mathematics, v. 31, 558 p., https://doi.org/10.1017/CBO9780511791253. · DOI
  24. LeVeque, R.J., George, D.L., and Berger, M.J., 2011, Tsunami modelling with adaptively refined finite volume methods: Acta Numerica, v. 20, p. 211-289, https://doi.org/10.1017/ S0962492911000043. · DOI
  25. Major, J.J., Iverson, R.M., McTigue, D.F., Macias, S., and Fiedorowicz, B.K., 1997, Geotechnical properties of debris- flow sediments and slurries, in Chen, Cheng-lung, ed., Debris-flow hazards mitigation-Mechanics, prediction, and assessment-Proceedings of First International Conference, San Francisco, Calif., August 7-9, 1997: New York, American Society of Civil Engineers, p. 249-259.
  26. Mandli, K.T., Ahmadia, A.J., Berger, M.J., Calhoun, D., George, D.L., Hadjimichael, Y., Ketcheson, D.I., Lemoine, G.I., and LeVeque, R.J., 2016, Clawpack-Building an open source ecosystem for solving hyperbolic PDEs: PeerJ Computer Science, v. 2, 27 p., https://doi.org/10.7717/ peerj-cs. · DOI
  27. Moretti, L., Allstadt, K., Mangeney, A., Capdeville, Y., Stutzmann, E., and Bouchut, F., 2015, Numerical modeling of the Mount Meager landslide constrained by its force history derived from seismic data: Journal of Geophysical Research Solid Earth, v. 120, no. 4, p. 2579-2599, https://doi.org/10.1002/2014JB011426. · DOI
  28. Pierson, T.C., and Scott, K.M., 1985, Downstream dilution of a lahar-Transition from debris flow to hyperconcentrated streamflow: Water Resources Research, v. 21, no. 10, p. 1511-1524, https://doi.org/10.1029/WR021i010p01511. · DOI
  29. Reid, M.E., Christian, S.B., Brien, D.L., and Henderson, S.T., 2015, Scoops3D-Software to analyze 3D slope stability throughout a digital landscape: U.S. Geological Survey Techniques and Methods, book 14, chap. A1, 218 p., https://doi.org/10.3133/tm14A1. · DOI
  30. Reid, M.E., Sisson, T.W., and Brien, D.L., 2001, Volcano collapse promoted by hydrothermal alteration and edifice shape, Mount Rainer, Washington: Geology, v. 29, no. 9, p. 779-782, https://doi.org/10.1130/0091- 7613(2001)029%3C0779:VCPBHA%3E2.0.CO;2. · DOI · Paper page
  31. Roberti, G., Friele, P., van Wyk de Vries, B., Ward, B., Clague, J.J., Perotti, L., and Giardino, M., 2017, Rheological evolution of the Mount Meager 2010 debris avalanche, southwestern British Columbia: Geosphere, v. 13, no. 2, p. 369-390, https://doi.org/10.1130/GES01389. · DOI
  32. Schilling, S.P., 1998, LAHARZ-GIS programs for automated mapping of lahar-inundation hazard zones: U.S. Geological Survey Open-File Report 98-638, 80 p., https://doi.org/ 10.3133/ofr98638. · DOI
  33. Scott, K.M., Vallance, J.W., and Pringle, P.T., 1995, Sedimentology, behavior, and hazards of debris flows at Mount Rainier, Washington: U.S. Geological Survey Professional Paper 1547, 56 p., https://doi.org/10.3133/ pp1547. · DOI
  34. Sisson, T.W., and Vallance, J.W., 2009, Frequent eruptions of Mount Rainier over the last ~2,600 years: Bulletin of Volcanology, v. 71, p. 595-618, https://doi.org/10.1007/ s00445-008-0245-7. · DOI
  35. Vallance, J.W., and Scott, K.M., 1997, The Osceola Mudflow from Mount Rainier-Sedimentology and hazard implications of a huge clay-rich debris flow: Geological Society of America Bulletin, v. 109, no. 2, p. 143-163, https://doi.org/10.1130/0016-7606(1997)109%3C0143:TO MFMR%3E2.3.CO;2. Moffett Field Publishing Service Center, California Manuscript approved for publication December 3, 2021 Edited by Tim Herold Layout and design by Kimber Petersen · DOI

Cited by

Metadata

Authors
George, D. L., Iverson, R. M., & Cannon, C. M.
ORCID
Venue
Open-File Report
Publisher
US Geological Survey
Published
2022
ISSN
2331-1258
DOI
10.3133/ofr20211118
Cited by
12
References
0

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