The Periglacial Environment, Fourth Edition, is an authoritative overview of the world's cold,
non-glacial environments. First published in 1976 and subsequently revised in 1996 and …

One of the distinguished efforts of AL Washburn was to reconstruct mean annual air
temperature using periglacial features as climate indicators. This paper reviews existing …

Results are presented from eight scaled centrifuge modelling experiments designed to
investigate mass movement processes on thawing ice-rich slopes. Four pairs of simple …

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

During Lateglacial cold periods, permafrost developed throughout Scotland, sediment-
mantled slopes were extensively modified by solifluction and other forms of periglacial mass …

Vegetation is an important factor influencing solifluction processes, while at the same time,
solifluction processes and landforms influence species composition, fine‐scale distribution …

Solifluction is one of the most widespread periglacial processes with low annual movement
rates in the range of—millimeters to centimeters. Traditional methods to assess solifluction …

Climate variability during the Mid‐Late Holocene has influenced the activity of geomorphic
processes in the current periglacial belt of the Sierra Nevada. We studied two types of …

Lateral moraines represent important sediment storages and are one of the most dynamic
areas within glacier forelands. Following glacier retreat, lateral moraine slopes adjust as …

Abstract Sediments at Pias (Galicia) provide evidence of Upper Pleistocene glacial activities
at a valley junction in the north-western mountains of Spain. The sedimentary sequence …