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What is an Iceberg? History in crystals
Icebergs are nothing more than solid water. They float because the density of the ice is less than the density of sea water. Icebergs come in all shapes and sizes, they have been compared to mountains, pyramids and castles. Many icebergs are moulded into unusual and fascinating shapes by the action of the wind and waves. The process of melting causes an iceberg to change shape, too. Icebergs are formed both in the Arctic and the Antarctic oceans. Arctic icebergs come mainly from Greenland, a huge island which is almost completely covered by an ice sheet. It is estimated that the Greenland ice cap produces from 10,000 to 30,000 icebergs each year. Up to several thousand can reach Newfoundland waters, starting in the north at Quirpon Island. The rest are lost by diversion into straits or bays, by being grounded in many fjords along Baffin Island and by deterioration. The course of an iceberg cannot be judged by wind direction alone. Since nine-tenths of an iceberg's mass lies under water, much more of a bergs surface is affected by water currents than by wind. The final direction is one that takes both the wind and currents into account. A berg can move against or across the wind, as well as downward or at small angles to it. Facts and Figures
Types and Sizes Types and size comparisons of icebergs:
Where to Search The further north you go, the more likely you are to find bergs, especially after mid July. As the bergs drift south in the Labrador Current they enter "Iceberg Alley" which extends along the coast of Newfoundland. Any of the bays and coves along the north coast of the island can be harbouring these ice giants but, as the summer progresses, those in the southern waters melt more rapidly. While May and June are considered the best months for iceberg viewing, in the north the colder waters and more plentiful bergs mean that impressive structures can exist into September (we once counted 11 from our helipad on Sept. 7th). |
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