Abstract The Mississippi River fluvial–marine sediment-dispersal system (MRS) has become
the focus of renewed research during the past decade, driven by the recognition that the …

Just as glaciers worldwide left a record of past advances and retreats that shifted latitudinally
in response to oscillating Quaternary climate changes, so too have cold-climate conditions …

Mantle seismic structure beneath the United States spanning from the active western plate
margin to the passive eastern margin was imaged with teleseismic P and S wave traveltime …

Efforts to extract information about climate and tectonics from topography commonly assume
that river networks are static. Drainage divides can migrate through time, however, and …

Determining factors that modify Earth's topography is essential for understanding continental
mass and nutrient fluxes, and the evolution and diversity of species. Contrary to the …

Topography is a reflection of the tectonic and geodynamic processes that act to uplift the
Earth's surface and the erosional processes that work to return it to base level. Numerous …

Establishing landscape response to uplift is critical for interpreting sediment fluxes, hazard
potential, and topographic evolution. We assess how landslides shape terrain in response to …

The lithospheric structure of the Southeastern United States is a product of earlier episodes
of continental collision and breakup. The region is located in the interior of the North …

Topographic relief results from the complex interactions between tectonics and erosional
surface processes, which are primarily mediated by bedrock erodibility and climatic …

Regolith‐mantled hillslopes are ubiquitous features of most temperate landscapes, and their
morphology reflects the climatically, biologically, and tectonically mediated interplay …