An International Tsunami Survey Team studying the effects of the December 26, 2004 tsunami on Indonesia“‘’’s island of Sumatra documented wave heights of 20 to 30 m (65 to 100 ft) at the island's northwest end and found evidence suggesting that wave heights may have ranged from 15 to 30 m (50 to 100 ft) along at least a 100-km (60 mi) stretch of the northwest coast.
Guy Gelfenbaum
Oceanographer Emeritus with the USGS Pacific Coastal and Marine Science Center in Santa Cruz, California
Ecosystem Dynamics, Project Chief: Coastal Habitats in Puget Sound - The goal of these projects is to develop scientific information and tools to support natural resource managers in the adaptive management of critical nearshore ecosystems in Puget Sound
Large-Scale Coastal Change, Project Chief: Southwest Washington Coastal Erosion Study - Research involves understanding complex relationships among sediment supply, littoral processes, and shoreline erosion or accretion in a high-energy coastal environment. Studies encompass multiple time and space scales of coastal evolution, and successfully differentiate natural and anthropogenic influences on coastal change.
Catastrophic Geologic Hazards, Co-Principal Investigator: Tsunami Hazards Study - Research effort to improve our understanding of tsunami hazards through identification and interpretation of sediments deposited from tsunamis
Professional Experience
2022: Oceanographer Emeritus, Pacific Coastal and Marine Science Center
2017-2021: Center Director, Pacific Coastal and Marine Science Center
Education and Certifications
1988 Ph.D. Geological Oceanography - University of Washington, Seattle
1982 M.S. Geological Oceanography - University of Washington, Seattle
1978 B.S. Geology - University of Wisconsin, Madison
Science and Products
Sediment Transport in Coastal Environments
Columbia River estuary
Tsunami Hazards, Modeling, and the Sedimentary Record
Estuaries and large river deltas in the Pacific Northwest
USGS science supporting the Elwha River Restoration Project
Tsunami Field Studies
PS-CoSMoS FAQs
Puget Sound - Coastal Storm Modeling System (PS-CoSMoS) frequently asked questions
Preliminary Analysis of Sedimentary Deposits from the June 23, 2001 Peru Tsunami
Preliminary Analysis of Sedimentary Deposits from the July 17, 1998 Papua New Guinea Tsunami
Tsunami deposit data and sediment transport models from the Salmon River estuary, central Oregon
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2022
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2018
Beach topography and nearshore bathymetry of the Columbia River littoral cell, Washington and Oregon (ver. 4.0, January 2024)
Radiocarbon, Cesium-137, Grain Size, and X-ray Fluorescence Data for Tsunami Geology Investigation, Driftwood Bay, Umnak Island, Alaska (2018)
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2017
Core logs, scans, photographs, grain size, and radiocarbon data from coastal wetlands on the Hawaiian islands of Kaua`i, O`ahu, and Hawai`i
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington
Oceanographic measurements and hydrodynamic modeling of the mouth of the Columbia River, Oregon and Washington, 2013
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2012
Bathymetry and topography data from the Elwha River delta, Washington, May 2012
Bathymetry and topography data from the Elwha River delta, Washington, August 2011
An International Tsunami Survey Team studying the effects of the December 26, 2004 tsunami on Indonesia“‘’’s island of Sumatra documented wave heights of 20 to 30 m (65 to 100 ft) at the island's northwest end and found evidence suggesting that wave heights may have ranged from 15 to 30 m (50 to 100 ft) along at least a 100-km (60 mi) stretch of the northwest coast.
A severely damaged home, or a portion of one, sits atop debris in Banda Aceh on the island of Sumatra. Damage was caused by a massive, highly destructive tsunami, triggered by a magnitude 9.1 earthquake just offshore of Sumatra, on December 26, 2004.
A severely damaged home, or a portion of one, sits atop debris in Banda Aceh on the island of Sumatra. Damage was caused by a massive, highly destructive tsunami, triggered by a magnitude 9.1 earthquake just offshore of Sumatra, on December 26, 2004.
Climate controls on longshore sediment transport and coastal morphology adjacent to engineered inlets
Testing megathrust rupture models using tsunami deposits
Nearshore subtidal community response during and after sediment disturbance associated with dam removal
Monitoring and modeling dispersal of a submerged nearshore berm at the mouth of the Columbia River, USA
Can modeling the geologic record contribute to constraining the tectonic source of the AD 1755 Great Lisbon earthquake?
