Understanding the manner and degree to which topography in active mountain ranges
reflects deformation of the Earth's surface remains a first order goal of tectonic …

The Sierra Nevada of the central Betic Cordillera is a 3000m-high mountain range
surrounded by Neogene–Quaternary sedimentary basins, having been uplifted since Late …

The present review paper is an attempt to summarize quantitative evidence of Late
Cenozoic changes in topographic relief. Different meanings of the word “relief”, as it is …

The persistence of topography within ancient orogens remains one of the outstanding
questions in landscape evolution. In the eastern North American Appalachians, this question …

The rate at which transient knickpoints propagate through a landscape fundamentally
controls the rate of geomorphic response to tectonic and climatic perturbation. Here we …

There appears to be no single axis of causality between life and its landscape, but rather,
each exerts a simultaneous influence on the other over a wide range of temporal and spatial …

What controls the chemical weathering of soils in tectonically active landscapes? Recent
field and modeling studies suggest that tectonic forcing and associated increases in erosion …

Hypsometry is thought to be sensitive to tectonic uplift rates and lithology differences. In this
study we calculated hypsometric integrals (HIs) using as topographic sources two digital …

Past variations in climate and tectonics have led to spatially and temporally varying erosion
rates across many landscapes. In this contribution I examine methods for detecting and …

Drainage density is a fundamental landscape metric describing the extent of the fluvial
network. We compare the relationship between drainage density (Dd) and erosion rate (E) …