This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

Uncertainties about landscape evolution under cold, nonglacial conditions raise a question
fundamental to periglacial geomorphology: what and where are periglacial landscapes? To …

Using in situ field measurements, laboratory analyses, and numerical modeling, we test the
potential efficacy of thermal stress weathering in the flaking of millimeter‐thick alteration …

Cirques are emblematic landforms of alpine landscapes. The statistical distribution of cirque-
floor elevations is used to infer glacial equilibrium-line altitude, and the age of their frontal …

Pegmatites and aplites share the common major constituents with the granitoid suite as well
as various gneissic lithologies, eg, orthogneisses, aplitic gneisses. Not surprising, the …

Periglacial environments are characterized by cold-climate non-glacial conditions and
ground freezing. The coldest periglacial environments in Pleistocene Britain were underlain …

This note suggests that decimal latitude/longitude [dLL] locations should be used to identify
features of interest, landforms, sample and investigations sites, in an 'information …

Landscapes and soils evolve in non‐linear ways over millennia. Current knowledge is
incomplete as only average denudation (or erosion) rates are normally estimated …

Recent research has established Schmidt Hammer exposure dating (SHED) as an effective
method for dating glacial landforms in the UK. This paper presents new data and discussion …

Bedrock outcrops punctuating regolith-covered surfaces in the summit/upper slope and
hillside positions (tors and crags) have long been a subject of inquiry in geomorphology for …