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The largest glacials were 2, 6, 12, and 16; the warmest interglacials, 1, 5, 9 and 11.
There is a general correspondence between glacials in different regions.
Extensive evidence now shows that a number of periods of growth and retreat of continental glaciers occurred during the ice age, called glacials and interglacials.
The advent of sediment and ice cores revealed the true situation: glacials are long, interglacials short.
Rapid glacial erosion of mountain belts likely keeps pace with tectonic uplift, thus limiting the height of mountain belts.
Viewed from the road above, the crushed glass roof covering and opaque glass skin of the walls dissolve the building into its glacial context.
In this landscape a powerful combination of natural and artificial land forms exist of a scale reminiscent of glacial action or volcanic action or flooding.
Large granite glacial boulders unearthed in the mining process.
There is no systematic correspondence of pluvials to glacials, however.
There is currently no evidence available for microbes living in glacial ice without initially melting it before analysis.
The registry clerk also noted that the glacial rivers were not so dangerous or difficult to cross as later became dominant in the area descriptions.
Glacial drift, both as till and fluvial deposits, is a major contributor to a variety of both micro- and macro-landforms.
The lake is fed by ephemeral glacial streams during 6 -8 weeks in the summer.
Most investigators have accepted a glacial formation, but some prefer a soft-sediment mechanism.
On short time scales, there seems to be a rather clear relationship between sedimentation rates and glacial- interglacial cycles.
