Gösta Hoffmann

ORCID: 0000-0002-2605-2672
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About
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Research Areas
  • Geology and Paleoclimatology Research
  • earthquake and tectonic studies
  • Marine and environmental studies
  • Geological formations and processes
  • Methane Hydrates and Related Phenomena
  • Maritime and Coastal Archaeology
  • Coastal and Marine Dynamics
  • Geological and Geophysical Studies
  • Earthquake Detection and Analysis
  • Tropical and Extratropical Cyclones Research
  • Geotourism and Geoheritage Conservation
  • Flood Risk Assessment and Management
  • Seismology and Earthquake Studies
  • Paleontology and Stratigraphy of Fossils
  • Geological and Geophysical Studies Worldwide
  • Geophysics and Gravity Measurements
  • Coastal wetland ecosystem dynamics
  • Landslides and related hazards
  • Ecology, Conservation, and Geographical Studies
  • Geography Education and Pedagogy
  • Coastal and Marine Management
  • Geological Formations and Processes Exploration
  • Disaster Response and Management
  • Aeolian processes and effects
  • Geological Studies and Exploration

University of Bonn
2018-2023

RWTH Aachen University
2008-2022

Faculty of 1000 (United States)
2021

Institute of Geosciences
2019

German University of Technology
2009-2018

Leibniz Institute for Baltic Sea Research
2010

Universität Greifswald
2004-2010

Utrecht University
2007

Link (Germany)
1894

Today's understanding of sea-level change developed through a combination process-based physical modelling and observational data. Observational data derives from coral reefs in the far-field former ice sheets where geographically variable relative signal is expected as response earth to ocean loading. Given this variability limited geographical distribution reefs, there need explore other, non-coral based markers further understand and, for example, 'fingerprint' melt-water. Here, we...

10.1016/j.margeo.2015.01.009 article EN cc-by-nc-nd Marine Geology 2015-01-28

Abstract The aim of this paper is to reconstruct the evolution early middle Holocene Rhine-Meuse river mouths in western Netherlands and understand observed spatial temporal changes facies. This achieved by constructing three delta wide cross-sections using a newly accumulated database with thousands core descriptions cone penetration test results, together large set pollen/diatom analyses OSL/ 14 C-dates. Most studied deposits fluvial-to-marine transition zone, highly complex area due...

10.1017/s0016774600000986 article EN Netherlands Journal of Geosciences – Geologie en Mijnbouw 2009-03-01

Research Article| October 01, 2014 An Indian Ocean tsunami triggered remotely by an onshore earthquake in Balochistan, Pakistan Gösta Hoffmann; Hoffmann * 1Department of Applied Geosciences, German University Technology, PO Box 1816, PC 130 Muscat, Sultanate Oman2Institute Neotectonics and Natural Hazards, RWTH Aachen University, Lochnerstrasse 4-20, 52056 Aachen, Germany *E-mails: goesta.hoffmann@gutech.edu.om; s.alyahyai@met.gov.om; ghazala_ghq@hotmail.com. Search for other works this...

10.1130/g35756.1 article EN Geology 2014-08-16

The Arabian Peninsula is surrounded by seismically highly active plate margins, while the interior seems to be free from destructive earthquakes. We report two historical earthquakes in Qalhat, Oman, >300 km any boundary and provide archaeoseismological analysis of ruined buildings. first quake hit city 1497 AD with an intensity VII at most; community survived damage was repaired. second event caused total devastation (intensity X-XI), sometime between 1580 1592. never recovered latter; it...

10.1016/j.quaint.2023.05.016 article EN cc-by Quaternary International 2023-05-26

10.1127/1860-1804/2013/0002 article EN Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 2013-02-05

Abstract. Isostatic response of the Earth's crust as a consequence fluctuating extent ice-sheet masses was accompanied by earthquakes probably due to local reactivation pre-existing faults. Our study glacilacustrine and glacifluvial succession exposed on Rügen Island (SW Baltic Sea) indicates that some soft-sediment deformation structures within must have formed shortly before front Pleistocene Scandinavian Ice Sheet reached area (during Last Glacial Maximum), thus during stage ice advance....

10.5194/deuquasp-2-61-2019 article EN DEUQUA Special Publications 2019-08-15

Abstract Sedimentological, geochemical, and paleontological investigations of the coastline northeastern Oman have provided authors with an in-depth insight into Holocene sea levels climate conditions. The spatial distribution species assemblage mangrove ecosystems are analyzed. These sensitive to changes in level precipitation thus reflect ecological close proximity archaeological sites allows us draw conclusions regarding human interaction ecosystems. Our interdisciplinary inquiry reveals...

10.1017/qua.2020.96 article EN Quaternary Research 2020-12-29
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