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Everyone knows the story of the Titanic1, the great ocean liner that struck an iceberg2 and sank to the bottom of the Atlantic. Less widely known is the iceberg’s story: where did it come from, and how did it get in the way of the ship?
Although the vast majority of icebergs3 come from the Antarctic region, icebergs found in the North Atlantic, including the one that sank the Titanic, come mostly from the coast of Greenland. Thousands of years of snowfall on the Greenland ice cap causes the snow to compact and form dense4 ice sheets and glaciers5.
The weight of the glaciers and sheets forces them to flow down towards the coast where, at the water’s edge, warm waves and spring weather weaken the ice, causing pieces to break off and enter the sea as icebergs.
Pushed by wind and the Labrador Current, Greenland-produced icebergs drift southward. Many become stuck in shallow waters, but those that stay in the main current make it to the open sea, where they last for approximately two years before melting completely.
Since typically only 1/7th of an iceberg is visible above the ocean surface, it is almost impossible to gauge6 its size with the naked eye. The actual size of North Atlantic icebergs varies, from a small car to a ten-story building.
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1 titanic | |
adj.巨人的,庞大的,强大的 | |
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2 iceberg | |
n.冰山,流冰,冷冰冰的人 | |
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3 icebergs | |
n.冰山,流冰( iceberg的名词复数 ) | |
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4 dense | |
a.密集的,稠密的,浓密的;密度大的 | |
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5 glaciers | |
冰河,冰川( glacier的名词复数 ) | |
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6 gauge | |
v.精确计量;估计;n.标准度量;计量器 | |
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7 dwarfed | |
vt.(使)显得矮小(dwarf的过去式与过去分词形式) | |
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