Geersen, Jacob (2019): Collated bathymetric data from convergent margins that experienced tsunami earthquakes. PANGAEA, https://doi.org/10.1594/PANGAEA.899049, Supplement to: Geersen, J (2019): Sediment-starved trenches and rough subducting plates are conducive to tsunami earthquakes. Tectonophysics, 762, 28-44, https://doi.org/10.1016/j.tecto.2019.04.024
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For each tsunami earthquake region, ship-based bathymetric data have been collated from German (http://www.bsh.de), French (http://en.data.ifremer.fr), Japanese (http://www.godac.jamstec.go.jp/darwin/e) and US (http://www.rvdata.us) research cruises as well as the compilation of data provided by the Global Multi-Resolution Topography (GMRT) synthesis (https://www.gmrt.org). The ship-based bathymetric soundings were quality checked and manually edited if necessary. The collated data is displayed on top of the SRTM15+ grid (https://www2.jpl.nasa.gov/srtm). For the New Zealand margin the collated data is displayed on top of the nationwide bathymetric compilation provided by The National Institute of Water and Atmospheric Research (NIWA) (https://www.niwa.co.nz/our-science/oceans/bathymetry).
Median Latitude: 6.714286 * Median Longitude: -177.142857 * South-bound Latitude: -38.000000 * West-bound Longitude: 98.000000 * North-bound Latitude: 53.000000 * East-bound Longitude: -81.000000
Bathymetry_Aleutians * Latitude: 53.000000 * Longitude: -163.000000 * Method/Device: Swath bathymetry mapping (SBM)
Bathymetry_Japan * Latitude: 40.000000 * Longitude: 144.000000 * Method/Device: Swath bathymetry mapping (SBM)
|#||Name||Short Name||Unit||Principal Investigator||Method/Device||Comment|
|1||Event label||Event||Geersen, Jacob|
|2||File content||Content||Geersen, Jacob|
|3||Reference of data||Ref data||Geersen, Jacob|
|4||File name||File name||Geersen, Jacob|
|5||File format||File format||Geersen, Jacob|
|6||File size||File size||kByte||Geersen, Jacob|
|7||Uniform resource locator/link to file||URL file||Geersen, Jacob|
84 data points