[HTML][HTML] How do landscapes record tectonics and climate?
AC Whittaker - Lithosphere, 2012 - pubs.geoscienceworld.org
The Earth's surface is shaped by tectonics and climate. This simple statement implies that
we should, in principle, be able to use the landscape as an archive of both tectonic rates and …
we should, in principle, be able to use the landscape as an archive of both tectonic rates and …
Landslide erosion controlled by hillslope material
IJ Larsen, DR Montgomery, O Korup - Nature Geoscience, 2010 - nature.com
Steep hillslopes in mountain belts are eroded by landslides, and landsliding is ultimately
driven by the topographic relief produced by fluvial and glacial erosion,,,,. Landslide erosion …
driven by the topographic relief produced by fluvial and glacial erosion,,,,. Landslide erosion …
[HTML][HTML] Coupled surface to deep Earth processes: Perspectives from TOPO-EUROPE with an emphasis on climate-and energy-related societal challenges
Understanding the interactions between surface and deep Earth processes is important for
research in many diverse scientific areas including climate, environment, energy …
research in many diverse scientific areas including climate, environment, energy …
New Constraints on the Late Oligocene‐Miocene Thermo‐Tectonic Evolution of the Southeastern Tibetan Plateau From Low‐Temperature Thermochronology
Abstract The southeastern (SE) Tibetan Plateau (Yunnan) is characterized by low‐relief
uplands that were deeply incised by large rivers. The thermal history of basement rocks in …
uplands that were deeply incised by large rivers. The thermal history of basement rocks in …
Driving the upper plate surface deformation by slab rollback and mantle flow
The relative contribution of crustal and mantle processes to surface deformation at
convergent plate margins is still controversial. Conflicting models involving either extrusion …
convergent plate margins is still controversial. Conflicting models involving either extrusion …
The trajectory of geomorphology
M Church - Progress in Physical Geography, 2010 - journals.sagepub.com
Modern geomorphology was founded in the nineteenth century as an exercise of historical
interpretation of landscapes. After the mid-twentieth century it dominantly became a quest to …
interpretation of landscapes. After the mid-twentieth century it dominantly became a quest to …
Morphotectonic and lithostratigraphic analysis of intermontane Karewa basin of Kashmir Himalayas, India
Morpho-tectonic study plays an important role in deciphering the effects of tectonic activity in
the geomorphic evolution of the drainage basins. Romushi watershed forms one of the …
the geomorphic evolution of the drainage basins. Romushi watershed forms one of the …
[HTML][HTML] Cenozoic low temperature cooling history of the eastern Lhasa terrane: Implications for high-relief topography of external drainage area in the southern …
Abstract The Tibetan Plateau geographically contains internal and external drainage areas
based on the distributions of river flows and catchments. The internal and external drainage …
based on the distributions of river flows and catchments. The internal and external drainage …
Badland landscape response to individual geomorphic events
Landscapes form by the erosion and deposition of sediment, driven by tectonic and climatic
forcing. The principal geomorphic processes of badland–landsliding, debris flow and runoff …
forcing. The principal geomorphic processes of badland–landsliding, debris flow and runoff …
Late Oligocene-Miocene morpho-tectonic evolution of the central Gangdese batholith constrained by low-temperature thermochronology
The morpho-tectonic evolution of the Tibetan Plateau is controlled by complicated
interactions between tectonic uplift and surface erosion. The Gangdese batholith in the …
interactions between tectonic uplift and surface erosion. The Gangdese batholith in the …