The cosmogenic nuclide exposure history method is undergoing major developments in
analytical, theoretical, and applied areas. The capability to routinely measure low …

Research in landscape evolution over millions to tens of millions of years slowed
considerably in the mid‐20th century, when Davisian and other approaches to …

Low temperature thermochronologic techniques (eg apatite fission track (AFT)
thermochronology and (U–Th)/He dating) constrain near-surface T–t paths and are often …

The Antarctic Dry Valleys (ADV) are generally classified as a hyper-arid, cold-polar desert.
The region has long been considered an important terrestrial analog for Mars because of its …

Sandstones form the backdrop to some of the world's most spectacular scenery, and are
found all over the planet and in all climates. Following on from the authors' successful 1992 …

In the last decades surface exposure dating using cosmogenic nuclides has emerged as a
powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic …

The production of noble gas isotopes by interactions of high-energy cosmic ray particles with
rocks was first recognized half a century ago when Paneth et al.(1952) showed that the high …

A thin glacial diamicton, informally termed Granite drift, occupies the floor of central Beacon
Valley in southern Victoria Land, Antarctica. This drift is< 1.0 m thick and rests with sharp …

Landscape evolution of the Antarctic continent since the breakup of Gondwana has been
controlled in the first order by changes in the location and configuration of plates. Following …

Blood Falls is the surface manifestation of brine released from below the Taylor Glacier,
McMurdo Dry Valleys, Antarctica. Geochemical analyses of Blood Falls show that this brine …