Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

Rivers are important agents of change that shape the Earth's surface and evolve through
time in response to fluctuations in climate and other environmental conditions. They are …

Changes in the steepness of river profiles or abrupt vertical steps (ie waterfalls) are thought
to be indicative of changes in erosion rates, lithology or other factors that affect landscape …

Sediment supply (Qs) is often overlooked in modelling studies of landscape evolution,
despite sediment playing a key role in the physical processes that drive erosion and …

Topographic metrics are designed to quantify scale‐relevant relationships between
geometric properties of landscapes to reveal the processes shaping them. They have long …

Deforestation is associated with a decrease in slope stability through the alteration of
hydrological and geotechnical conditions. As such, deforestation increases landslide activity …

Waterfalls are inspiring landforms that set the pace of landscape evolution as a result of
bedrock incision,–. They communicate changes in sea level or tectonic uplift throughout …

Single‐grain post‐infrared infrared stimulated luminescence (SG‐pIRIR) of feldspar has
recently been introduced as a method to date Quaternary deposits. The method is …

Waterfalls are among the fastest-eroding parts of river networks, but predicting natural
waterfall retreat rates is difficult due to multiple processes that can drive waterfall erosion …