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Most of my research is related to earthquake and tsunami hazards in Alaska, with a focus on paleoseismology, submarine landslides, and active faulting. I am the Alaska Coordinator for the Earthquake Hazards Program of the USGS. I also study various aspects of the framework geology of Alaska, with a focus on neotectonics and tectonics.
I use various tools to understand earthquakes and earthquake hazards in Alaska. I’ve studied the tectonic evolution of parts of Alaska, accretionary prisms along Alaska’s margin, forearc and splay faulting, submarine landslides, mountain building and exhumation, landscape evolution, glacial histories, and sedimentary basins. I’ve worked with marine and terrestrial seismic reflection and potential field data. Current work is focused on lacustrine paleoseismology, splay faulting, and various seismic hazards projects.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
To better understand the geophysical characteristics and seismic history of the Cascadia Subduction Zone, USGS researchers conduct fieldwork at sea to collect evidence of turbidity currents from underwater landslides likely caused by earthquake shaking.
To better understand the geophysical characteristics and seismic history of the Cascadia Subduction Zone, USGS researchers conduct fieldwork at sea to collect evidence of turbidity currents from underwater landslides likely caused by earthquake shaking.
Ocean bottom seismometers being loaded onto the R/V Sikuliaq to be deployed on the sea floor in the Gulf of Alaska.
Ocean bottom seismometers being loaded onto the R/V Sikuliaq to be deployed on the sea floor in the Gulf of Alaska.
Stratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
Stratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
USGS and Geological Survey of Canada scientists sample sediment cores collected from the sea floor along the Queen Charlotte Fault. This was taken while they were working with (or in) the Geological Survey of Canada.
USGS and Geological Survey of Canada scientists sample sediment cores collected from the sea floor along the Queen Charlotte Fault. This was taken while they were working with (or in) the Geological Survey of Canada.
USGS scientists deploy a seismic streamer aboard the R/V David Starr offshore of southeast Alaska to study the Queen Charlotte Fault.
USGS scientists deploy a seismic streamer aboard the R/V David Starr offshore of southeast Alaska to study the Queen Charlotte Fault.
Tyndall Glacier in Taan Fiord, Alaska, is a modern day remnant of the glaciers that once flowed over the Gulf of Alaska.
Tyndall Glacier in Taan Fiord, Alaska, is a modern day remnant of the glaciers that once flowed over the Gulf of Alaska.
USGS scientists investigate trees knocked over by the tsunami at the mouth of Taan Fjord. Flow depth here was likely 5 m based on the height of branches stripped off trees in the background. This event had the 4th highest tsunami runup ever recorded.
USGS scientists investigate trees knocked over by the tsunami at the mouth of Taan Fjord. Flow depth here was likely 5 m based on the height of branches stripped off trees in the background. This event had the 4th highest tsunami runup ever recorded.
USGS scientists collect seismic data to image the 2015 Taan Fjord landslide in southeast Alaska.
USGS scientists collect seismic data to image the 2015 Taan Fjord landslide in southeast Alaska.
USGS scientists work with academic collaborators from the University of Ghent (Belgium) to core earthquake-related submarine landslide deposits in Skilak Lake, Alaska.
USGS scientists work with academic collaborators from the University of Ghent (Belgium) to core earthquake-related submarine landslide deposits in Skilak Lake, Alaska.
Scientist leaning over side of R/V Alaskan Gyre adjusting the multibeam arm
Scientist leaning over side of R/V Alaskan Gyre adjusting the multibeam arm
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
This is a remarkable film of the underwater landslide and tsunami at Valdez, Alaska, taken during the 1964 Great Alaska earthquake.
It has never been seen before in its correct sequence. There is no other film that we are aware of that shows the formation of a large submarine landslide.
To better understand the geophysical characteristics and seismic history of the Cascadia Subduction Zone, USGS researchers conduct fieldwork at sea to collect evidence of turbidity currents from underwater landslides likely caused by earthquake shaking.
To better understand the geophysical characteristics and seismic history of the Cascadia Subduction Zone, USGS researchers conduct fieldwork at sea to collect evidence of turbidity currents from underwater landslides likely caused by earthquake shaking.
Ocean bottom seismometers being loaded onto the R/V Sikuliaq to be deployed on the sea floor in the Gulf of Alaska.
Ocean bottom seismometers being loaded onto the R/V Sikuliaq to be deployed on the sea floor in the Gulf of Alaska.
Stratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
Stratigraphic contact marking uplift of Montague Island, caused by slip on the Patton Bay fault system during the 1964 M9.2 Great ALaska Earthquake.
USGS and Geological Survey of Canada scientists sample sediment cores collected from the sea floor along the Queen Charlotte Fault. This was taken while they were working with (or in) the Geological Survey of Canada.
USGS and Geological Survey of Canada scientists sample sediment cores collected from the sea floor along the Queen Charlotte Fault. This was taken while they were working with (or in) the Geological Survey of Canada.
USGS scientists deploy a seismic streamer aboard the R/V David Starr offshore of southeast Alaska to study the Queen Charlotte Fault.
USGS scientists deploy a seismic streamer aboard the R/V David Starr offshore of southeast Alaska to study the Queen Charlotte Fault.
Tyndall Glacier in Taan Fiord, Alaska, is a modern day remnant of the glaciers that once flowed over the Gulf of Alaska.
Tyndall Glacier in Taan Fiord, Alaska, is a modern day remnant of the glaciers that once flowed over the Gulf of Alaska.
USGS scientists investigate trees knocked over by the tsunami at the mouth of Taan Fjord. Flow depth here was likely 5 m based on the height of branches stripped off trees in the background. This event had the 4th highest tsunami runup ever recorded.
USGS scientists investigate trees knocked over by the tsunami at the mouth of Taan Fjord. Flow depth here was likely 5 m based on the height of branches stripped off trees in the background. This event had the 4th highest tsunami runup ever recorded.
USGS scientists collect seismic data to image the 2015 Taan Fjord landslide in southeast Alaska.
USGS scientists collect seismic data to image the 2015 Taan Fjord landslide in southeast Alaska.
USGS scientists work with academic collaborators from the University of Ghent (Belgium) to core earthquake-related submarine landslide deposits in Skilak Lake, Alaska.
USGS scientists work with academic collaborators from the University of Ghent (Belgium) to core earthquake-related submarine landslide deposits in Skilak Lake, Alaska.
Scientist leaning over side of R/V Alaskan Gyre adjusting the multibeam arm
Scientist leaning over side of R/V Alaskan Gyre adjusting the multibeam arm
*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
