In mountainous settings, increases in rock uplift are often followed by a commensurate
uptick in denudation as rivers incise and steepen hillslopes, making them increasingly prone …

This paper describes a general method for determining the amount of earthquake-induced
landsliding that occurs in a seismically active region over time; this determination can be …

Despite the importance of soil erosion in sustainable development goals in arid and semi-
arid areas, the study of the geo-environmental conditions and factors influencing gully …

Soil erosion in the United States has been a matter of public concern since the 1930s.
Conditions were improved by the 1960s, although no one knew just how much (1). Starting …

Stream channel erosion has long been suspected as the major contributor to long-term
sediment yield from urbanizing watersheds. For San Diego Creek in southern California …

The total measured rate of alluvial sediment accretion in the agricultural Coon Creek Basin
for the period 1975–93 was only about 6 percent of the rate that occurred in the 1930s, but …

Gully erosion removes comparatively large volumes of soil from small areas. It is often
difficult to quantify the loss of soil because the footprint of individual gullies is too small to be …

In June 1982, a storm with a return period greater than 100 yr, but lasting less than 2.5 hr,
destabilized hillslopes and produced a suite of geomorphologically and sedimentologically …

Precipitation drives seasonal velocity changes in slow-moving landslides by increasing pore-
water pressure and reducing the effective normal stress along basal shear zones. This …

The cycle of organic carbon burial and exhumation moderates atmospheric chemistry and
global climate over geologic timescales. The burial of organic carbon occurs predominantly …