The stream power law, expressed as E= KA m S n—where E is erosion rate [LT− 1], K is an
erodibility coefficient [T− 1 L (1− 2m)], A is drainage area [L 2], S is channel gradient [L/L] …

First, I benchmark existing methods of calculating subsurface 26 Al, 10 Be, and 14 C
production rates due to cosmic-ray muons against published calibration data from bedrock …

As cosmogenic nuclide applications continue to expand, the need for a common basis for
calculation becomes increasingly important. In order to accurately compare between results …

Over the last decades, cosmogenic exposure dating has permitted major advances in many
fields of Earth surface sciences and particularly in paleoglaciology. Yet, exposure age …

Landscape denudation in actively deforming mountain ranges is controlled by a
combination of rock uplift and surface runoff induced by precipitation. Whereas the relative …

The first arrivals of hominin populations into Eurasia during the Early Pleistocene are
currently considered to have occurred as short and poorly dated biological dispersions …

Geological surface-exposure dating using cosmogenic-nuclide accumulation became a
practical geochronological endeavor in 1986, when the utility of 10 Be, 26 Al, 36 Cl, and 3 …

Chlorine-36 production rates obtained from different geological calibration studies (eg
Evans et al., 1997; Phillips et al., 2001; Schimmelpfennig et al., 2011; Stone et al., 1996; …

Since its discovery within a travertine quarry, the fragmentary cranium of the only known
Turkish Homo erectus, the Kocabaş hominid, has led to conflicting biochronological …

Surface exposure dating using cosmic-ray-produced nuclides has been applied to
determine the age of thousands of landforms produced by alpine glaciers in mountain areas …