Results 51 to 60 of about 3,134 (203)
Range‐Parallel Extension of the Andes in the 2020 Mw 5.7 Humahuaca Earthquake
Journal of Geophysical Research: Solid Earth, Volume 130, Issue 12, December 2025.Abstract Normal‐faulting earthquakes in mountain ranges provide important constraints on the dynamics of mountain building. To date, well‐documented examples of range‐parallel extension come primarily from the Tibetan Plateau, limiting our ability to test different models for its cause.
Simon Orrego +3 more
wiley +1 more source
Journal of Maps, 2020 This work presents a tectonic geomorphology analysis of a river bend in the middle Tavo River valley, in the piedmont area of the NE Apennines (Abruzzo Region), between the eastern slope of the chain (Gran Sasso Massif) and the Adriatic coast.
Cristiano Carabella +5 more
doaj +1 more source
Frontiers in Earth Science, 2021 The aim of this work is to make a synthesis at regional scale focused on the geophysical characterization of submarine faults around the Iberian margin to identify active structures and analyze their development in the framework of the present plate ...
Luis Somoza +4 more
doaj +1 more source
Applied Water Science, 2017 Morphological and morphotectonic analyses have been used to obtain information that influence hydrographic basins, predominantly these are modifications of tectonic elements and the quantitative description of landforms.
K. Prakash +4 more
semanticscholar +1 more source
Is the Suez Rift in Its Post‐Rift Phase?
Geophysical Research Letters, Volume 52, Issue 21, 16 November 2025.Abstract Failed rifts are widely assumed to enter post‐rift tectonic quiescence after termination of intracontinental rifting, but a comprehensive understanding of their regional morphotectonics is lacking. Our quantitative, rift‐scale geomorphic analyses in the Suez Rift, an archetypal failed rift in Egypt, reveals widespread rifting after presumed ...
David Fernández‐Blanco +2 more
wiley +1 more source
Scale-dependence of lithological control on topography: Bedrock channel geometry and catchment morphometry in western Scotland [PDF]
, 2010 We propose that a scale-dependent topographic signature of erodibility arises due to fluvial and glacial erosion acting on different parts of the landscape at different times.
Bishop, P. +3 more
core +3 more sources
Tectonics, Volume 44, Issue 10, October 2025.Abstract In a subduction zone, variability in the buoyancy and structure of the downgoing plate impacts deformation patterns in the overriding plate. Thick and buoyant lithosphere or smaller‐scale indentors entering the trench can lead to significant relief development and exhumation. To investigate such processes, we target the Cenozoic reorganization
E. M. Conrad, C. Faccenna, D. F. Stockli
wiley +1 more source
Geosciences, 2018 Morphometric analyses of both the topography and drainage network have been carried out in a large sector of the Ionian coastal belt of southern Italy in order to unravel the possible control of Late Quaternary thrust front activity on the evolution of ...
Dario Gioia +2 more
doaj +1 more source
Controls on Water‐Magma Interactions at Hydraulically‐Charged Volcanic Islands
Geophysical Research Letters, Volume 52, Issue 18, 28 September 2025.Abstract The interaction of rising magma with groundwater can produce phreatomagmatic explosions, which, given their enhanced explosivity and unpredictability, increase the hazard potential of volcanic eruptions. To investigate the link between groundwater occurrence and phreatomagmatism, we compare the volcanic record of Flores Island (Azores) with ...
M. Andrade +7 more
wiley +1 more source
Anais da Academia Brasileira de Ciências, 2007 An investigation of the tectonic controls of the fluvial morphology and sedimentary processes of an area located southwest of Manaus in the Amazon Basin was conducted using orbital remote sensing data.
Clauzionor L. Silva +4 more
doaj +1 more source