As glacial geologists, some of the biggest questions that we'd like to answer are not only how large former ice sheets were, but also how fast did the recede and how quickly did they thin?
As a glacial geologist, George was responsible for the areal extent of these ice sheets and, as a glaciologist, I was responsible for their vertical extent.
Not exact matches
Geologists at UC Santa Cruz have now taken a close look at the structure and chemistry of
glacial polish and found that it consists of a thin coating smeared onto the rock
as the glacier moved over it.
Terrestrial
glacial geologists (such
as ourselves) can gain information of past
glacial behaviour from mapping and dating former ice sheet extents, and determining the rates at which they receded and thinned, [e.g., 16, 17 - 19].
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As glaciologists and
glacial geologists, we respond to the article «Glaciers — science and nonsense» by Cliff Ollier in the March issue of Geoscientist1.
Due largely to the discovery of stalactites in the underwater caves found in the Belize Barrier Reef,
geologists have discovered that the Belize Barrier Reef was not created by volcanic activity (
as many reefs are) but instead by the most recent
glacial period instead.
My field
geologist gut instinct tells me that the great forcings of major
glacial periods (insolation, albedo, etc.) are regional and radically focused direct surface application or radiation of extra heat
as compared with the well mixed, relatively homogeneous and isotropic CO2 tropospheric increase.
Formally, it is termed
glacial inception, informally we
geologists refer to it
as «the climatic madhouse».
In 2010
geologists found evidence for a Dryas trigger in a massive release of
glacial meltwater,
as Broecker had predicted, only by way of the Mackenzie River system of northern Canada rather than the St. Lawrence, Murton et al. (2010).