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Great Barrier Reef @ nationalgeographic.com (Site not responding. Last check: 2007-10-07) |
 | | Fringing reefs grow outward from the mainland’s shores, but more often they are found surrounding the region’s 618 continental, or high, islands, which were mountains and hills along Australia’s Ice Age coast before the glaciers melted and raised sea levels; the Aborigines’ legends of ancient generations walking out to those islands are true. |
 | | A coral reef is made of “squillions” of coral colonies plus other limestone depositing organisms, growing on and among the skeletons of their predecessors, and the sands and silts derived from them. |
 | | On the Great Barrier Reef, depending on where it grows, a reef can be either a ribbon reef (on the continental shelf edge), a platform reef (on the shelf), or a fringing reef (along the continental islands and mainland). |
| www.nationalgeographic.com /ngm/0101/feature2 (5781 words) |
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