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Matukutūreia

Auckland Region geography stubsAuckland volcanic fieldHills of the Auckland RegionManurewa Local Board Area
Matukutureia or McLaughlin's Hill
Matukutureia or McLaughlin's Hill

Matukutūreia (also McLaughlins Mountain) is one of the volcanic cones in the Auckland volcanic field. It has a peak 73 metres above sea level, and was the site of a pā. The scoria cone was originally crescent-shaped and featured Māori terraces and kumara pits, before extensive quarrying reduced it to a pyramid-shaped mound big enough to support the summit water tank for Papatoetoe. A small part of the summit and the eastern side of the cone were left unquarried, plus a large area of lava flows to the south of the cone remains intact. These remaining parts have recently been transferred to Department of Conservation Management, primarily because of the high heritage values of the Matukuturua Stonefields gardens. Matukutūreia and nearby Wiri Mountain are collectively known as Matukurua (also Ngā Matukurua).From July to September 2010, the water tank was removed from the top of Matukutūreia, as part of an agreement when the land was handed over to the Department of Conservation.

Excerpt from the Wikipedia article Matukutūreia (License: CC BY-SA 3.0, Authors, Images).

Matukutūreia
Stonehill Drive, Manurewa

Geographical coordinates (GPS) Address Nearby Places
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Wikipedia: MatukutūreiaContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N -37.013511 ° E 174.845974 °
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Address

Matukuturua Stonefields Historic Reserve

Stonehill Drive
2242 Manurewa
Auckland, New Zealand
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Matukutureia or McLaughlin's Hill
Matukutureia or McLaughlin's Hill
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Nearby Places

Puhinui Craters
Puhinui Craters

The Puhinui Craters are located in Auckland's Puhinui Reserve and are part of the Auckland volcanic field in the North Island of New Zealand. They were first recognised as volcanic craters in 2011. A cluster of three small maar craters like these is unique in the Auckland volcanic field. Their ages are unknown but most probably all three erupted during the same eruptive episode. They could have been associated with the eruption of nearby Matukutureia (also known as McLaughlin's Mountain) but this is speculation at present. The cluster is composed of three maars, encircled by tuff cones that over tens of thousands of years have been partly breached and eroded by runoff from the small freshwater lakes appearing in the craters shortly after the eruption. Due to the maars' very gentle rise over the otherwise level terrace of Pleistocene age, their volcanic origin had not been recognised earlier. Puhinui Pond Crater, located near the reserve entrance, contains a farm pond. The crater is 200 m × 150 m (660 ft × 490 ft) across and the nearly complete surrounding tuff cone rim rises 1.5–2 m (4.9–6.6 ft) above the pond.Puhinui Arena Crater is breached on both the west and east sides. It is 250 m × 150 m (820 ft × 490 ft) across and its drained and sediment-filled flat floor is 2–2.5 m (6.6–8.2 ft) below the rim of the surrounding tuff ring.Puhinui Eroded Crater lies directly east of Arena Crater on the route of the small stream that drains the latter. Eroded Crater is breached at both west and east ends and its tuff cone partly eroded by the adjacent Puhinui Creek. It is less well-preserved than the other two craters but of similar size.