Alluvial and fluvial fans are the most widespread depositional landforms bordering the
margins of long-lived highland regions and actively subsiding continental basins, across a …

Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively
studied in many of these regions, but there are few studies on fans in periglacial, Arctic and …

Recent investigations have shown that the extent of the channel network in some drainage
basins is controlled by a threshold for overland flow erosion. The sensitivity of such basins to …

Tectonics, climate and base level are the underlying controls of alluvial fan development. On
many fans base level is stable, but where base-level change occurs it may itself be a …

Conventionally, a fall in base level is seen as stimulating incision into the distal zones of
alluvial fans. In the Cabo de Gata ranges of southeast Spain evidence exists to the contrary …

Alluvial fan deposits along the Providence Mountains piedmont in the eastern Mojave
Desert that (1) are derived from diverse rock types,(2) are dated with luminescence …

Alluvial fan development in Alpine areas is often affected by catastrophic sedimentary
processes associated with extreme floods events, causing serious risks for people living on …

Geomorphologie ist die Wissenschaft von den Oberflächenformen der Erde. Die Entstehung
und Weiterbildung des Reliefs unseres Planeten ist Ausdruck geologischer Prozesse, der …

Stable carbon and oxygen isotopes in soil carbonates provide an additional technique for
investigating Quaternary ecogeomorphic changes in arid and semiarid regions. This study …

Quaternary alluvial fans in the tectonically active Pinjaur Dun, an intramontane valley in the
Sub‐Himalaya, were deposited in front of the Nalagarh Thrust and were influenced both by …