The West Pacific pattern correlates with high pressure, increased temperature, decreased precipitation, and higher burned area during autumn in the western United States.
Cyclic changes of fluid pressure in fault zones can induce slow-slip events that advance in the direction of fluid flow, even when the faults are stable.
From hordes rushing into national parks to mourners holding glacier funerals, tourists wanting to take in threatened natural places may be shifting visitation patterns.
The Landslide Blog is written by Dave Petley, who is widely recognized as a world leader in the study and management of landslides. Back in 2022, I wrote (on the old site) about a landslide that ...
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