Jon Major
My research focuses on hydrological hazards associated with volcanic eruptions and landscape responses to large inputs of sediment, including from dam removals. Projects focus on: (1) identifying hydrogeomorphic processes altered by volcanic disturbance; (2) evaluating hydrogeomorphic consequences; and (3) quantifying characteristic hydrogeomorphic response times and durations.
Professional Experience
Scientist-in-Charge, USGS Cascades Volcano Observatory, 2021–present
Research hydrologist, USGS Cascades Volcano Observatory, 1997–2021
Hydrologist, USGS Cascades Volcano Observatory, 1993–1997
Geologist, USGS Cascades Volcano Observatory, 1984–1993
Hydrologic field assistant, technician, USGS Cascades Volcano Observatory, 1982–1984
Other professional service:
Panel member, GSA Quaternary Geology and Geomorphology (QG&G) Division, 2002-2004
Secretary, GSA QG&G Division, 2006-2012
Member, International Organizing Committee, International Debris Flow Hazards Mitigation Conferences (DFHM), 2008-2015
Chair, DFHM IOC, 2008-2012Chair, DFHM IOC, 2008-2012
Co-chair of local planning committee for IAVCEI 2017 Scientific Assembly, Portland,
Education and Certifications
University of Dayton, B.S., 1980, Geology
The Pennsylvania State University, M.S., 1984, Geology
University of Washington, Ph.D., 1996, Geology
Affiliations and Memberships*
Geological Society of America
American Geophysical Union
International Association of Volcanology and Chemistry of Earth's Interior (IAVCEI)
American Avalanche Association (Member affiliate)
Editor:
Associate editor, Geological Society of America Bulletin, 2000-2011
Associate editor, Journal of Geophysical Research–Earth Surface, 2010-2014
Review editor, Frontiers in Volcanology, 2014 - Present
Co-editor, Geological Society of America Special Paper 375, Natural Hazards in El Salvador
Co-editor, Debris Flow Hazards Mitigation--Mechanics, Prediction, and Assessment: Proceedings of 4th International Conference on Debris Flow Hazards Mitigation (Millpress)
Chief guest editor, Andean Geology issue focused on the eruption of Chaitén Volcano (2013, v. 40(2))
Honors and Awards
Fellow, Geological Society of America (GSA)
E.B. Burwell Award, GSA, 1991
University of Dayton Alumni Special Achievement Award, 1999
Kirk Bryan Award, GSA, 2008
DOI Superior Service Award, 2018
Science and Products
My research publications can be parsed among various disciplinary studies. A full listing can be found on my Google Scholar profile (search for this via your web browser) and under the publications tab listing below. Publication topics include:
- Landslides, debris flows, and slurry rheology
- Volcanic eruptions and volcaniclastic processes (lahars, pyroclastic flows)
- Hydrogeomorphic responses to eruptions
- Geomorphic and ecologic responses to dam removals
- Photogrammetric analyses of eruptive processes
Lahar—River of volcanic mud and debris
Sediment erosion and delivery from Toutle River basin after the 1980 eruption of Mount St. Helens: A 30-year perspective
Geomorphic response of the Muddy River Basin to the 1980 eruptions of Mount St. Helens, 1980–2000
Geomorphic responses to dam removal in the United States – a two-decade perspective
The geologic, geomorphic, and hydrologic context underlying options for long-term management of the Spirit Lake outlet near Mount St. Helens, Washington
Surface morphology of caldera-forming eruption deposits revealed by lidar mapping of Crater Lake National Park, Oregon- Implications for emplacement and surface modification
Dam removal: Listening in
Landscape context and the biophysical response of rivers to dam removal in the United States
Camera system considerations for geomorphic applications of SfM photogrammetry
Extraordinary sediment delivery and rapid geomorphic response following the 2008–2009 eruption of Chaitén Volcano, Chile
Digital database of channel cross-section surveys, Mount St. Helens, Washington
Rapid reservoir erosion, hyperconcentrated flow, and downstream deposition triggered by breaching of 38 m tall Condit Dam, White Salmon River, Washington
Science and Products
- Science
- Data
- Publications
My research publications can be parsed among various disciplinary studies. A full listing can be found on my Google Scholar profile (search for this via your web browser) and under the publications tab listing below. Publication topics include:
