A USGS scientist stands in a crack in tide flat sediment that opened during strong shaking in the November 30, 2018 Anchorage earthquake. This upland ground crack near Cottonwood Creek, Palmer Slough had horizontal displacements of ~2.5ft locally and observed maximum depth of ~3ft. The crack was observed ~150ft from the active river channel.
Alex Grant
Alex is a Research Engineer specializing in regional-scale landslide and liquefaction hazards and risk.
Alex got his Ph.D. in 2017 from the University of Washington where he studied coseismic landslide hazard and risk in Lebanon, New Zealand, Japan, and the Pacific Northwest of N. America. Alex received his BSCE from Tufts University in 2013 and a MSE in 2014 from the University of Washington in Geotechnical Engineering. Alex joined the USGS in 2018 to research earthquake-induced ground failures, and is actively working on projects in the Pacific Northwest and California.
Science and Products
Crustal Characterization
Landslide Headscarps in Marine Terraces along the Pacific Coast of Washington and Oregon
Coseismic landslide runout and mobility ratio data from publicly available mapped landslide inventories
Cone Penetration Test data of Paleoliquefaction sites in Washington and Oregon
Bedrock stratigraphic and structural data and deep-seated landslide density for the Tyee Formation, OR, USA
Compiled onshore and offshore paleoseismic data along the Cascadia Subduction zone
Field reconnaissance of ground failure triggered by shaking during the 2018 M7.1 Anchorage, Alaska, earthquake
Field observations of ground failure triggered by the 2020 Puerto Rico earthquake sequence
A USGS scientist stands in a crack in tide flat sediment that opened during strong shaking in the November 30, 2018 Anchorage earthquake. This upland ground crack near Cottonwood Creek, Palmer Slough had horizontal displacements of ~2.5ft locally and observed maximum depth of ~3ft. The crack was observed ~150ft from the active river channel.
A USGS scientist investigates cracks along Trunk Road in Wasilla, Alaska. Extensional crack and damage to roadway along S Trunk Rd.
A USGS scientist investigates cracks along Trunk Road in Wasilla, Alaska. Extensional crack and damage to roadway along S Trunk Rd.
Exposed sand within a extensional crack along the Knik River, Alaska. Measuring a crack in sandy sediment along the south bank of the Knik River. This crack was one of many that opened across the Anchorage and Mat-Su region due to strong shaking during the M7.1 November 30, 2018 Anchorage earthquake.
Exposed sand within a extensional crack along the Knik River, Alaska. Measuring a crack in sandy sediment along the south bank of the Knik River. This crack was one of many that opened across the Anchorage and Mat-Su region due to strong shaking during the M7.1 November 30, 2018 Anchorage earthquake.
Global patterns of coseismic landslide runout mobility differ from aseismic landslide trends
Complex landslide patterns explained by local intra-unit variability of stratigraphy and structure: Case study in the Tyee Formation, Oregon, USA
Evidence of Seattle Fault earthquakes from patterns of deep-seated landslides
3-D wave propagation simulations of Mw 6.5+ earthquakes on the Tacoma Fault, Washington state, considering the effects of topography, a geotechnical gradient, and a fault damage zone
Limits to coseismic landslides triggered by Cascadia Subduction Zone earthquakes
Regional-scale liquefaction analyses
Changes in liquefaction severity in the San Francisco Bay Area with sea-level rise
The normal faulting 2020 Mw5.8 Lone Pine, Eastern California earthquake sequence
Site response, basin amplification, and earthquake stress drops in the Portland, Oregon area
Ensemble ShakeMaps for magnitude 9 earthquakes on the Cascadia Subduction Zone
A generic soil velocity model that accounts for near-surface conditions and deeper geologic structure
Rainfall triggers more deep-seated landslides than Cascadia earthquakes in the Oregon Coast Range, USA
Liquefaction and Sea-Level Rise
Science and Products
Crustal Characterization
Landslide Headscarps in Marine Terraces along the Pacific Coast of Washington and Oregon
Coseismic landslide runout and mobility ratio data from publicly available mapped landslide inventories
Cone Penetration Test data of Paleoliquefaction sites in Washington and Oregon
Bedrock stratigraphic and structural data and deep-seated landslide density for the Tyee Formation, OR, USA
Compiled onshore and offshore paleoseismic data along the Cascadia Subduction zone
Field reconnaissance of ground failure triggered by shaking during the 2018 M7.1 Anchorage, Alaska, earthquake
Field observations of ground failure triggered by the 2020 Puerto Rico earthquake sequence
A USGS scientist stands in a crack in tide flat sediment that opened during strong shaking in the November 30, 2018 Anchorage earthquake. This upland ground crack near Cottonwood Creek, Palmer Slough had horizontal displacements of ~2.5ft locally and observed maximum depth of ~3ft. The crack was observed ~150ft from the active river channel.
A USGS scientist stands in a crack in tide flat sediment that opened during strong shaking in the November 30, 2018 Anchorage earthquake. This upland ground crack near Cottonwood Creek, Palmer Slough had horizontal displacements of ~2.5ft locally and observed maximum depth of ~3ft. The crack was observed ~150ft from the active river channel.
A USGS scientist investigates cracks along Trunk Road in Wasilla, Alaska. Extensional crack and damage to roadway along S Trunk Rd.
A USGS scientist investigates cracks along Trunk Road in Wasilla, Alaska. Extensional crack and damage to roadway along S Trunk Rd.
Exposed sand within a extensional crack along the Knik River, Alaska. Measuring a crack in sandy sediment along the south bank of the Knik River. This crack was one of many that opened across the Anchorage and Mat-Su region due to strong shaking during the M7.1 November 30, 2018 Anchorage earthquake.
Exposed sand within a extensional crack along the Knik River, Alaska. Measuring a crack in sandy sediment along the south bank of the Knik River. This crack was one of many that opened across the Anchorage and Mat-Su region due to strong shaking during the M7.1 November 30, 2018 Anchorage earthquake.