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Le développement actuel de la partie étudiée de la vallée Imeretinsky est caractérisé par le recul rapide du trait de côte et l’encaissement de la baie en face de la gorge Novyj. En même temps, l’échancrure de la Cape de Konstantinovskij est
tronquée de 4 mètres par an et les produits de l’érosion sont transportés principalement dans les gorges adjacentes. La réfraction des vagues joue un rôle important dans les processus lithodynamiques. Elle entraîne une concentration de l’énergie et provoque
l’augmentation du volume de flux sédimentaire le long des bords Est des gorges Novyj et Konstantinovskij. Le risque que représente aujourd’hui la côte de la zone étudiée, nécessite la prise urgente de mesures de lutte contre l’érosion par l'apport de galets.
2013

Reducing nitrogen and phosphorus losses from arable slope land with contour hedgerows and perennial alfalfa mulching in Three Gorges Area, China
The loss of nitrogen and phosphorus from arable slope land threatens the aquatic environment in the Three Gorges Area, China, and the protection of these slopes will play an important role in regional agricultural development. During the last 10
2013

of flow regulation and climate change. They can also be used to set flushing flows in bedrock channels. In sandstone gorges of the Nepean River, Australia, the crustose lichen,Lecidea terrena Nyl, was common at both gorge and cemetery (sandstone headstones
2013

The AA. use luminescence signals from debris flow and fluvial deposits as well as OSL dating of 3 deposits to detect the main paraglacial processes in Gredos Gorge, a glaciated valley of Sierra de Gredos (Central Spain). They identify 2 major phases
the deglaciation of Gredos Gorge, paraglacial sediment was depleted as theory predicts. The AA. propose that the poor coverage of vegetation driven by the Mediterranean climate prevents the stabilization of glacigenic sediment that is only mobilized during high
2013

. In present days the Csernely Creek cuts into the higher relief Palaeozoic rock and crosses it through a narrow gorge. There is one explanation for this. The Palaeozoic rocks must have been covered with the Lower Miocene rocks. On the top
2013

in the fault zone are manifest in form of palaeo-landslide cones, unpaired terraces, fault facets, soaring waterfalls, deep gorges and slope failures etc. The soft sedimentary structures, e.g., micro-faulting and flame structures in the exposed profile also
2013

Using aerial photographs, field surveys, and hydrological data, the AA. constrain the incision history of a bedrock gorge 1200 m long and up to 20 m deep cut by Da'an River in western Taiwan. This reach of the river experienced 10 m of uplift during
2013

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