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Horotiu
Horotiu is a small township on the west bank of the Waikato River in the Waikato District of New Zealand. It is on the Waikato Plains north of Hamilton, New Zealand, Hamilton and south of Ngāruawāhia. From early in the 20th century it developed around a freezing works and other industries. The North Island Main Trunk railway runs through the town, as did State Highway 1 (New Zealand), State Highway 1 until opening of part of the Waikato Expressway in 2013. An hourly bus runs between Huntly, New Zealand, Huntly and Hamilton. Name The name, Horotiu, seems to have been used interchangeably with Waikato River, or Pukete. Its first use for the current township seems to occur in 1864, shortly after the invasion of the Waikato. Until then, Horotiu was the name of the upper Waikato river, where its current became faster and of Horotiu pā, on its banks, near Cambridge, New Zealand, Cambridge. An 1858 map only shows the name as Horotiu Plains in the area near the pā. The name, Ho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horotiu Geological Map
Horotiu is a small township on the west bank of the Waikato River in the Waikato District of New Zealand. It is on the Waikato Plains north of Hamilton, New Zealand, Hamilton and south of Ngāruawāhia. From early in the 20th century it developed around a freezing works and other industries. The North Island Main Trunk railway runs through the town, as did State Highway 1 (New Zealand), State Highway 1 until opening of part of the Waikato Expressway in 2013. An hourly bus runs between Huntly, New Zealand, Huntly and Hamilton. Name The name, Horotiu, seems to have been used interchangeably with Waikato River, or Pukete. Its first use for the current township seems to occur in 1864, shortly after the invasion of the Waikato. Until then, Horotiu was the name of the upper Waikato river, where its current became faster and of Horotiu pā, on its banks, near Cambridge, New Zealand, Cambridge. An 1858 map only shows the name as Horotiu Plains in the area near the pā. The name, Ho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato Expressway
The Waikato Expressway is a dual carriageway section of (SH 1) in New Zealand's Waikato region. Constructed in stages, it forms part of the link between Auckland and Hamilton. Currently stretching from Auckland to south of Cambridge, the highway was first built in 1993. Throughout its current lifetime, it had underwent many upgrades to optimize traffic flow throughout the Waikato region, including various bypasses of most towns in the region, and lastly Hamilton in 2022. The final part of the Expressway was completed on 12 July 2022. The expressway forms a long continuous four-lane dual carriageway from the Bombay Hills to beyond the town of Cambridge, south-east of Hamilton. Hamilton, as well as several other towns along the current route of SH 1 (such as Huntly, Ngāruawāhia and Cambridge), which have been completely bypassed by the expressway, allowing through traffic to move much more efficiently. History While not officially designated as the Waikato Expressway until t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato River
The Waikato River is the longest river in New Zealand, running for through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Wai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hamilton, New Zealand
Hamilton ( mi, Kirikiriroa) is an inland city in the North Island of New Zealand. Located on the banks of the Waikato River, it is the seat and most populous city of the Waikato region. With a territorial population of , it is the country's fourth most-populous city. Encompassing a land area of about , Hamilton is part of the wider Hamilton Urban Area, which also encompasses the nearby towns of Ngāruawāhia, Te Awamutu and Cambridge. In 2020, Hamilton was awarded the title of most beautiful large city in New Zealand. The area now covered by the city was originally the site of several Māori villages, including Kirikiriroa, from which the city takes its Māori name. By the time English settlers arrived, most of these villages, which sat beside the Waikato River, were abandoned as a result of the Invasion of Waikato and land confiscation (''Raupatu'') by the Crown. Initially an agricultural service centre, Hamilton now has a diverse economy and is the third fastest growing urba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Island Main Trunk
The North Island Main Trunk (NIMT) is the main railway line in the North Island of New Zealand, connecting the capital city Wellington with the country's largest city, Auckland. The line is long, built to the New Zealand rail gauge of and serves the large cities of Palmerston North and Hamilton. Most of the NIMT is single track with frequent passing loops, but has double track - * between Wellington and Waikanae, except for of single-track through tunnels between North Junction ( from Wellington) and South Junction, ( from Wellington), on the Pukerua Bay to Paekakariki section, * between Hamilton and Te Kauwhata (except for the single-track Waikato River Bridge at Ngāruawāhia), and * between Meremere and Auckland Britomart. Around (approximately 65%) of the line is electrified in three separate sections: one section at 1600 V DC between Wellington and Waikanae, and two sections at 25 kV AC: between Palmerston North and Te Rapa (Hamilton) and between Papakura and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waihorotiu Stream
Waihorotiu (from the Māori language, Māori Wai Horotiu), sometimes called the Waihorotiu Stream and the 'Queen Street River', is a stream that ran down the Queen Street, Auckland, Queen Street gully in the Auckland CBD, New Zealand, into the Waitemata Harbour. It has long since been covered over and put underground by the urbanisation of the area. History Originally this was an open stream that was one of the tributaries of the Waitemata River, now submerged by rising sea levels in the Waitematā Harbour. The Waihorotiu carved out the Queen Street valley millions of years ago. The upper part of that valley now forms Myers Park (Auckland), Myers Park. The references to a spring feeding the stream in the area of the Baptist Tabernacle in Myers Park are problematic (no historical document references this and if a spring existed it is unlikely it would have been built over). The stream ran through a swampy area (now Aotea Square), formed when lava flows from the Albert Park Volcano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato Regional Council
