|
Kaihere
Kaihere is a dispersed Waikato rural settlement on SH27, overlooking the Hauraki Plains. It has a school, hall, domain a rest area and is the starting point for the Hapuakohe Walkway. Demographics Kaihere's meshblock (1069500 includes the school and most houses) had these census results - Geology The village lies on the edge of greywacke, of the Jurassic Manaia Hill Group, and the peat of the Hauraki graben. Much of the village is built on the Pliocene Puketoka formation between those. That formation has boulders of andesite, quartz vein-stone, cryptocrystalline silica, and banded rhyolite, with cobbles of greywacke, in a poorly cemented bed of pumice silt. The Hauraki rift probably started about 3 million years ago. Subsidence now is about a year. History The early inhabitants largely used the wetlands for fishing. Ngāti Hako and Ngāti Pāoa lived in the area when early settlers arrived. The Musket Wars caused much disruption in the 1820s. Government gradually ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hauraki Plains
The Hauraki Plains are a geographical feature and non-administrative area (though Hauraki Plains County Council existed from 1920 to 1989 and a statistical Area Unit remains) located in the northern North Island of New Zealand, at the lower (northern) end of the Thames Valley. They are located 75 kilometres south-east of Auckland, at the foot of the Coromandel Peninsula and occupy the southern portion of a rift valley bounded on the north-west by the Hunua Ranges, to the east by the Coromandel and Kaimai ranges and the west by a series of undulating hills which separate the plains from the much larger plains of the Waikato River. Broadly, the northern and southern parts of the Hauraki Plains are administered by the Hauraki District and the Matamata-Piako District respectively. The alluvial plains have been built up by sediment deposited by the Piako and Waihou rivers, which flow north to reach the sea at the Firth of Thames, and earlier by the ancestral Waikato River. The r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piako River
The Piako River is a lowland river system that drains into the Firth of Thames on the North Island of New Zealand. Together with the Waihou River, it is one of the two main rivers systems which drains the Hauraki Plains. It is the dominant river system in the Matamata-Piako District, and on its journey it passes through the towns of Morrinsville and Ngatea. The Piako River has an annual mean flow of (at Paeroa-Tahuna Road), with a total catchment area of approximately . The river system is approximately long, aligned in a north-south direction and occupies much of the central and western Hauraki Plains (or more broadly, the Thames Valley), extending from Hinuera in the south before discharging into the Firth of Thames in the north, five kilometres west of Thames. The Piako River has two major stems: the first, and main, stem drains the northern Te Miro-Tahuroa hills, and the Pakaroa Range. The dominant tributaries on the eastern slopes of these hills are the Piakonui and Piako ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hauraki District
Hauraki District is a territorial authority within the Hauraki region of New Zealand. The seat of the council is at Paeroa. The area covered by the district extends from the southwest coast of the Firth of Thames southeast towards Te Aroha, although that town lies beyond its boundaries. It extends eastwards to the Bay of Plenty coast, taking in the southernmost part of the Coromandel Peninsula. The rest of the peninsula is part of Thames-Coromandel District. Features of the district include the Karangahake Gorge, Whiritoa, the Hauraki Plains, Ngatea and the gold mining town of Waihi. Demographics Hauraki District covers and had an estimated population of as of with a population density of people per km2. live in Paeroa and in Waihi. Hauraki District had a population of 20,022 at the 2018 New Zealand census, an increase of 2,214 people (12.4%) since the 2013 census, and an increase of 2,166 people (12.1%) since the 2006 census. There were 7,869 households, comprising 9,8 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand State Highway 27
State Highway 27 (SH 27) is a state highway in the Waikato region of the North Island of New Zealand. It is an important north–south link along the Waihou/ Piako valley and forms an important transport route across the mostly dairy farming Matamata-Piako District. SH 27, in conjunction with , is often used as an alternative route to between Auckland and Tauranga, Rotorua and Taupō. For its entire length, SH 27 is a single carriageway road with one lane in each direction and at-grade intersections and property access. The New Zealand Transport Agency classifies the highway as an arterial route. Traffic at Kaihere increased by 31%, from an average of 3,965 vehicles a day in 2008, to 5,182 in 2017 and 5,467 in 2019. In 2017 982 (19%) of those were heavy vehicles, mainly trucks. The road was gravelled and classified as No.19 Main Highway in 1926. Major junctions See also *List of New Zealand state highways *List of roads and highways List of articles rela ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hapuakohe Range
