Slip distribution, slip rate, and slip per event for strike‐slip faults are commonly determined
by correlating offset stream channels—under the assumption that they record seismic slip …

In areas where regional tectonic strain is accommodated by broad zones of short and low
slip rate faults, geomorphic and paleoseismic characterization of faults is difficult because of …

Intraplate settings far from tectonic plate boundaries are normally thought to be tectonically
inactive regions in which the landscape evolves via the slow downcutting of fluvial systems …

We propose a novel way to measure and analyze networks of drainage divides from digital
elevation models. We developed an algorithm that extracts drainage divides based on the …

Here we examine the landscape of New Zealand's Marlborough Fault System (MFS), where
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …

This chapter reviews quantitative modeling of landscape evolution–which means that not
just model studies but also modeling concepts are discussed. Quantitative modeling is …

Drainage divides can become unstable due to tectonic disturbances and therefore can be
used to constrain past tectonic activity. However, many studies have focused mainly on the …

Drainage divides are organized into tree-like networks that may record information about
drainage divide mobility. However, views diverge about how to best assess divide mobility …

River aggradation or incision at different spatial-temporal scales are governed by tectonics,
climate change, and surface processes which all adjust the ratio of sediment load to …

Quantifying off-fault deformation (OFD) rates on geomorphic time scales (102–105 yr) along
strike-slip faults is critical for resolving discrepancies between geologic and geodetic slip …