Erosion rates and patterns in a transient landscape, Grand Staircase, southern Utah, USA

Early Younger Dryas glacier culmination in southern Alaska: Implications for North Atlantic climate change during the last deglaciation

The role of permafrost on the morphology of an MIS 3 moraine from the southern Laurentide Ice Sheet

Climate amelioration during the Last Glacial Maximum recorded by a sensitive mountain glacier in New Zealand

Comparison of monitoring data with paleo–slip rates: Cosmogenic nuclide dating detects acceleration of a rockslide

Pliocene–Pleistocene orographic control on denudation in northwest Argentina

Late Miocene rejuvenation of central Idaho landscape evolution: A case for surface processes driven by plume-lithosphere interaction

Dating growth strata and basin fill by combining 26 Al/ 10 Be burial dating and magnetostratigraphy: Constraining active deformation in the Pamir–Tian Shan convergence zone, NW China

Rates of subcritical cracking and long-term rock erosion

Climatically controlled delivery and retention of meteoric 10 Be in soils

Termination II, Last Glacial Maximum, and Lateglacial chronologies and paleoclimate from Big Cottonwood Canyon, Wasatch Mountains, Utah

Ongoing bedrock incision of the Fortymile River driven by Pliocene–Pleistocene Yukon River capture, eastern Alaska, USA, and Yukon, Canada

Trough geometry was a greater influence than climate-ocean forcing in regulating retreat of the marine-based Irish-Sea Ice Stream

Millennial-scale denudation rates of the Santa Lucia Mountains, California: Implications for landscape evolution in steep, high-relief, coastal mountain ranges

Record of coupled hillslope and channel response to Pleistocene erosion and deposition in a sandstone headwater valley, central Pennsylvania

How fast can low-angle normal faults slip? Insights from cosmogenic exposure dating of the active Mai’iu fault, Papua New Guinea

Soil production and transport on postorogenic desert hillslopes quantified with 10 Be and 26 Al

Persistent millennial-scale glacier fluctuations in Ireland between 24 ka and 10 ka