Increased flood exposure in the Pacific Northwest following earthquake-driven subsidence and sea-level rise. [PDF]
Dura T +19 more
europepmc +1 more source
The formation mechanism of the Liantang trough in Qiaojia County along the Jinsha River. [PDF]
Song L, Shang Y, Wang Y, Chang Z.
europepmc +1 more source
Active protothrusts and fluid highways: Seismic noise reveals hidden subduction dynamics in Cascadia. [PDF]
Kidiwela M +3 more
europepmc +1 more source
Magnitude determination for earthquake early warning using P-alert low-cost sensors during 2024 Mw7.4 Hualien, Taiwan earthquake. [PDF]
Lin YH, Wu YM.
europepmc +1 more source
Coral geochemical response to uplift in the aftermath of the 2005 Nias-Simeulue earthquake. [PDF]
Sosdian SM +9 more
europepmc +1 more source
Long term carbon export from mountain forests driven by hydroclimate and extreme event driven landsliding. [PDF]
Howarth JD +8 more
europepmc +1 more source
From foreshock to mainshock: transient sliding velocity sets nucleation time
Fryer B +3 more
europepmc +1 more source
Effects of slope instability on coseismic landslide susceptibility during earthquakes
openaire +1 more source
Limits to coseismic landslides triggered by Cascadia Subduction Zone earthquakes [PDF]
Landslides are a significant hazard and dominant feature throughout the landscape of the Pacific Northwest. However, the hazard and risk posed by coseismic landslides triggered by great Cascadia Subduction Zone (CSZ) earthquakes is highly uncertain due to a lack of local and global data.
William Struble
exaly +3 more sources
Related searches:
A numerical simulation of seismic signals of coseismic landslides
Engineering Geology, 2021Abstract When a coseismic landslide is triggered by an earthquake, seismic stations close to the location of the landslide will simultaneously record the seismic signals caused by the earthquake and landslide, causing confusion between the two signals.
Zheng-Yi Feng
exaly +2 more sources

