Renland ...

The experiments are performed down the Edward Bailey valley, in the Renland peninsula, Scoresby Sund, Greenland. General purpose: ambient seismic noise recordings are obtained to characterize the geometry/structure of the valley the geometry/structure of the glaciers the microseismicity of the glaci...

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Bibliographic Details
Main Author: Larose, Eric
Format: Dataset
Language:English
Published: GFZ Data Services 2016
Subjects:
Monitoring system
In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers
In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS
Geophysics
FOS: Earth and related environmental sciences
Passive seismic
Seismometers
Velocity
MiniSEED
GIPP
MESI
Temporary[g]
Greenland
Renland
Scoresby
Scoresby Sund
Sund
glacier
Online Access:https://dx.doi.org/10.14470/8u7561563769
http://geofon.gfz-potsdam.de/doi/network/3H/2016
Description
Summary:The experiments are performed down the Edward Bailey valley, in the Renland peninsula, Scoresby Sund, Greenland. General purpose: ambient seismic noise recordings are obtained to characterize the geometry/structure of the valley the geometry/structure of the glaciers the microseismicity of the glacier, the friction process, crack orientation and mechanisms the seismic activity of glacial rivers, the relation between hydrological flow and noise spectrum the localization and characterization of sub-glacial flow from surface recordings. Seismic stations were composed of 3C broadband Trillium compact seismometer, a Cube datalogger and a 12V (D-cell types, stacked) battery pack.The experiment splits into three surveys performed at three different sites, one after the other, from july to august 2016. In the first experiment, we deploy 11 stations, 9 of them on a flat sandy area covering, partly, immobile ice that seems to be blocked between the Bailey Glacier (upstream) and the Apusinikajik glacier (downstream). ...

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