Barrytown Flats

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Age6,500 years
Elevation10 m (33 ft)
Barrytown Flats
View of Barrytown Flats from Razorback Point
View of Barrytown Flats from Razorback Point
Interactive map of Barrytown Flats
Coordinates: 42°14′38″S 171°19′35″E / 42.24389°S 171.32639°E / -42.24389; 171.32639
LocationWest Coast, New Zealand
Age6,500 years
Formed byGlacial outwash
Dimensions
  Length17 km
  Width1.5 km
Elevation10 m (33 ft)
Highest elevation30 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. Consents for a sand mining operation were granted in 2024 following a three year consenting process. The mining operation will extract 4.8 million tonnes of mineral sands over an area of 63 ha (160 acres).

The Barrytown Flats are at 42º 10' S, 29 km (18 mi) north of Greymouth on the West Coast of the South Island, and immediately south of the pancake rocks of Dolomite Point, Punakaiki. They are 17 km (11 mi) in length north–south, up to 1.5 km (0.93 mi) wide east–west, bounded by the Tasman Sea to the west and the Paparoa Range to the east.[3] The southern end of the flats is defined by the headland Seventeen Mile Bluff, and their northern end by Razorback Point and the mouth of the Punakaiki River.[citation needed]

This coastal plain is mostly below 10 metres (33 ft) in altitude, reaching 30 metres (98 ft) at points, and is crossed by numerous creeks and waterways, the most significant from south to north being Fagan Creek, Granite Creek (near Barrytown), Little Granite Creek, Canoe Creek (which roughly bisects the flats), Deverys Creek, Maher Creek, Waiwhero Creek, and Hibernia Creek (which flows into Nikau Scenic Reserve).[1]

Geology

The eastern boundary of the flats consists of former sea cliffs, and the flats themselves were formed after the end of the last glaciation from coastal progradation – the accumulation of sediment washed down from the hills. Gravel fans have been created by creeks, especially Granite Creek and Canoe Creek, and sandy sediment is constantly carried along the coast by wave action, creating an almost straight shoreline.[1] The Barrytown sands contain gold, ilmenite, garnet, and zircon at sufficient levels to be of economic interest.[3]

Flora and fauna

The most significant remnant of the flats' original vegetation is Nikau Scenic Reserve, a 20 ha block stretching from the coast to the post-glacial cliff. The reserve is notable for containing a full sequence of coastal vegetation. Towards the hills it consists of forest dominated by northern rātā (Metrosideros robusta) and rimu (Dacrydium cupressinum), along with kamahi (Weinmannia racemosa), toro (Myrsine salicina), and nīkau (Rhopalostylis sapida). The sand-dune forest is mostly totara (Podocarpus laetus and P. totara). The younger coastal ridges contain totara, kōwhai (Sophora microphylla) and akeake (Olearia avicenniifolia), and on their seaward side gorse, flax (Phormium spp.) and Coprosma propinqua.[2]

In 2008, 80 ha of Barrytown Flats land owned by Rio Tinto, previously earmarked for ilmenite mining, was designated Te Ara Taiko Nature reserve. A restoration project run by the Department of Conservation (DOC) and Conservation Volunteers New Zealand had planted 200,000 trees on the site by February 2020.[6][7]

History

Mining

References

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