Barrytown Flats | |
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Coordinates: 42°14′38″S 171°19′35″E / 42.24389°S 171.32639°E | |
Location | West Coast, New Zealand |
Age | 6,500 years |
Formed by | Glacial outwash |
Dimensions | |
• Length | 17 km |
• Width | 1.5 km |
Elevation | 10 m (30 ft) |
Highest elevation | 30 m |
The Barrytown Flats are a 17 km (11 mi) coastal plain north of Greymouth on the West Coast of New Zealand's South Island. A series of postglacial shorelines and dunes backed by a former sea cliff,[1] they was originally covered with wetland and lowland forest, including numerous nīkau palms (the southern limit of this species on the West Coast).[2] The sands were extensively sluiced and dredged for gold from the 1860s, centred on the small settlement of Barrytown.[3] The drier areas of the flats have been converted into pasture, but significant areas of forest remain, including Nikau Scenic Reserve.[4] The flats are bordered by Paparoa National Park and the only breeding site of the Westland petrel (Procellaria westlandica).[5] There are significant deposits of ilmenite (titanium dioxide) in the Barrytown sands, and there have been several mining proposals, but the possible environmental consequences have been contentious.[citation needed]