Onshore flow characteristics of the 1755 CE Lisbon tsunami: Linking forward and inverse numerical modeling
Selective sediment transport during Hurricane Sandy on Fire Island (New York, USA): Inferences from heavy-mineral assemblages
Observations of coastal change and numerical modeling of sediment-transport pathways at the mouth of the Columbia River and its adjacent littoral cell
World’s largest dam removal reverses coastal erosion
Evidence for frequent, large tsunamis spanning locked and creeping parts of the Aleutian megathrust
Sedimentary evidence of prehistoric distant-source tsunamis in the Hawaiian Islands
Increased sediment load during a large-scale dam removal changes nearshore subtidal communities
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
Sediment Transport in Coastal Environments
Columbia River estuary
Tsunami Hazards, Modeling, and the Sedimentary Record
Estuaries and large river deltas in the Pacific Northwest
USGS science supporting the Elwha River Restoration Project
Tsunami Field Studies
PS-CoSMoS FAQs
Puget Sound - Coastal Storm Modeling System (PS-CoSMoS) frequently asked questions
Preliminary Analysis of Sedimentary Deposits from the June 23, 2001 Peru Tsunami
Preliminary Analysis of Sedimentary Deposits from the July 17, 1998 Papua New Guinea Tsunami
Tsunami deposit data and sediment transport models from the Salmon River estuary, central Oregon
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2022
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2018
Beach topography and nearshore bathymetry of the Columbia River littoral cell, Washington and Oregon (ver. 4.0, January 2024)
Radiocarbon, Cesium-137, Grain Size, and X-ray Fluorescence Data for Tsunami Geology Investigation, Driftwood Bay, Umnak Island, Alaska (2018)
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2017
Core logs, scans, photographs, grain size, and radiocarbon data from coastal wetlands on the Hawaiian islands of Kaua`i, O`ahu, and Hawai`i
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington
Oceanographic measurements and hydrodynamic modeling of the mouth of the Columbia River, Oregon and Washington, 2013
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2012
Bathymetry and topography data from the Elwha River delta, Washington, May 2012
Bathymetry and topography data from the Elwha River delta, Washington, August 2011
An International Tsunami Survey Team studying the effects of the December 26, 2004 tsunami on Indonesia“‘’’s island of Sumatra documented wave heights of 20 to 30 m (65 to 100 ft) at the island's northwest end and found evidence suggesting that wave heights may have ranged from 15 to 30 m (50 to 100 ft) along at least a 100-km (60 mi) stretch of the northwest coast.
An International Tsunami Survey Team studying the effects of the December 26, 2004 tsunami on Indonesia“‘’’s island of Sumatra documented wave heights of 20 to 30 m (65 to 100 ft) at the island's northwest end and found evidence suggesting that wave heights may have ranged from 15 to 30 m (50 to 100 ft) along at least a 100-km (60 mi) stretch of the northwest coast.
A severely damaged home, or a portion of one, sits atop debris in Banda Aceh on the island of Sumatra. Damage was caused by a massive, highly destructive tsunami, triggered by a magnitude 9.1 earthquake just offshore of Sumatra, on December 26, 2004.
A severely damaged home, or a portion of one, sits atop debris in Banda Aceh on the island of Sumatra. Damage was caused by a massive, highly destructive tsunami, triggered by a magnitude 9.1 earthquake just offshore of Sumatra, on December 26, 2004.
Climate controls on longshore sediment transport and coastal morphology adjacent to engineered inlets
Testing megathrust rupture models using tsunami deposits
Nearshore subtidal community response during and after sediment disturbance associated with dam removal
Monitoring and modeling dispersal of a submerged nearshore berm at the mouth of the Columbia River, USA
Can modeling the geologic record contribute to constraining the tectonic source of the AD 1755 Great Lisbon earthquake?
Onshore flow characteristics of the 1755 CE Lisbon tsunami: Linking forward and inverse numerical modeling
Selective sediment transport during Hurricane Sandy on Fire Island (New York, USA): Inferences from heavy-mineral assemblages
Observations of coastal change and numerical modeling of sediment-transport pathways at the mouth of the Columbia River and its adjacent littoral cell
World’s largest dam removal reverses coastal erosion
Evidence for frequent, large tsunamis spanning locked and creeping parts of the Aleutian megathrust
Sedimentary evidence of prehistoric distant-source tsunamis in the Hawaiian Islands
Increased sediment load during a large-scale dam removal changes nearshore subtidal communities
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.