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INDEPTH IV passive
As part of the INDEPTH IV passive-source experiment from May 2007 until October 2008, 50 broadband seismographs (35 from GIPP, Germany and 15 from SEIS-UK) were deployed along... -
Extended Pollino Seismic Experiment, 2014-2015, GFZ Potsdam (FEFI, Pompei, NE...
The temporary Extended Pollino Seismic Experiment (FDSN network code Y4) monitored the earthquake swarm in the Pollino Range region, Italy, between September 2014 and April... -
Anillo
The Anillo is a dense temporary seismic and geodetic network extending approximately 200 km along the strike of the subduction zone in North Chile in order to investigate how... -
DOCTAR
We installed two seismological broadband arrays on the volcanic oceanic island of Madeira and in western Portugal on continental crust for a comparison and combination with a... -
DARE: Dense ARray for seismic site effect Estimation
The project DARE proposes an integrated study of seismic site effects on the deep and elongated Messinian Rhône Canyon (French Rhône Valley). Lithological information from... -
Taskforce Tocopilla 2007
After the November 14, 2007 M7.7 Tocopilla earthquake in northern Chile, a local seismic network was installed in the rupture area between approximately Tocopilla and... -
DESIRE - Seismology (2006/2008)
For the seismology part of DESIRE 38 short period stations and 27 broadband stations were deployed in the area of the southern Dead Sea basin in Israel and Jordan. The... -
PUNA
The PUNA (Plateau Untersuchung Nw Argentinien) seismograph network was deployed across the Andes at ∼23.5°S. The array was centered in the backarc, atop the Puna high plateau in... -
The ANCORP Seismic Network
Local seismic network in Northern Chile, Southern Bolivia. (Grant-number: GIPP199604) Waveform data is available from the GEOFON data centre. License: “Creative Commons... -
The Irpinia seismic Array
Irpinia seismic Array is part of the DEnse mulTi-paramEtriC observations and 4D high resoluTion imaging (DETECT) project focused on the acquisition of a unique multiparametric... -
1-month seismological experiment on Etna, Italy in 2019
“1-month seismological experiment on Etna, Italy in 2019" is a 1-month seismological experi-ment realized near the Pizzi Deneri Observatory on Etna, Italy, by Eva Eibl and... -
TIPTEQ-Temporary seismological network (North) (2004/2005)
Understanding the factors leading to large earthquakes in the coupling zone of convergent margins and their interrelation with surface deformation were the main aims of the... -
The Jutland-to-Lower-Saxony (JULS) profile
This project investigates the crust and upper mantle along a north-south oriented, about 350 km long profile from around the town of Ringkøbing in western Jutland to south of... -
SMARTnet : Seismic Monitoring of the Armutlu Fault Zone
This field campaign aimed at densifying the station coverage on the Armutlu Peninsula in the eastern Sea of Marmara. The Armutlu peninsula is directly crossed by the Armutlu... -
Illgraben
The Illgraben is a 10 km² steep side valley located in Switzerland. This active debris flow catchment supplies 5-15% of the total sediment load of the Rhône River upstream of... -
2-year seismological experiment near Fagradalsfjall, Reykjanes peninsula in 2...
"2-year seismological experiment near Fagradalsfjall, Reykjanes peninsula in 2021/22" is a two-year seismological experiment realized near the eruptive site at Fagradalsfjall on... -
HART-La Palma volcanic eruption
Following a sequence of seismic events detected by the National Geographic Institute (IGN Spain), on 13.09.2021 the new volcano Cumbre Vieja initiated an eruption, located on... -
The COBO/CV-PLUME temporary seismic network
There is a growing debate on the conventional plume model and no consensus about their deep origin. Davaille et al. (2005) showed, using fluid mechanics experiments, the... -
Seismic sensing of hydraulic and sediment transport patterns below frozen sub...
Our understanding of the effects of ice on channel morphodynamics and bedload transport in northern rivers, frozen for several months, are hindered by the difficulties of... -
Data of the temporary seismic WILAS network
The lithosphere of Iberia has been formed through a number of processes of continental collision and extension. In Lower Paleozoic, the collision of three tectonics blocks...
