If you missed last week’s live session, you can now watch the full recording here:
🔗 www.youtube.com/watch?v=tuhd...
If you missed last week’s live session, you can now watch the full recording here:
🔗 www.youtube.com/watch?v=tuhd...
This has been known to seismologists for decades, because we can see the permanent offset in our seismograms. With large earthquakes, even 100s of km will still cause mm of offset.
This has been known to seismologists for decades, because we can see the permanent offset in our seismograms. With large earthquakes, even 100s of km will still cause mm of offset.
👉 www.isprs2026toronto.com/special-sess...
#InSAR #DisasterRiskReduction #ISPRS2026
👉 www.isprs2026toronto.com/special-sess...
#InSAR #DisasterRiskReduction #ISPRS2026
www.linkedin.com/posts/franzm...
www.linkedin.com/posts/franzm...
youtu.be/8SGIrUTRpq0?...
youtu.be/8SGIrUTRpq0?...
www.youtube.com/watch?v=sLjv...
www.youtube.com/watch?v=sLjv...
Properly staggering! 😮😱
Properly staggering! 😮😱
@CopernicusEU
#RemoteSensing #EO #Iran
@CopernicusEU
#RemoteSensing #EO #Iran
A comprehensive analysis of GNSS‑derived velocities, strain rates, stress orientations, and seismic anisotropy along the Alpine‑Himalayan (Tethyan) Belt—from Iberia to Southeast Asia:
🔗 doi.org/10.22541/ess...
#GNSS #Tectonics #StrainRates #Geodesy
A comprehensive analysis of GNSS‑derived velocities, strain rates, stress orientations, and seismic anisotropy along the Alpine‑Himalayan (Tethyan) Belt—from Iberia to Southeast Asia:
🔗 doi.org/10.22541/ess...
#GNSS #Tectonics #StrainRates #Geodesy
Community-driven natural hazard and physical vulnerability assessment – developing a collaborative understanding
23rd April 2025 at 4pm UK time
Dr Annie Winson
BGS, UK
Please register at:
ukri.zoom.us/webinar/regi...
Community-driven natural hazard and physical vulnerability assessment – developing a collaborative understanding
23rd April 2025 at 4pm UK time
Dr Annie Winson
BGS, UK
Please register at:
ukri.zoom.us/webinar/regi...
evrimagaci.org/dertuncay/
evrimagaci.org/dertuncay/
Prelim. source models point to rupture duration & length of ~120s and at least 200km. It likely filled large part of seismic gap S of Sagaing (previous rupture in 1839) ⚒️ 🧪
Map from doi.org/10.1002/2013... (Wang et al.)
1/n
Prelim. source models point to rupture duration & length of ~120s and at least 200km. It likely filled large part of seismic gap S of Sagaing (previous rupture in 1839) ⚒️ 🧪
Map from doi.org/10.1002/2013... (Wang et al.)
1/n