Results 41 to 50 of about 8,222 (215)
Remote SensingComplete records of fault activity are very valuable for assessing possible earthquakes. Fault scarps are one key to exploring past fault activity. Through the records of fault scarps, we can obtain evidence of fault activity and faulting events in ...
Xianghe Ji, Klaus Reicherter
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The role of neo-tectonics in the sedimentary infilling and geomorphological evolution of the Guadalquivir estuary (Gulf of Cadiz, SW Spain) during the Holocene. [PDF]
, 2016 Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution of the Guadalquivir estuary during the Holocene. The sedimentation and geomorphological disposition have been strongly conditioned by neotectonic activity ...
Celestino Pérez, Sebastián, 1957- +9 more
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Tectonics, Volume 45, Issue 4, April 2026.Abstract Young active faults pose an underestimated seismic hazard as they can have limited geomorphic and structural expression. The Aigion‐Erineos fault system (AEFS) is a young normal fault on the south coast of the Gulf of Corinth, Greece that provides a key structural link with the Gulf of Patras.
Alexander C. Whittaker +2 more
wiley +1 more source
Investigation on Reflection of Tectonic Pattern in ASG EUPOS Data in the Sudetes and Adjacent Areas
Reports on Geodesy and Geoinformatics, 2016 The GNSS data evaluated from on observation of ASG EUPOS stations in the Sudety Mts. and in adjacent areas is analyzed by the author in the scope of disturbances in daily solutions that can be induced by tectonics stress.
Szczerbowski Zbigniew
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Unravelling the evolution of the Frébouge polygenetic cone in Val Ferret (Mont Blanc Massif)
Boreas, Volume 55, Issue 2, Page 454-475, April 2026.Proglacial settings in the Alps are typically polygenetic, often characterized by a complex and discontinuous interplay between glacial, fluvial and gravitational processes. These processes yield high volumes of sediments, which usually exceed their transportation capacity.
Catharina Dieleman +6 more
wiley +1 more source
Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield [PDF]
Bulletin of the Geological Society of Finland, 2018 As a result of melting of the last ice sheet in the southeastern edge of the Fennoscandian shield, ridge structures called eskers were formed. One of these eskers is the subject of our study.
A. Poleshchuk, D. Zykov, S. Shvarev
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Boreas, Volume 55, Issue 2, Page 585-599, April 2026.Bioerosional scars made by limpets (Patella) on a cliff in Co. Antrim, Northern Ireland, indicate a Mid‐Holocene RSL of +7.8±0.55 m relative to local mid‐tide level today. This is higher than previous empirical data for the region and extrapolated levels from raised shorelines in Scotland but consistent with some recent GIA models.
Michael J. Simms, Paula J. Reimer
wiley +1 more source
Environmental Sciences EuropeBackground In July 2021, destructive floods in Western Europe were triggered by enormous precipitation rates related to a low-pressure system named "Bernd." These catastrophic events led not only to major damage to infrastructure, severe economic losses,
Vanessa Steinritz +5 more
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GeoHazardsThe Longshou Shan area is located on the northeastern margin of the Tibetan Plateau in northwest China. The study area is located where the sinistral Altyn Tagh and Haiyuan Faults overlap and the Qilian Shan thrust fault systems in the northeastern ...
Xianghe Ji, Klaus Reicherter
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Acta Universitatis Carolinae Geographica, 2019 The morphometric analysis of lineaments, valleys and signs of erosion taken from a digital elevation model (DEM) made it possible to not only confirm most of the conclusions of the morphotectonic development of the Blue Nile Basin from the previously ...
Michal Kusák +2 more
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