Results 61 to 70 of about 105,084 (302)
The Possible Observation of Slow Slip Events Prior to the Occurrence of the 1999 Chi-Chi Earthquake
Possible short-term precursors several days before the Taiwan Chi-Chi earthquake (Mw = 7.6) on 20 September 1999 were observed by examining crustal deformation that were directly integrated from broadband velocity seismograms.
Cheng-Horng Lin
doaj +1 more source
Disaster Governance and Challenges in a Rural Nepali Community: Notes from Future Village NGO [PDF]
More than two years after the 2015 earthquakes devastated Nepal, Katunge village in Dhading district, Nepal, remained as destroyed as it was right after the earthquake.
Khanna, Varun +2 more
core +1 more source
Slow slip events are regular earthquakes [PDF]
Abstract Slow slip events usually occur downdip of seismogenic zones in subduction megathrusts and crustal faults, with rupture speeds much slower than earthquakes. The empirical moment-duration scaling relation can help constrain the physical mechanism of slow slip events, yet it is still debated whether this scaling is linear or cubic and a ...
openaire +1 more source
From disorientation to preparedness: Information practices as scaffolding in acute crises
Abstract This qualitative study examines how adults in Israel enacted information practices during an acute national crisis. Using the information transitions framework, we investigate how concrete practices emerge and evolve across three stages: understanding, negotiating, and resolving. Semi‐structured Zoom interviews with 18 adults were analyzed via
Lilach Alon +2 more
wiley +1 more source
The Maintenance of Virtue Over Time: Notes on Changing Household Lives in Post-Disaster Nepal [PDF]
Although it is banal to say the series of earthquakes that hit Nepal in Spring 2015 will radically change the country, what this change will consist of still remains undetermined.
Haxby, Andrew W
core +2 more sources
The development of magmatism along the Cameroon Volcanic Line: evidence from seismicity and seismic anisotropy [PDF]
The Cameroon Volcanic Line (CVL) straddles the continent-ocean boundary in West Africa but exhibits no clear age progression. This renders it difficult to explain by traditional plume/plate motion hypotheses; thus, there remains no consensus on the ...
Bastow, I.D. +5 more
core +1 more source
Abstract The long‐term viability of Jatropha curcas as a biodiesel feedstock has been widely debated. Many early initiatives failed to deliver consistent economic returns despite promising environmental attributes. This study re‐evaluated J. curcas‐based systems within an integrated environmental–economic framework, focusing on their potential role in ...
Eduardo Sansão Sozinho Maurício +3 more
wiley +1 more source
Monitoring tectonic tremors is crucial for understanding stress release in subduction zones and assessing megathrust earthquake risk. The Hyuga‐nada region, at the western edge of the Nankai Trough, Japan, provides a natural laboratory for investigating ...
Kodai Sagae +3 more
doaj +1 more source
Low-frequency earthquakes along the Ryukyu Islands triggered by teleseismic earthquakes
Tremors and low-frequency earthquakes (LFEs), which occur in the plate interface, can provide useful information about the state of aseismic stress transfer in mega-earthquake fault zones.
Ayumi Kinjo, Mamoru Nakamura
doaj +1 more source
A mechanism for preseismic steady rupture fronts observed in laboratory experiments [PDF]
It has been shown that the onset of frictional instability is characterized by a transition from stable, quasi-static rupture growth to unstable, inertially-controlled high-speed rupture.
Ampuero, J.-P., Kaneko, Y.
core +1 more source