- Landslides, debris flows, and slurry rheology
- Volcanic eruptions and volcaniclastic processes (lahars, pyroclastic flows)
- Hydrogeomorphic responses to eruptions
- Geomorphic and ecologic responses to dam removals
- Photogrammetric analyses of eruptive processes
Filter Total Items: 99Lahar—River of volcanic mud and debris
Lahar, an Indonesian word for volcanic mudflow, is a mixture of water, mud, and volcanic rock flowing swiftly along a channel draining a volcano. Lahars can form during or after eruptions, or even during periods of inactivity. They are among the greatest threats volcanoes pose to people and property. Lahars can occur with little to no warning, and may travel great distances at high speeds, destroyAuthorsJon J. Major, Thomas C. Pierson, James W. VallanceSediment erosion and delivery from Toutle River basin after the 1980 eruption of Mount St. Helens: A 30-year perspective
Exceptional sediment yields persist in Toutle River valley more than 30 years after the major 1980 eruption of Mount St. Helens. Differencing of decadal-scale digital elevation models shows the elevated load comes largely from persistent lateral channel erosion across the debris-avalanche deposit. Since the mid-1980s, rates of channel-bed-elevation change have diminished, and magnitudes of lateralAuthorsJon J. Major, Adam R. Mosbrucker, Kurt R. SpicerGeomorphic response of the Muddy River Basin to the 1980 eruptions of Mount St. Helens, 1980–2000
The 18 May 1980 eruption of Mount St. Helens produced a mosaic of primary landscape disturbances that decreased in intensity with distance from the volcano across the headwaters of Muddy River and its tributaries. Subsequent geomorphic responses were influenced by evolving hillslope and channel conditions that affected fluxes of water, sediment, and wood, as well as by an exceptional storm in FebrAuthorsThomas E. Lisle, Jon J. Major, J. H. HardisonGeomorphic responses to dam removal in the United States – a two-decade perspective
Recent decades have seen a marked increase in the number of dams removed in the United States. Investigations following a number of removals are beginning to inform how, and how fast, rivers and their ecosystems respond to released sediment. Though only a few tens of studies detail physical responses to removals, common findings have begun to emerge. They include: (1) Rivers are resilient and respAuthorsJon J. Major, Amy E. East, Jim E. O'Connor, Gordon E. Grant, Andrew C. Wilcox, Christopher S. Magirl, Matthias J. Collins, Desiree D. TullosThe geologic, geomorphic, and hydrologic context underlying options for long-term management of the Spirit Lake outlet near Mount St. Helens, Washington
The 1980 eruption of Mount St. Helens produced a massive landslide and consequent pyroclastic currents, deposits of which blocked the outlet to Spirit Lake. Without an outlet, the lake began to rise, threatening a breaching of the blockage and release of a massive volume of water. To mitigate the hazard posed by the rising lake and provide an outlet, in 1984–1985 the U.S. Army Corps of Engineers bAuthorsGordon E. Grant, Jon J. Major, Sarah L. LewisSurface morphology of caldera-forming eruption deposits revealed by lidar mapping of Crater Lake National Park, Oregon- Implications for emplacement and surface modification
Large explosive eruptions of silicic magma can produce widespread pumice fall, extensive ignimbrite sheets, and collapse calderas. The surfaces of voluminous ignimbrites are rarely preserved or documented because most terrestrial examples are heavily vegetated, or severely modified by post-depositional processes. Much research addresses the internal sedimentary characteristics, flow processes, andAuthorsJoel E. Robinson, Charles R. Bacon, Jon J. Major, Heather M. Wright, James W. VallanceDam removal: Listening in
