Introduction [1]: Since their discovery, a variety of formation hypotheses have been proposed to explain the diversity of gully observations. These hypotheses can be divided into three broad categories: entirely dry mechanisms [2,3], wet mechanisms invoking groundwater release [4,5], and wet mechanisms invoking surficial meltwater [6,7,8]. It has been difficult to differentiate between these hy...

Sediment-laden flows with significant amounts of large wood can impact alluvial fans and seriously damage infrastructure property which makes a profound knowledge exposure an essential requisite for risk mitigation. To investigate its spatial variability, we executed experiments on simplified physical model assessed the observed process patterns by quantifying synthetic indexes geostatistically...

Magnetostratigraphic chronologies, together with sedimentological, petrological, seismic and borehole data derived from the Oligo/Miocene Lower Freshwater Molasse Group of the North Alpine foreland basin enable a detailed reconstruction of alluvial architecture in relation to Alpine orogenic events. Six depositional systems are recorded in the Lower Freshwater Molasse Group. The bajada depositi...