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Whatipu
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. 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. Geography 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. Major features of Whatipu include Te Toka-Tapu-a-Kupe / Ninepin Rock and Paratutae Island, which are remnants of the Miocene era Waitākere Volcano. From the 1930s to the 1960s, sandy material began accumulating at Whatipu, creating a 1.5km strip of sand, where plants and fresh water swamps developed. Much of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whatipu Beach
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. 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. Geography 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. Major features of Whatipu include Te Toka-Tapu-a-Kupe / Ninepin Rock and Paratutae Island, which are remnants of the Miocene era Waitākere Volcano. From the 1930s to the 1960s, sandy material began accumulating at Whatipu, creating a 1.5km strip of sand, where plants and fresh water swamps developed. Much of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whatipu From Ōmanawanui Trail
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. 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. Geography 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. Major features of Whatipu include Te Toka-Tapu-a-Kupe / Ninepin Rock and Paratutae Island, which are remnants of the Miocene era Waitākere Volcano. From the 1930s to the 1960s, sandy material began accumulating at Whatipu, creating a 1.5km strip of sand, where plants and fresh water swamps developed. Much of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paratutae Island
Paratutae Island, also known as Paratūtai Island, is an island at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area. Geology The island is a portion of a Miocene era volcanic dyke swarm. History In Te Kawerau ā Maki oral histories, the island was visited by the Polynesian navigator Kupe. A section of the island is known by the name Te Hoe-a-Kupe ("The Paddle of Kupe"), referring to the location where Kupe struck his paddle against the island, to commemorate his visit. The island was the location of a Te Kawerau ā Maki defensive pā, guarding the entrance to the Manukau Harbour. Around the year 1700, the pā was captured by Kawharu, the famed Tainui warrior who led Ngāti Whātua warriors to take the Waitākere Ranges area. The island is one of the few locations where pre-European Māori textiles have been found, during an archaeological survey in the early 1900s. The etymology of the island's name is contested. Many attest that the word is a corr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paorae
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 (sweet potato) 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. Geology New Zealand geologist Bruce Hayward theorised that Paorae formed from accumulated volcanic material from the Hatepe eruption of the Taupō Volcano, which occurred 1,800 years ago. Sediment from the eruption washed down the Waikato River, forming a large sand bank north of the Waikato River mouth, along the Āwhitu Peninsula. The land eroded in the 18th century, but material from Paorae continues to move northwards up the west coast. History Māori his ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Toka-Tapu-a-Kupe / Ninepin Rock
Te Toka-Tapu-a-Kupe / Ninepin Rock is an island at the mouth of the Manukau Harbour, at Whatipu in the Waitākere Ranges area. Geology The island is a volcanic plug of the Miocene era Waitākere Volcano, composed of stratified rudite and intrusive andesite. The rock is what remains of one of the volcano's funnel-shaped vents on the eastern side of the mountain, which was uplifted from the sea between 3 and 5 million years ago. The island is a volcanic plug of the Miocene era Waitākere Volcano, composed of stratified rudite and intrusive andesite. The rock is what remains of one of the volcano's funnel-shaped vents on the eastern side of the mountain, which was uplifted from the sea 17 million years ago. As the volcano aged and eroded, the vent filled with collapsed lava, scoria and volcanic bombs, until it formed into its modern-day shape. History The traditional name for the rock, Te Toka-Tapu-a-Kupe, refers to the Polynesian navigator Kupe. According to Te Kawerau ā Mak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anawhata
Anawhata is a beach on the coast of New Zealand west of Auckland. Geography Anawhata Beach is located along the West Coast of West Auckland, between the Tasman Sea and the Waitākere Ranges. It is located south of Te Henga / Bethells Beach, and north of Piha. The Anawhata Stream exits into the Tasman Sea at Anawhata. The beach and coastal area including Parera Point is home to a number of plant species, including New Zealand flax, toetoe, tauhinu, ''Muehlenbeckia axillaris'' and buffalo grass. History Local iwi (tribe) Te Kawerau ā Maki occupied this area for hundreds of years, and many settlements and fortifications were established. The name Anawhata refers to the elevated rock shelters found in the surrounding bluffs, which were used during seasonal fishing expeditions. These caves feature in Te Kawerau ā Maki legends, where a woman of high birth was saved from being imprisoned in a cave on the beach, by her lover who rescued her by lowering a rope down from the cliff ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
HMS Orpheus (1861)
