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Achilles Point

Geography of AucklandHauraki GulfHeadlands of the Auckland RegionŌrākei Local Board Area
Looking east over Gentleman's Bay
Looking east over Gentleman's Bay

Achilles Point (Te Pane o Horoiwi – The head of Horoiwi) is a rocky point on the headland at the eastern end of the small sandy beach named Ladies Bay, Auckland, New Zealand. The name 'Te Pane o Horoiwi' can also sometimes refer to the whole headland between St Heliers and Tamaki River estuary. Achilles Point is named after a ship called HMNZS Achilles (70) which defeated the German pocket battleship Admiral Graf Spee in 1939. The headland, from the point round to the Tamaki heads, was previously known as Te Pane o Horoiwi, named after Horoiwi who arrived in New Zealand on the Tainui canoe (waka). Ladies Bay is a secluded beach, below steep cliffs, on the headland west of the lookout over Achilles point. Both Ladies Bay and further to the east, the more secluded Gentleman's Bay beach are unofficially places where nudists can often be found enjoying the sun and sand however the fine for indecent exposure is $200. The secluded bays are also popular with the male gay community. Glover Park is an ancient volcanic crater which erupted about 160,000 years ago. The volcanic tuff ring crater is also known in Māori language as Whakahumu or geologically as the 'St Heliers explosion crater'. It is found in the center of the headland between West Tamaki Head and the eastern end of St Heliers Bay beach. It was filled in during the 1950s to form a public sports field. Before that it formed a seasonal shallow lake or swamp. The seaward side of the tuff crater is falling away down the coastal cliffs to 'Gentleman's Bay' far below. The tuff ring is made from ash and ejected material. The cliffs were there before the volcano erupted so the volcanic rock draped over the clay hill that once existed before sea levels rose and began eroding it away to become the steep cliffs we see today. Some volcanic rocks can be found on the beach below – some fragments ejected from deep in the earth, or blocks of tuff ring that were once perched on top of the cliff. Rangitoto Island is directly to the north, however Rangitoto is a recent eruption (1,000 years ago) and was not always there to shelter the cliffs from powerful wave action. There is an old concrete water tower built on the tuff ring formed around the edge of the crater opposite the seaward side.

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

Achilles Point
Cliff Road, Ōrākei Saint Heliers

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Wikipedia: Achilles PointContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N -36.84339 ° E 174.8638 °
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Address

Achilles Point Lookout

Cliff Road
1074 Ōrākei, Saint Heliers
Auckland, New Zealand
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Looking east over Gentleman's Bay
Looking east over Gentleman's Bay
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Taylors Hill
Taylors Hill

Taylors Hill (also Te Taurere), is a volcano in the Auckland volcanic field. It erupted about 33,000 years ago. Its scoria cone reaches 56 m high. It was the site of a Māori pā (fortification), and retains earthworks from that era such as kumara (sweet potato) pits and terracing. It was most likely first occupied in 1400s, and was an area where ōnewa (greywacke) was quarried to make toki (stone adzes).Waiorohe (Karaka Bay) was a mooring site of Tainui waka inside the west heads of the Tāmaki. From here Horoiwi left the waka and settled with the Tangata whenua at Te Pane o Horoiwi. Te Keteanataua and Taihaua disembarked and made their way to Taurere, whilst Taikehu and others went on by foot to explore the upper reaches of the river and the shores of the Manukau Harbour. The Karaka trees of the bay descend from the sacred Karaka grove Te Uru-Karaka a Parehuia of Taurere Pa. Until the 18th century the area around Taylors Hill was the traditional eastern boundary for Waiohua lands, After the pā was attacked by Ngāti Whātua around the year 1750, Waiohua retreated to South Auckland. Ngāti Whātua gifted the land to Ngāti Pāoa in the late 1700s.The volcano is named for William Taylor, who purchased the land in 1845. The volcano's lower slopes and scoria mounds to the east and south were quarried away following European settlement, with only the north-west section of the volcanic area remaining. The area around the volcanic cone became a public reserve in the 1920s.