Rock control, the influence of rock properties on landform development, has for long been a
relatively under-researched topic, but numerous techniques have been developed …

Rapid, field‐based measurements of rock hardness are of use in investigating many
geomorphological and heritage science problems. Several different methods are now …

Variation in the erodibility of rock units has long been recognized as an important
determinant of landscape evolution but has been little studied in landscape evolution …

The mineral ore potential of many mountainous regions of the world, like the Kurdistan
region of Iraq, remains unexplored. For logistical and sometimes political reasons, these …

Headwater streams expand, contract, and disconnect in response to seasonal moisture
conditions or those related to individual precipitation events. The fluctuation of the surface …

Climate regulation of erosion in unglaciated landscapes remains difficult to decipher. While
climate may disrupt process feedbacks that would otherwise steer landscapes toward steady …

Mountainous landscapes often feature alluviated valleys that control both ecosystem
diversity and the distribution of human populations. Alluviated, flat valley floors also play a …

An attempt is made to explain the relationship of landslides to litho-tectonic and precipitation
regimes. The possible influence of these factors on the dimensional pattern of landslides is …

Field and modeling studies suggest that bedrock channels equilibrate to base‐level change
through geometry and slope adjustment to imposed discharge, sediment supply, and …

Bedrock channels are shaped by fluvial erosion, which is often described by the stream
power model. However, recent research indicates that the applicability of the stream power …