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Lyttelton Harbour
Lyttelton Harbour / Whakaraupō is one of two major inlets in Banks Peninsula, on the coast of Canterbury, New Zealand; the other is Akaroa Harbour on the southern coast. It enters from the northern coast of the peninsula, heading in a predominantly westerly direction for approximately from its mouth to the aptly-named Head of the Bay near Teddington. The harbour sits in an eroded caldera of the ancient Banks Peninsula Volcano, the steep sides of which form the Port Hills on its northern shore. The harbour's main population centre is Lyttelton, which serves the main port to the nearby city of Christchurch, linked with Christchurch by the single-track Lyttelton rail tunnel (opened 1867), a two lane road tunnel (opened 1964) and two roads over the Port Hills. Diamond Harbour lies to the south and the Māori village of Rāpaki to the west. At the head of the harbour is the settlement of Governors Bay. The reserve of Otamahua / Quail Island is near the harbour head and Ripap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christchurch
Christchurch ( ; mi, Ōtautahi) is the largest city in the South Island of New Zealand and the seat of the Canterbury Region. Christchurch lies on the South Island's east coast, just north of Banks Peninsula on Pegasus Bay. The Avon River / Ōtākaro flows through the centre of the city, with an urban park along its banks. The city's territorial authority population is people, and includes a number of smaller urban areas as well as rural areas. The population of the urban area is people. Christchurch is the second-largest city by urban area population in New Zealand, after Auckland. It is the major urban area of an emerging sub-region known informally as Greater Christchurch. Notable smaller urban areas within this sub-region include Rangiora and Kaiapoi in Waimakariri District, north of the Waimakariri River, and Rolleston and Lincoln in Selwyn District to the south. The first inhabitants migrated to the area sometime between 1000 and 1250 AD. They hunted moa, which led ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Hills
The Port Hills are a range of hills in Canterbury Region, so named because they lie between the city of Christchurch and its port at Lyttelton. They are an eroded remnant of the Lyttelton volcano, which erupted millions of years ago. The hills start at Godley Head, run approximately east–west along the northern side of Lyttelton Harbour, and continue running to the south, dividing the city from the harbour. The range terminates near Gebbies Pass above the head of the harbour. The range includes a number of summits between 300 and 500 metres above sea level. The range is of significant geological, environmental and scenic importance. History The volcano is one of two from which Banks Peninsula was originally formed 12 million years ago. The area was first populated by Māori during the 14th century. During early European settlement some 500 years later the Port Hills presented a challenging barrier between the harbour and the planned settlement of Christchurch, their st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula Volcano
The Banks Peninsula Volcano is an extinct volcanic complex to the east of Christchurch on New Zealand's South Island.Sewell 1986 While the volcano is highly eroded it still forms the majority of Banks Peninsula with a highest point of . It is a composite of two main eruptive centers one originating at Lyttelton Harbour, the other at Akaroa Harbour. The eruptions were predominantly basaltic, with associated andesite and trachytes, with minor rhyolite. The volcanic activity occurred in the Late Miocene and possibly extended into the Early Pliocene. There are four volcanic groups, all of which are within the Māui Supergroup.Mortimer et al. 2014 The Christchurch earthquakes led to rumors of a possible eruption, however, there is no known magma chamber beneath the volcano and there has not been any sign of volcanic activity in the last 5 million years. Origin and relationship to other volcanoes New Zealand's South Island has many extinct volcanic centers with no obvious tectonic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teddington, New Zealand
Teddington is a very small community on Banks Peninsula at the head of Lyttelton Harbour / Whakaraupō. It sits on the junction of the road to Gebbies Pass and the road from Purau to Christchurch. It dates back to the early settlers of Christchurch but is now reduced to a pub and a restored working blacksmith's forge. Tsunami An earthquake near Chile on 23 May 1960 caused a tsunami which crossed the Pacific to hit New Zealand. The tsunami was funnelled up Lyttleton Harbour and flooded low-lying farmland and the Wheatsheaf Tavern in Teddington. A similar event occurred in 2010 following an earthquake in Chile with three waves that were greater than two metres high inundating the head of the harbour around Teddington. An earlier tsunami occurred in 1868 following an earthquake off the coast of Peru. This caused an eight foot high wave to be funnelled up Lyttleton Harbour towards Teddington. Demographics The Teddington statistical area, which extends from Governors Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akaroa Harbour
Akaroa Harbour, is part of Banks Peninsula in the Canterbury region of New Zealand. The harbour enters from the southern coast of the peninsula, heading in a predominantly northerly direction. It is one of two major inlets in Banks Peninsula, on the coast of Canterbury, New Zealand; the other is Lyttelton Harbour on the northern coast. The name Akaroa is an alternative spelling of Whakaroa, Whangaroa or Wangaloa from the Kāi Tahu dialect of Māori. Whakaroa means "Long Harbour". The harbour was used commercially in the mid-19th century for ship-based and shore-based whaling. Cruise ships occasionally enter the harbour, with the passengers visiting Akaroa. Ōnawe Peninsula is at the head of the harbour, the former site of a Māori pā. Settlements Akaroa Harbour's waterfront has been continually inhabited since the 1840s. Akaroa, Duvauchelle, Takapūneke, Takamatua, Barrys Bay, French Farm and Wainui lie on the shoreline of the harbour. They are connected to the rest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canterbury, New Zealand
Canterbury ( mi, Waitaha) is a region of New Zealand, located in the central-eastern South Island. The region covers an area of , making it the largest region in the country by area. It is home to a population of The region in its current form was established in 1989 during nationwide local government reforms. The Kaikoura District joined the region in 1992 following the abolition of the Nelson-Marlborough Regional Council. Christchurch, the South Island's largest city and the country's second-largest urban area, is the seat of the region and home to percent of the region's population. Other major towns and cities include Timaru, Ashburton, Rangiora and Rolleston. History Natural history The land, water, flora, and fauna of Waitaha/Canterbury has a long history stretching from creation of the greywacke basement rocks that make up the Kā Tiritiri o te Moana/Southern Alps to the arrival of the first humans. This history is linked to the creation of the earth, the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Purau Bay
Purau is a small town in Canterbury, New Zealand, facing Lyttelton Harbour. Geography Purau is located on Banks Peninsula, one of the southern bays forming Lyttelton Harbour. History Purau has a long history of Māori settlement. Ngāti Māmoe lived here prior to Ngāi Tahu settling the bay. There are many Māori burial sites in the area. European occupation started in 1843, when the Greenwood brothers started a farm here. They sold to the Rhodes brothers in 1847 ( William Barnard and George, with the latter taking over management of the station). When Robert Heaton Rhodes, another of the Rhodes brothers, came to New Zealand in 1850, he took over Purau. Demographics Purau is described by Statistics New Zealand as a rural settlement, and covers . It is part of the Eastern Bays-Banks Peninsula SA2 statistical area. Purau had a population of 69 at the 2018 New Zealand census, an increase of 18 people (35.3%) since the 2013 census, and an increase of 6 people (9.5%) since t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