Dam removal is widely used as an approach for river restoration in the United States. The increase in dam removals—particularly large dams—and associated dam-removal studies over the last few decades motivated a working group at the USGS John Wesley Powell Center for Analysis and Synthesis to review and synthesize available studies of dam removals and their findings. Based on dam removals thus farAuthorsMelissa M. Foley, James Bellmore, James E. O'Connor, Jeffrey J. Duda, Amy E. East, Gordon G. Grant, Chauncey W. Anderson, Jennifer A. Bountry, Mathias J. Collins, Patrick J. Connolly, Laura S. Craig, James E. Evans, Samantha Greene, Francis J. Magilligan, Christopher S. Magirl, Jon J. Major, George R. Pess, Timothy J. Randle, Patrick B. Shafroth, Christian E. Torgersen, Desiree D. Tullos, Andrew C. WilcoxByEcosystems Mission Area, Natural Hazards Mission Area, Water Resources Mission Area, Volcano Hazards Program, Forest and Rangeland Ecosystem Science Center, John Wesley Powell Center for Analysis and Synthesis, Oregon Water Science Center, Pacific Coastal and Marine Science Center, Volcano Science Center, Western Fisheries Research Center, Columbia River Research Laboratory (CRRL)Landscape context and the biophysical response of rivers to dam removal in the United States
Dams have been a fundamental part of the U.S. national agenda over the past two hundred years. Recently, however, dam removal has emerged as a strategy for addressing aging, obsolete infrastructure and more than 1,100 dams have been removed since the 1970s. However, only 130 of these removals had any ecological or geomorphic assessments, and fewer than half of those included before- and after-remoAuthorsMelissa M. Foley, Francis J. Magilligan, Christian E. Torgersen, Jon J. Major, Chauncey W. Anderson, Patrick J. Connolly, Daniel J. Wieferich, Patrick B. Shafroth, James E. Evans, Dana M. Infante, Laura CraigByEcosystems Mission Area, Water Resources Mission Area, Science Synthesis, Analysis and Research Program, Science Analytics and Synthesis (SAS) Program, Forest and Rangeland Ecosystem Science Center, John Wesley Powell Center for Analysis and Synthesis, Oregon Water Science Center, Pacific Coastal and Marine Science CenterCamera system considerations for geomorphic applications of SfM photogrammetry
The availability of high-resolution, multi-temporal, remotely sensed topographic data is revolutionizing geomorphic analysis. Three-dimensional topographic point measurements acquired from structure-from-motion (SfM) photogrammetry have been shown to be highly accurate and cost-effective compared to laser-based alternatives in some environments. Use of consumer-grade digital cameras to generate teAuthorsAdam R. Mosbrucker, Jon J. Major, Kurt R. Spicer, John PitlickExtraordinary sediment delivery and rapid geomorphic response following the 2008–2009 eruption of Chaitén Volcano, Chile
The 10 day explosive phase of the 2008–2009 eruption of Chaitén volcano, Chile, draped adjacent watersheds with a few cm to >1 m of tephra. Subsequent lava-dome collapses generated pyroclastic flows that delivered additional sediment. During the waning phase of explosive activity, modest rainfall triggered an extraordinary sediment flush which swiftly aggraded multiple channels by many meters. TenAuthorsJon J. Major, Daniel Bertin, Thomas C. Pierson, Alvaro Amigo, Andres Iroume, Hector Ulloa, Jonathan M. CastroDigital database of channel cross-section surveys, Mount St. Helens, Washington
Stream-channel cross-section survey data are a fundamental component to studies of fluvial geomorphology. Such data provide important parameters required by many open-channel flow models, sediment-transport equations, sediment-budget computations, and flood-hazard assessments. At Mount St. Helens, Washington, the long-term response of channels to the May 18, 1980, eruption, which dramatically alteAuthorsAdam R. Mosbrucker, Kurt R. Spicer, Jon J. Major, Dennis R. Saunders, Tami S. Christianson, Cole G. KingsburyRapid reservoir erosion, hyperconcentrated flow, and downstream deposition triggered by breaching of 38 m tall Condit Dam, White Salmon River, Washington
Condit Dam on the White Salmon River, Washington, a 38 m high dam impounding a large volume (1.8 million m3) of fine-grained sediment (60% sand, 35% silt and clay, and 5% gravel), was rapidly breached in October 2011. This unique dam decommissioning produced dramatic upstream and downstream geomorphic responses in the hours and weeks following breaching. Blasting a 5 m wide hole into the base of tAuthorsAndrew C. Wilcox, James E. O'Connor, Jon J. Major - News
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government