Whatipu | |
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Coordinates: 37°01′48″S174°28′48″E / 37.03000°S 174.48000°E | |
Location | Auckland Region, New Zealand |
Whatipu is a remote beach on the west coast of the Auckland Region in the North Island of New Zealand. The Whatipu area has been managed as a scientific reserve by the Auckland Regional Council since 2002. [1] The road to it is unsealed. To the south of Whatipu is Manukau Harbour. To the north is Karekare. Whatipu is located at the southern end of the Waitākere Ranges. Shifting sands have substantially changed the beach since the 1940s. Over 6 square kilometres has been added to the beach since then.[ citation needed ]
Between 3 and 5 million years ago, tectonic forces between the Pacific Plate and Australian Plate uplifted the Waitākere Ranges and subsided the Manukau Harbour. [2] Major features of Whatipu include Te Toka-Tapu-a-Kupe / Ninepin Rock and Paratutae Island, which are remnants of the Miocene era Waitākere Volcano. [2] From the 1930s to the 1960s, sandy material began accumulating at Whatipu, creating a 1.5 km strip of sand, where plants and fresh water swamps developed. [3] [4] [2] Much of the sandy material was formed from Paorae, a former flat sand dune that eroded in the 18th century. [2]
The Whatipu area is predominantly an Exposed Coastal Ecosystem, dominated by sand dunes and pōhutukawa trees, as well as saltspray tolerant species such as Urostemon kirkii , taupata, Veronica obtusata and horokaka. The hilly Waitākere Ranges areas further from the beaches are dominated by a warm lowlands pūriri forest, with a narrow band of mānuka-dominated band of Stormy Coastal Hill Ecosystem. [5]
The legendary voyager Kupe is said to have visited Whatipu when exploring Aotearoa. Te Toka-Tapu-a-Kupe / Ninepin Rock at the southern end of Whatipu are named after his visit. [6] In pre-European times the area was actively used by Māori, living along the coastline and river valleys. [7] There are caves about 20 minutes walk from the carpark, but there is no access from the caves to the beach. These caves and rock shelters were used as refuges during times of war between the 16th and 18th centuries. [7] Textile remains such as fishing nets, baskets, cloak fragments were collected from four archeological sites in the area in the early 1900s: one at Whatipu and three on Paratutae Island to the south east. [8]
Whatipu was part of the Hikurangi purchase by the Crown in 1853. The Te Kawerau tribe had reserves set aside at Bethells Beach and Piha. [9]
HMS Orpheus ran aground just inside the Manukau Harbour entrance south of Whatipu in 1863 with the loss of 189 lives. It was the biggest shipping disaster in New Zealand history. [10]
Nicholas Gibbons, a sawmill operator in St Johns, Newfoundland, came to New Zealand in 1853. In March 1854 they purchased land in the Waitakeres and started a large timber milling operation in Whatipu and the wider area that would last until the 1870s. [11] The timber mill was built at Whatipu in 1867 to service the kauri trade. The Whatipu Stream was dammed during the establishment of the mill. [12] A tramline was built to a second timber mill three kilometers north in 1870, and eventually extended up to Piha and Anawhata. The mills closed in 1886 when the kauri ran out. While the timbermill was open, mill workers used the larger caves in the area were as a popular venue for meetings, [13] and in the early 20th century the largest cave was used for dances, but sand has since drifted into the cave and the dance floor is now covered by five metres of sand. [14]
In the latter 19th century, Whatipu was used as black market port, where perfume, spirits and tobacco were smuggled into New Zealand. [15] A road connecting Whatipu to Auckland was constructed in the 1920s. [16]
In 2005, the remains of a man who had been missing for four years were found by police at Whatipu's Destruction Gully. It was speculated that the man was the victim of an accident during fishing on the Manukau Harbour. [17] In 2006, the location was featured on Ghost Hunt , a New Zealand paranormal television show. [18] In the 21st century, Whatipu has been used for the Wild Turkey Off-Road Half Marathon/15 km. [19] The Whatipu Beach Beacon is a lighthouse of the area. [20]
Whatipu has four category II Auckland Council heritage listings. These are: Whatipu Lodge, an unnamed dwelling, Whatipu Wharf, and a commemorative plaque at Paratutai. [11]
The Whatipu beach does not have a surf patrol. Swimming may not be safe due to rips, in common with all beaches west of Auckland.
Whatipu is the starting point for the Whatipu-Gibbons Track & Kura-Omanawanui Tracks, a six-hour return walking track. It leads up the hill to the right of the carpark and is clearly marked.[ citation needed ] It follows the top of the cliffs to the Pararaha Valley where it descends to the beach at Pararaha point. It then follows the beach back to Whatipu. Paratutae Rock at the harbour entrance is difficult and particularly dangerous to climb down. [21] The Kura-Omanawanui Tracks are the other notable walk out of Whatipu. Follows Kura Track eastwards alongside the stream through bush, then climbs steeply to Puriri Ridge and the Whatipu Road. Back via Omanawanui Track, a switchback ridge in open bush with views across the Manukau Harbour and the Whatipu valley to the west coast. Time 4 hours. [22]
The Manukau Harbour is the second largest natural harbour in New Zealand by area. It is located to the southwest of the Auckland isthmus, and opens out into the Tasman Sea.
