Much of the final shaping of the global landscape is accomplished by incision of river
networks. The base-level is a principle determinate controlling the global relief by processes …

Abstract The Dead Sea area, located within the African Rift Valley, occupies the deepest
depression on earth. Its hydrological regime is typified by long dry intervals, high-intensity …

The following key factors control the impact of the base-level: 1. The contributing drainage
area which is the proxy for sediment and water discharge that controls and regulates the …

First-generation sequence stratigraphic models have dealt in a very rudimentary fashion
with the response of fluvial systems to eustasy. A major element of presently accepted …

Marine terraces are ephemeral planar landforms. While tectonic and climatic forcings
responsible for the generation of existing marine terraces have operated for at least 1 Myr …

While propagating upstream, knickpoints do not retain their form. Form evolution during
headward knickpoint migration may include diffusion, parallel retreat, rotation or …

Channel incision is part of denudation, drainage-network development, and landscape
evolution. Rejuvenation of fluvial networks by channel incision often leads to further network …

Channel incision is part of denudation, drainage-network development, and landscape
evolution. Rejuvenation of fluvial networks by channel incision generally leads to further …

The episodic transfer of sediment from source to sink is a fundamental process in fluvial
systems that influences river morphology, aquatic and riparian ecosystems, and risk from a …

We present new field data from rivers draining across active normal faults that incise across
the same lithology at the fault, have been subjected to similar climatic regimes and tectonic …