Published in Geomorphology
Morphological evidence for ancient channelized flows (fluvial and fluvial-like landforms) exists on the surfaces of all of the inner planets and on some of the satellites of the Solar System. In some cases, the relevant fluid flows are related to a planetary evolution that involves the global cycling of a volatile component (water for Earth and Mar...
Published in Geomorphology
•Land use/design scenarios were evaluated for their effects on soil redistributions.•Scenarios were analysed in terms of soil redistribution using the LandSoil model.•Inappropriate land uses induces higher soil export than landscape design changes.•Land use is a major factor controlling the sediment production.•Landscape design is a major factor co...
Published in Geomorphology
In New Caledonia, numerous cays are distributed on platform reefs in the southwest lagoon behind the barrier reef. At Mba Island, a vegetated sand cay in this area, we examined Holocene sea-level change, and reef development and evolution. The late Holocene sea-level curve for the area was updated using newly found fossil microatolls. Component-spe...
Published in Geomorphology
A response is given to ‘Discussion: “Streamlined erosional residuals and drumlins in central British Columbia, Canada”’. Emphasis is made that the main purpose of the paper under discussion is to present the recognition of a distinctive landscape pattern in central British Columbia that appears to be an immense anastomosing channel network. A chann...
Published in Regional Environmental Change
The lake-rich glacial landscapes of north-eastern central Europe play an important role in the preservation and use of water resources, including protection of biodiversity, carbon storage and promotion of tourism. With a view to the last c. 20 years and the future, a regional ‘syndrome of water shortage’ has been frequently stated, which impairs p...
Published in Geomorphology
•Palaeogeographic reconstruction of the shoreline in Eretria (Euboea, Greece).•Marine environments from ca. 4500 to 3000 cal. BC and from ca. 2000 to 1050 cal. BC.•A lagoonal stage developped from ca. 3000 to 2000 cal. BC.
Published in Geomorphology
A very large deep-seated landslide (DSL) in the northern Pyrenees with over ∼1.4×109m3 was mapped and dated based on sedimentation rates and 10Be terrestrial cosmogenic radionuclide surface exposure (CRE) dating. Our analysis on the landslide reveals the role of inherited structures in the landslide process, and highlighted typical gravitational mo...
Published in Geomorphology
•1071 Pleistocene cirques are studied across a climatic gradient in the Pyrenees.•ANOVA reveals complex links between morphometric attributes, climate and bedrock type.•Cirque size partly reflects solar radiation intensity and prevailing wind direction.•Larger cirques occur on the icefield margins where the glacial footprint was lightest.•Morphomet...
Published in Geomorphology
•Shorelines detected from Landsat images allows to know the storm impact on beaches.•Storm impact and recovery process are analysed along 100 km of the Valencian coast.•Beach response is influenced by beach slope, foredune presence and coast orientation.•Recovery is strongly influenced by longshore transport efficiency
Published in Geomorphology
Within the northern Mississippi embayment the ancestral Mississippi River flowed south through the Western Lowlands and the ancestral Ohio River flowed through the Eastern Lowlands for most of the Pleistocene. Previous investigators have mapped and dated the terraces of their respective braid belts. This current research investigates the three-dime...