HMS ''Orpheus'' was a ''Jason''-class Royal Navy corvette that served as the flagship of the Australian squadron. ''Orpheus'' sank off the west coast of Auckland, New Zealand on 7 February 1863: 189 crew out of the ship's complement of 259 died in the disaster, making it the worst maritime tragedy to occur in New Zealand waters. The ship HMS ''Orpheus'' (named after the Greek hero) was a ''Jason''-class corvette, a screw-driven vessel built in Chatham Dockyard in Kent, England, in 1861. She was owned by the Royal Navy, and was 69 metres long with a crew of 259. ''Orpheus'' was commanded by Captain Robert Heron Burton. She displayed a broad pennant to indicate that Commodore William Farquharson Burnett, senior officer of HM ships and vessels on the Australian and New Zealand Stations, was also on board. It was wrecked when delivering naval supplies and troop reinforcements to Auckland for the New Zealand Wars. Background ''Orpheus's'' first journey was in December 1861 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitākere Ranges
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 of public and private land. The area, traditionally known to Māori as ''Te Wao Nui o Tiriwa'' (The Great Forest of Tiriwa), is of local, regional, and national significance. The Waitākere Ranges includes a chain of hills in the Auckland Region, generally running approximately from north to south, 25 km west of central Auckland. The ranges are part of the Waitākere Ranges Regional Park. From 1 May 2018 the forested areas of the Waitākere Ranges Regional Park were closed, with some exceptions, while Auckland Council upgraded the tracks to dry foot standard protect the roots and to prevent the spread of kauri dieback, bacteria that affect kauri trees and prevents them from getting nutrients, effectively killing them. There is no cure. But Etymology The name ''Wai-tākere'' origina ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitakere City Council
Waitākere City was a territorial authority in West Auckland, New Zealand; it was governed by the Waitākere City Council from 1989 to 2010. It was New Zealand's fifth-largest city, with an annual growth of about 2%. In 2010 the council was amalgamated with the other authorities of the Auckland Region to form the current Auckland Council. The name "Waitākere" comes from the Waitākere River in the Waitākere Ranges. History Before being settled by Europeans, the Māori iwi Te Kawerau a Maki and Ngāti Whātua had already settled in the Waitakere area. In the 1830s, European settlers started to arrive, concentrating on timber milling, kauri gum digging and flax milling, with brickworks and pottery industries following later. In the 20th century, industry and service trades started to grow, with population taking off after World War II, partly due to improved transport links with Auckland City, such as the Northwestern Motorway, whose first section opened in 1952. Subu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karekare, New Zealand
Karekare is a small coastal settlement in West Auckland, New Zealand, sandwiched between the Waitākere Ranges and a large black sand surf beach. Geography It is located west of Auckland city centre, south of the larger beach of Piha. It is north of Whatipu, south of Piha and west of the Centennial Memorial Park and Water Catchment area, which cover most of the native bushland Waitākere Ranges. Karekare Beach is the confluence of the Company Stream, which was traditionally known by the name Waiteahoaho, and the Karekare Stream. The Karekare Falls are located inland from the beach. The beach at Karekare is split into two sections separated by the, Karekare Stream, Karekare Beach to the south and Tāhoro / Union Bay, to the north. Two major geographical sites within Karekare are The Watchman, traditionally known by the names Te Matua and Te Tokamatua, a significant knoll on the beach's ridge, and Paratahi Island, located to the south of Karekare. Karekare is the remains of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kupe
Kupe ( ~1180-1320) was a legendary Polynesian explorer, navigator and great rangatira of Hawaiki, who is said to have been the first human to discover New Zealand. Whether Kupe existed historically is likely but difficult to confirm. He is generally held to have been born to a father from Rarotonga and a mother from Raiatea, and probably spoke a proto-Māori language similar to Cook Islands Māori or Tahitian. His voyage to New Zealand would ensure that the land would be known to the Polynesians, and he would therefore be responsible for the genesis of Māori civilisation. Kupe features prominently in the mythology and oral history of some Māori iwi (tribes), but the details of his life differ between iwi. Various legends and histories describe Kupe's extensive involvement in the settlement of Aotearoa, around 1000–1300 CE, with many talking of his achievements, such as the hunting and destruction of the great octopus, Te Wheke-a-Muturangi. Time of arrival Estimates of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Region
Auckland () is one of the sixteen regions of New Zealand, which takes its name from the eponymous urban area. The region encompasses the Auckland Metropolitan Area, smaller towns, rural areas, and the islands of the Hauraki Gulf. Containing percent of the nation's residents, it has by far the largest population and economy of any region of New Zealand, but the second-smallest land area. On 1 November 2010, the Auckland region became a unitary authority administered by the Auckland Council, replacing the previous regional council and seven local councils. In the process, an area in its southeastern corner was transferred to the neighbouring Waikato region. Geography On the mainland, the region extends from the mouth of the Kaipara Harbour in the north across the southern stretches of the Northland Peninsula, through the Waitākere Ranges and the isthmus of Auckland and across the low-lying land surrounding the Manukau Harbour, ending within a few kilometres of the mouth o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