Henderson is a suburb of West Auckland, in the North Island of New Zealand. It is 13 kilometres (8.1 mi) west of Auckland city centre, and two kilometres (1.2 mi) west of the Whau River, a southwestern arm of the Waitematā Harbour. The suburb is located within the Henderson-Massey Local Board of the Waitākere Ward, one of the thirteen administrative divisions of Auckland Council.
The Waitākere Ranges is a mountain range in New Zealand. Located in West Auckland between metropolitan Auckland and the Tasman Sea, the ranges and its foothills and coasts comprise some 27,720 hectares of public and private land. The area, traditionally known to Māori as Te Wao Nui o Tiriwa, is of local, regional, and national significance. The Waitākere Ranges includes a chain of hills in the Auckland Region, generally running approximately 25 kilometres (16 mi) from north to south, 25 km west of central Auckland. The ranges are part of the Waitākere Ranges Regional Park.
Karekare is a small coastal settlement in West Auckland, New Zealand, sandwiched between the Waitākere Ranges and a large black sand surf beach.
Anawhata is a beach on the coast of New Zealand west of Auckland.
The Manukau Heads is the name given to the two promontories that form the entrance to the Manukau Harbour – one of the two harbours of Auckland in New Zealand. The southern head, at the northern tip of Āwhitu Peninsula, is simply termed "The South Head", whereas the northern head is named "Burnett Head". Both heads are hilly areas of land that rise steeply from the water to over 240m within less than 400m of the shoreline.
Huia is a western coastal settlement in West Auckland, New Zealand and forms part of the Waitākere Ranges Regional Park. The majority of houses in Huia are located along Huia Road, which arcs around Huia Bay and heads west towards Little Huia.
Kitekite Falls is a scenic 3-tiered waterfall near Auckland, New Zealand. The falls drop a total of 40 metres (130 ft). From the lookout on Kitekite track the falls appear even higher because there is white water running over rocks into a small pool from the upper swimming hole, then falling down into a large pool, then falling to a small pool before beginning an almost vertical descent in the final 3-tiers, making the total height closer to 80 metres (260 ft). They are located on the Glen Esk Stream near Piha Beach.
Lion Rock is a rocky headland located on Piha Beach in the Waitākere Ranges area of the Auckland Region, New Zealand.
The Āwhitu Peninsula is a long peninsula in the North Island of New Zealand, extending north from the mouth of the Waikato River to the entrance to Manukau Harbour.
West Auckland is one of the major geographical areas of Auckland, the largest city in New Zealand. Much of the area is dominated by the Waitākere Ranges, the eastern slopes of the Miocene era Waitākere volcano which was upraised from the ocean floor, and now one of the largest regional parks in New Zealand. The metropolitan area of West Auckland developed between the Waitākere Ranges to the west and the upper reaches of the Waitematā Harbour to the east. It covers areas such as Glen Eden, Henderson, Massey and New Lynn.
The Little Muddy Creek is a river of the Auckland Region of New Zealand's North Island. It flows south from its source in Titirangi, meets the tributaries Waituna Stream and Waiohua Creek which run through the suburbs of Waima and Woodlands Park, before reaching the Manukau Harbour.
The Big Muddy Creek is an estuarine tidal inlet of the Auckland Region of New Zealand's North Island. It flows south from its tributary rivers, the Nihotupu Stream and the Island stream in the Waitākere Ranges which are dammed at the Lower Nihotupu Reservoir, towards the Manukau Harbour.
Little Huia is a western coastal settlement of West Auckland, Auckland, New Zealand and forms part of the Waitākere Ranges Regional Park, bordering the Manukau Harbour. It is located south-west of the settlement of Huia.
Te Toka-Tapu-a-Kupe / Ninepin Rock is an island at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area.
Paratutae Island, also known as Paratūtai Island, is an island off New Zealand at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area.
Pukematekeo is a hill in the Waitākere Ranges of the Auckland Region of New Zealand's North Island. It is located west of Henderson, and is the northernmost hill in the Waitākere Ranges Regional Park.
Paorae is the name of a migrating coastal dune, formerly located west of the Āwhitu Peninsula in the Auckland Region of New Zealand. Paorae was an important area for cultivating kūmara and taro for Tāmaki Māori tribes Ngāiwi and Ngāoho, and later Waikato Tainui. The land eroded in the 18th century, becoming known as a legendary "Māori Atlantis" to European New Zealanders. Material from Paorae forms the Manukau Heads sandbars and the modern day beach at Whatipu, which began forming in the 1930s.
Te Rau-o-te-Huia / Mount Donald McLean is a hill in the Waitākere Ranges of the Auckland Region of New Zealand's North Island. It is located to the south of the ranges, near the township of Huia. It is the highest peak of the Waitākere Ranges that borders the Manukau Harbour.
Piha Stream is a stream of the Auckland Region of New Zealand's North Island. It flows westwards from its sources in the Waitākere Ranges through Piha village, and enters the Tasman Sea south of Lion Rock.