Glaciers, ice sheets and ice caps represent tectonic systems driven by gravity. Their
movement can be studied in real time and the rheological properties and strength of ice …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Longitudinal surface structures (" flowstripes") are common on many glaciers but their origin
and significance are poorly understood. In this paper we present observations of the …

Abstract The central Red Sea is a nascent oceanic basin. Miocene evaporites, kilometers in
thickness, were deposited during its continental rifting phase and early seafloor spreading …

This paper studies the evolution of a zone in the Fimbul Ice Shelf that is characterised by
large crevasses and rifts west of Jutulstraumen, an outlet glacier flowing into Fimbulisen …

Longitudinal ice-surface structures in the Antarctic Ice Sheet can be traced continuously
down-ice for distances of up to 1200 km. A map of the distribution of~ 3600 of these features …

The morphological properties of glacial deposits located within a cirque-like alcove in
eastern Protonilus Mensae, Mars (Mars grid reference: 54.55° lon, 40.80° lat), have been …

The Antarctic Peninsula has recently seen a rapid breakup of its peripheral ice shelves,
attributed to atmospheric and oceanic warming in the region. Previous work has illustrated …

Fast ice flow on the Antarctic continent constitutes much of the mass loss from the ice sheet.
However, geophysical methods struggle to constrain ice flow history at depth, or separate …

Longitudinal ice-surface structures in the Antarctic Ice Sheet can be traced continuously
down-ice for distances of up to 1200 km. A map of the distribution of∼ 3600 of these …