Results 51 to 60 of about 405 (165)

Right-Angle Pattern of Minor Fluvial Networks from the Ionian Terraced Belt, Southern Italy: Passive Structural Control or Foreland Bending?

open access: yesGeosciences, 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

Multidisciplinary approach to revisit the state of activity of a deep‐seated gravitational slope deformation in the frame of the Quaternary geomorphological evolution of the Central Apennines (Italy)

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 3, March 2026.
Abstract Evaluating the state of activity of Deep‐Seated Gravitational Slope Deformation (DSGSD) is a challenge that requires multidisciplinary analytical approaches. This research focuses on the slope‐scale gravitational process, framing the role of the Quaternary morphodynamics of a river valley where multiple DSGSDs coexist, to reconstruct the ...
Giorgia Berardo   +5 more
wiley   +1 more source

Analysis of tectonic-controlled fluvial morphology and sedimentary processes of the western Amazon Basin: an approach using satellite images and digital elevation model

open access: yesAnais 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

Tectonics and Surface Processes During Collisional Orogenesis—Exploring the Parameter Space of the Beaumont Number

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 12, December 2025.
Abstract The collision of continents typically leads to orogenesis as a result of crustal thickening and isostatic compensation. High topography is a main locus of precipitation‐fueled erosion, providing a feedback‐loop between tectonics, surface processes, and climate.
S. G. Wolf, R. S. Huismans, J. Braun
wiley   +1 more source

Ongoing Deformation at the Southern Apennine Front: Insights from the Gulf of Taranto (Italy)

open access: yesGeosciences
The Gulf of Taranto (Ionian Sea) is a key transitional sector between the Southern Apennines collisional belt and the Calabrian Arc system, where the expression of Pleistocene–Holocene deformation in the shallow stratigraphic record remains debated. This
Agostino Meo   +3 more
doaj   +1 more source

Inference of a seismic gap from geological data: Thessaly ( Central Greece) as a case study

open access: yesAnnals of Geophysics, 1995
As a result of neotectonic, morphotectonic and seismotectonic research it is now possible to draw detailed maps of the major active faults affecting Thessaly, a large region of continental Greece.
R. Caputo
doaj   +1 more source

Neotectonic-related landforms in the Campos do Jordão Plateau, Southeast Brazil

open access: yesDerbyana, 2022
The Campos do Jordão Plateau, situated in the Serra da Mantiqueira – western flank of the Continental Rift of Southeastern Brazil, presents several morphological features that are indicative of neotectonic activity.
Silvio Takashi Hiruma   +2 more
doaj   +1 more source

A morphotectonic approach to the study of earthquakes in Rome

open access: yesNatural Hazards and Earth System Sciences, 2022
Abstract. Rome has the world's longest historical record of felt earthquakes, with more than 100 events during the last 2600 years. However, no destructive earthquake has been reported in the sources, and all of the greatest damage suffered in the past has been attributed to far-field events.
Fabrizio Marra   +7 more
openaire   +7 more sources

Structural Controls on Splay Fault Rupture Dynamics During Cascadia Megathrust Earthquakes

open access: yesAGU Advances, Volume 6, Issue 6, December 2025.
Abstract Great subduction earthquakes (Mw ≥ 8.0) can generate devastating tsunamis by rapidly displacing the seafloor and overlying water column. These potentially tsunamigenic seafloor offsets result from coseismic fault slip and deformation beneath or within the accretionary wedge. The mechanics of these shallow rupture phenomena and their dependence
J. Biemiller   +8 more
wiley   +1 more source

Reef-rim structure and building history, Rangiroa, an uplifted Atoll, French Polynesia: The role of morphotectonics and extreme marine hazard events

open access: yes, 2022
International audienceReconstructing the responses of low-lying, atoll-rim islands to future environmental changes due to global warming requires a robust knowledge of the building history of reef rims through time.
Innocent, Ch.   +5 more
core   +1 more source

Home - About - Disclaimer - Privacy