Waikato () is a local government region of the upper North Island of New Zealand. It covers the Waikato District, Waipa District, Matamata-Piako District, South Waikato District and Hamilton City, as well as Hauraki, Coromandel Peninsula, the northern King Country, much of the Taupō District, and parts of Rotorua District. It is governed by the Waikato Regional Council. The region stretches from Coromandel Peninsula in the north, to the north-eastern slopes of Mount Ruapehu in the south, and spans the North Island from the west coast, through the Waikato and Hauraki to Coromandel Peninsula on the east coast. Broadly, the extent of the region is the Waikato River catchment. Other major catchments are those of the Waihou, Piako, Awakino and Mokau rivers. The region is bounded by Auckland on the north, Bay of Plenty on the east, Hawke's Bay on the south-east, and Manawatū-Whanganui and Taranaki on the south. Waikato Region is the fourth largest region in the country in a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
State Highway 1 (New Zealand)
State Highway 1 (SH 1) is the longest and most significant road in the New Zealand road network, running the length of both main islands. It appears on road maps as SH 1 and on road signs as a white number 1 on a red shield, but it has the official designations SH 1N in the North Island, SH 1S in the South Island. SH 1 is long, in the North Island and in the South Island. Since 2010 new roads have reduced the length from . For the majority of its length it is a two-lane single carriageway, with at-grade intersections and property accesses, in both rural and urban areas. These sections have some passing lanes. Around of SH 1 is of motorway or expressway standard : in the North Island and in the South Island. Route North Island (SH 1N) SH 1 starts at Cape Reinga, at the northwestern tip of the Aupouri Peninsula, and since April 2010 has been sealed (mainly with either chipseal or asphalt) for its entire length. From Waitiki Landing south of Cape Reinga, SH 1 trav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikato
Waikato () is a Regions of New Zealand, local government region of the upper North Island of New Zealand. It covers the Waikato District, Waipa District, Matamata-Piako District, South Waikato District and Hamilton, New Zealand, Hamilton City, as well as Hauraki Plains, Hauraki, Coromandel Peninsula, the northern King Country, much of the Taupō District, and parts of Rotorua, Rotorua District. It is governed by the Waikato Regional Council. The region stretches from Coromandel Peninsula in the north, to the north-eastern slopes of Mount Ruapehu in the south, and spans the North Island from the west coast, through the Waikato and Hauraki to Coromandel Peninsula on the east coast. Broadly, the extent of the region is the Waikato River catchment. Other major catchments are those of the Waihou River, Waihou, Piako River, Piako, Awakino River (Waikato), Awakino and Mokau River, Mokau rivers. The region is bounded by Auckland Region, Auckland on the north, Bay of Plenty on the east ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taupō Volcano
Lake Taupō, in the centre of New Zealand's North Island, is the caldera of the Taupō Volcano, a large rhyolitic supervolcano. This huge volcano has produced two of the world's most violent eruptions in geologically recent times. ImageSize = width:320 height:800 PlotArea = right:50 top:10 left:50 bottom:10 DateFormat = yyyy TimeAxis = orientation:vertical order:reverse Period = from:-10000 till:2050 AlignBars = early ScaleMajor = unit:year increment:1000 start:-10000 Colors = id:canvas value:rgb(1,1,0.85) BackgroundColors = canvas:canvas PlotData = width:15 color:white bar:test from:-10000 till:1200 # Pre Maori PlotData = width:15 color:yellow bar:test from:1200 till:1840 # Pre accurate PlotData = width:15 color:orange bar:test from:1840 till:2050 # Accurate PlotData = at:-9999 shift:(30,0) text: Recent eruptions of Taupō caldera at:-9999 shift:(200,0) textcolor:red text: Eruptive at:-9850 shift:(80,-1) textcolor:red fontsize:S text:(Er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pumice
Pumice (), called pumicite in its powdered or dust form, is a volcanic rock that consists of highly vesicular rough-textured volcanic glass, which may or may not contain crystals. It is typically light-colored. Scoria is another vesicular volcanic rock that differs from pumice in having larger vesicles, thicker vesicle walls, and being dark colored and denser.Jackson, J.A., J. Mehl, and K. Neuendorf (2005) ''Glossary of Geology'' American Geological Institute, Alexandria, Virginia. 800 pp. McPhie, J., M. Doyle, and R. Allen (1993) ''Volcanic Textures A guide to the interpretation of textures in volcanic rocks'' Centre for Ore Deposit and Exploration Studies, University of Tasmania, Hobart, Tasmania..198 pp. Pumice is created when super-heated, highly pressurized rock is violently ejected from a volcano. The unusual foamy configuration of pumice happens because of simultaneous rapid cooling and rapid depressurization. The depressurization creates bubbles by lowering the solubi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pākehā
Pākehā (or Pakeha; ; ) is a Māori term for New Zealanders primarily of European descent. Pākehā is not a legal concept and has no definition under New Zealand law. The term can apply to fair-skinned persons, or to any non-Māori New Zealander. Papa'a has a similar meaning in Cook Islands Māori. Historically before the arrival of other ethnic groups the word Māori meant 'ordinary' or 'normal'. The arrival of Europeans led to the formation of a new term to distinguish the self-regarded 'ordinary' or 'normal' Māori from the new arrivals. The etymology of the word ''Pākehā'' remains unclear, but the term was in use by the late-18th century. In December 1814 the Māori children at Rangihoua in the Bay of Islands were "no less eager to see the ''packaha'' than the grown folks". In Māori, plural noun-phrases of the term include (the definite article) and (the indefinite article). When the word was first adopted into English, the usual plural was 'Pakehas'. However, spe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
