"a normal process that happens all the time".
It is indeed Tom, all glaciers that terminate in the sea must break up at the tail.
Roy.
"a normal process that happens all the time".
Get yourself a trip up to the base of a glacier when it's cold enough to freeze your breath and you may well see the melt water cascading out from under the glacier ice.Digit":35gfnepf said:.....and can you get glacial melt water when temps are low enough to freeze sea water?
Hence I am puzzled.
Roy.
see the melt water cascading out from under the glacier ice.
2
MOVEMENT OF WATER IN GLACIERS*
By R. L. SHREVE
(University of California, Los Angeles, California 90024, U.S.A.)
ABSTRACT. A network of passages situated along three-grain intersections enables water to percolate
through temperate glacier ice. The deformability of the ice allows the passages to expand and contract in
response to changes in pressure, and melting of the passage walls by heat generated by viscous dissipation
and carried by above-freezing water causes the larger passages gradually to increase in size at the expense
of the smaller ones. Thus, the behavior of the passages is primarily the result of three basic characteristics:
(J) the capacity of the system continually adjusts, though not instantly, to fluctuations in the supply of melt
water; (2) the direction of movement of the water is determined mainly by the ambient pressure in the ice,
which in turn is governed primarily by the slope of the ice surface and secondarily by the local topography
of the glacier bed; and, most important, (3) the network of passages tends in time to become arborescent,
with a superglacial part much like an ordinary river system in a karst region, an englacial part comprised
of tree-like systems of passages penetrating the ice from bed to surface, and a subglacial part consisting of
tunnels in the ice carrying water and sediment along the glacier bed. These characteristics indicate that a
sheet-like basal water layer under a glacier would normally be unstable, the stable form being tunnels:
and they explain, among other things, why ice-marginal melt-water streams and lakes are so common,
why eskers, which are generally considered to have formed in subglacial passages, trend in the general
direction of ice flow with a tendency to follow valley floors and to cross divides at their lowest points, why
they are typically discontinuous where they cross ridge crests, why they sometimes contain fragments from
bedrock outcrops near the esker but not
Me too.I know whom I would prefer to believe.
However, i think what we're asking is, what was going around when HE discovered that fire and or hot water made some foods easier to eat/digest and allowed new foods (starchy roots, etc) to be added to their diet.
in areas unrelated to their area of competence - that's academic bad form.
Al-Gore doesn't present academic qualifications when he talks about global warming.
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