glacial flow

glacial flow

[¦glā·shəl ′flō]
(hydrology)
References in periodicals archive ?
Driven by dim sunlight, this would be directly comparable to the hydrological cycle that feeds ice caps on Earth, where water is evaporated from the oceans, falls as snow, and returns to the seas through glacial flow.
These are important products for mapping topography to produce digital elevation models and to monitor surface deformation caused by, for example, mining, earthquakes, volcanic activity, melting permafrost and glacial flow.
Not just the melting on the surface, but melting at the base of the ice sheet, which is causing much faster glacial flow into the ocean.
Plant geography, soil character, rock cycles, tectonics, weathering, groundwater, surface water flow, glacial flow, desert and coastal environments are covered in turn, with the final chapter focusing on the relevance of physical geography to environmental issues, with recent case studies.
Yet there's something irresistible about watching the glacial flow of pitch.
These structures are believed to be caused by the passage of loose debris and ice during the 'Amazonian' period (which continues to this day) due to glacial flow along the channel.
The 100-year-old mountain railway, which now has four uniquely-designed stops (but all of them with the same look, hinting at the curve of the mountains, glacial flow and other echoes of nature), winds up the mountain on the city's northern edge to the village of Hungerberg.
various geological structures (faults, lineaments, contacts, fold axes, glacial flow indicators, etc.
Written especially to draw attention to underutilized yet remarkably powerful and profound human attributes, A New Romanticism explores the profound emotions of hope and despair, the majesty of the natural world, the glacial flow of time, and the twin cycles of creation and destruction.
These are informally discussed as: (a) phase 1, early glacial flow; (b) phase 2, glacial maximum; and (c) phase 3, late glacial flow.
There are yet more glacial flow patterns visible in the valley at the centre of the image.
This glacial flow direction represents initial glacial erosion from the advance of local Appalachian ice (Pronk et al.