In this paper, we review ideas on the geomorphological history of the southwest African
passive margin, focusing on the central Namib sector and presenting new evidence on the …

This study explores the long‐duration (0.8–2.3 Ma), time‐averaged micrometeorite flux
(mass and size distribution) reaching Earth, as recorded by the Transantarctic Mountains …

The time‐dependent physics of ice sublimation through thin layers of till is considered, to
determine whether sublimation could be sufficiently slow to permit the preservation of ice for …

Microtektites represent high-velocity/distal meteorite impact ejecta. Demonstrating that
microtektites found at several locations throughout East-Antarctica consist of a …

Petrographic and geochemical studies of microtektites collected in newly explored summit
plateaus of the Transantarctic Mountains (ie, Schroeder Spur, Killer Nunatak, Miller Butte in …

Separate regions within the Transantarctic Mountains, the uplifted flank of the West Antarctic
rift system, appear to have distinct Neogene histories of glaciation and valley downcutting …

In this study, we investigate the thermo-mechanical controls on the formation of the Ross
Sea basin (Antarctica) and the uplift of the adjacent Transantarctic Mountains (TAM) rift …

Each year, approximately 5000 tons of extraterrestrial material reaches the Earth's surface
as micrometeorites, cosmic dust particles ranging from 10 to 2000 μm in size. These …

Aeromagnetic signatures over the Edward VII Peninsula (E7) provide new insight into the
largely ice-covered and unexplored eastern flank of the Ross Sea Rift (RSR). Positive …

In 2001, a small H4 chondrite, Frontier Mountain (FRO) 01149, was found on a glacially
eroded surface near the top of Frontier Mountain, Antarctica, about 600 m above the present …