Hapuakohe Range of hills is aligned north-south, between the Waikato River and the Hauraki Plains in the Waikato region of New Zealand. It is separated from the Taupiri Range by an air-gap at Mangawara, where the Waikato flowed about 20,000 years ago. The range is drained by the Waitakaruru and Whangamarino Rivers and their tributaries at the north end. Further south, tributaries of the Piako River drain the east side of the range and streams flow to the Waikato on the west. The 1865 confiscation boundary ran along the range. The boundary between Waikato and Ohinemuri (from 1920 Hauraki Plains) counties followed a similar line, as does the current boundary between Waikato, Hauraki and Matamata Piako Districts. Named summits and road From north to south, the features named on the LINZ map are: * Pukekamaka * Okaeria * Karamuroa * Otane * Ikeike - west of main ridge – a low priority walkway plan may link them. * Matahuru Rd - in 2007 the lower part of the road ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1915 Patetonga And Kaihere Plans And Notice Of Auction
Events Below, the events of World War I have the "WWI" prefix. January *January – British physicist Sir Joseph Larmor publishes his observations on "The Influence of Local Atmospheric Cooling on Astronomical Refraction". *January 1 ** WWI: British Royal Navy battleship HMS ''Formidable'' is sunk off Lyme Regis, Dorset, England, by an Imperial German Navy U-boat, with the loss of 547 crew. **Battle of Broken Hill: A train ambush near Broken Hill, New South Wales, Australia, is carried out by two men (claiming to be in support of the Ottoman Empire) who are killed, together with 4 civilians. * January 5 – Joseph E. Carberry sets an altitude record of , carrying Capt. Benjamin Delahauf Foulois as a passenger, in a fixed-wing aircraft. * January 12 ** The United States House of Representatives rejects a proposal to give women the right to vote. ** ''A Fool There Was'' premières in the United States, starring Theda Bara as a ''femme fatale''; she quickly becomes one of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cementation (geology)
Cementation involves ions carried in groundwater chemically precipitating to form new crystalline material between sedimentary grains. The new pore-filling minerals forms "bridges" between original sediment grains, thereby binding them together. In this way, ''sand'' becomes sandstone, and ''gravel'' becomes conglomerate or breccia. Cementation occurs as part of the diagenesis or lithification of sediments. Cementation occurs primarily below the water table regardless of sedimentary grain sizes present. Large volumes of pore water must pass through sediment pores for new mineral cements to crystallize and so millions of years are generally required to complete the cementation process. Common mineral cements include calcite, quartz, and silica phases like cristobalite, iron oxides, and clay minerals; other mineral cements also occur. Cementation is continuous in the groundwater zone, so much so that the term "zone of cementation" is sometimes used interchangeably. Cementati ... [...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] |
Silt
Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz. Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt also can be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles). Silt is a common material, making up 45% of average modern mud. It is found in many river deltas and as wind-deposited accumulations, particularly in central Asia, north China, and North America. It is produced in both very hot climates (through such processes as collisions of quartz grains in dust storms) and very cold climates (through such processes as glacial grinding of quartz grains.) Loess is soil rich in silt which makes up some of the most fertile agricultural land on Earth. However, silt is very vulnerable to erosion, and it has poor mechanical properties, making construction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the poi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Settler
A settler is a person who has human migration, migrated to an area and established a permanent residence there, often to colonize the area. A settler who migrates to an area previously uninhabited or sparsely inhabited may be described as a pioneer. Settlers are generally from a Sedentism, sedentary culture, as opposed to nomads, nomadic peoples who may move settlements seasonally, within traditional territories. Settlement sometimes relies on dispossession of already established populations within the contested area, and can be a very violent process. Sometimes settlers are backed by governments or large countries. Settlements can prevent native people from continuing their work. Historical usage One can witness how settlers very often occupied land previously residents to long-established peoples, designated as Indigenous peoples, Indigenous (also called "natives", "Aborigines" or, in the Americas, "Indians"). The process by which Indigenous territories are settled by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Hako
Ngāti Hako is a Māori iwi of New Zealand. The people of Ngati Hako are acknowledged as the earliest settlers in the Hauraki region. Although Ngati Hako endured long periods of conflict with the Marutūāhu peoples, they were never completely overcome. They have maintained a presence in Hauraki to the present day. Their origins are not known, but it is suggested that they belonged to the ancient Te Tini o Toi people, who were descendants of the Polynesian navigator Toitehuatahi. The survival of Ngati Hako through the period of Marutūāhu expansion was assisted by a strategic marriage. The high-born Ngati Hako woman Ruawehea was married to Tamatera, the son of Marutūāhu. The special relationship between Ngati Hako and the lands of Hauraki is recalled in their traditional call of welcome. See also *List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
