Icebergs
are blocks of fresh-water ice that break off from glaciers and float
out to sea. Glaciers are formed in polar regions where snowfall lasts
for centuries, or even millennia, without entirely melting, and is
eventually compressed into ice.
In
the North Atlantic, most icebergs originate from the tidewater glaciers
of Western Greenland. Compressed snow becomes firm, a granular snow,
transformed eventually by pressure into a dense ice. The weight of the
icecap builds, causing the ice to flow as much as 60 feet a day through
openings in the coastal mountains.
Rising and falling tides cause slabs of ice to break off and form moving `rivers of ice.'
Published in The Hindu on June 06, 2002.
Published in The Hindu on June 06, 2002.