The growth will extend upstream and increase in width until the point where the frazil ice accumulations bridge together and block the water.
12.
The ice cover is composed of juxtaposed frazil ice pans and break-away border ice pieces that consolidate in the river flow direction.
13.
The uppermost layer of the ocean is supercooled to slightly below the freezing point, at which time tiny ice platelets ( frazil ice ) form.
14.
When the irregular frazil crystals collect, they form something like an icy city filled with streets, elevators and bridges that link countless small pocketlike abodes.
15.
If the level of turbulence is sufficient, the frazil ice will be mixed down into the upper layer and form a surface layer of grease ice.
16.
"' Grease ice "'is a very thin, soupy layer of frazil crystals clumped together, which makes the ocean surface resemble an oil slick.
17.
On the swells far below, long ribbons of grease ice _ a thin, transparent film made from jumbled ice crystals known as frazil _ extended from the pack edge.
18.
Frazil ice has also been demonstrated to form beneath temperate ( or " warm-based " ) glaciers as water flows quickly downhill and supercools due to a rapid loss of pressure.
19.
As the crystals grow in number and size, the frazil ice will begin to adhere to objects in the water, especially if the objects themselves are at a temperature below water s freezing point.
20.
With any kind of turbulence in the water, these fragments break up further into random-shaped small crystals which form a suspension of increasing density in the surface water, an ice type called frazil or grease ice.
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