Pigeon Island (Houtman Abrolhos)
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Map of Pigeon Island
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| Geography | |
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| Location | Indian Ocean, off the coast of Western Australia |
| Coordinates | 28°27′18″S 113°43′34″E / 28.45500°S 113.72611°ECoordinates: 28°27′18″S 113°43′34″E / 28.45500°S 113.72611°E |
| Archipelago | Houtman Abrolhos |
| Area | 4.3 ha (11 acres) |
| Length | 430 m (1,410 ft) |
| Width | 140 m (460 ft) |
| Highest elevation | 3 m (10 ft) |
| Administration | |
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Australia
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| State | Western Australia |
| Demographics | |
| Population | Seasonally inhabited by lobster fishers (2006) |
Pigeon Island is a small island located need the middle of the Wallabi Group of the Houtman Abrolhos, an archipelago off the coast of Western Australia. It is almost entirely given over to western rock lobster fishers' camps, and as a result is far more disturbed than most other islands in the archipelago. A nearby island also seasonally populated by fishers is named Little Pigeon Island, hence Pigeon Island is sometimes referred to as "Big Pigeon Island".
The geographic location of Pigeon Island suggests that it might have been visited by survivors of the 1629 Batavia shipwreck, but there is no surviving evidence of this, either documentary or archaeological. It was mined for guano in the 20th century.
Pigeon Island is roughly triangular in shape, with a short side on the south west, and two long sides coming together at a point in the north east. The island is covered with infrastructure, with a high density of huts covering the entire island, right down to the water line; in total there are 54 camps, a school and a pub. There are also around 20 jetties, mainly along the northwest side, as this is the only direction from which the island may be approached by boat. The island is surrounded by reef to the south and east, but a passage known as Pigeon Island Anchorage runs along the northwest side.
The basement of Pigeon Island is the Wallabi Limestone, a dense calcretised, coral limestone platform that underlies the entire Wallabi Group. This platform, which arises abruptly from a flat shelf, is about 40 metres thick, and is of Quaternary origin. Reef that formed during the Eemian interglacial (about 125,000 years ago), when sea levels were higher than at present, are now emergent in places, and constitute the basement of the group's "central platform" islands, of which Pigeon Island is one.
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