For a variety of reasons, Madagascar's rich and highly distinctive faunal assemblage has
long attracted attention. Recurring questions with the associated studies have concerned …

Earth's mantle undergoes convection on million‐year timescales as heat is transferred from
depth to the surface. While this flow has long been linked to the large‐scale horizontal forces …

Continental topography is dominantly controlled by a combination of crustal thickness and
density variations. Nevertheless, it is clear that some additional topographic component is …

Topography and bathymetry are principally supported by some combination of crustal and
sub‐crustal density variations. However, dynamic topography is generated by vertical …

Understanding the primary drivers of lateral and vertical variability in the stratal architecture
of shelf-margin settings is key to understanding how sediments are partitioned from the shelf …

The slow creeping motion of Earth's mantle drives transient changes in surface topography
across a variety of spatial and temporal scales. Recent decades have seen substantial …

Constraints on the erosion history of the southern African Plateau have played a key role in
the debate over the plateau's age and origins. Previous low-temperature thermochronology …

Geometries of eroding landscapes contain important information about geologic, climatic,
biotic and geomorphic processes. They are also characterized by variability, which makes …

There is considerable interest in developing quantitative methods for analyzing present‐day
fluvial landscapes with a view to extracting information about tectonic forcing and drainage …

Ethiopian topography is dominated by an~ 2‐km high plateau that underwent uplift and
incision after or during the Cenozoic Flood Basalt event in the Early Oligocene; however, the …