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Stratigraphy Of New Zealand
This is a list of the geological unit, units into which the lithostratigraphy, rock succession of New Zealand is formally divided. As new geological relationships have been discovered new names have been proposed and others are made obsolete. Not all these changes have been universally adopted. This table is based on the 2014 New Zealand Stratigraphic Lexicon (Litho2014). However, obsolete names that are still in use and names postdating the lexicon are included if it aids in understanding. Names for particular rock units have two parts, a proper name which is almost always a geographic location where the rock is found and a hierarchical rank (e.g. Waitematā Harbour, Waitematā Group (stratigraphy), Group). This ranking system starts with individual 'beds' of rock which can be grouped into 'members', members are grouped into 'formations', formations into 'subgroups' then 'groups'. In New Zealand, groups are further combined into 'supergroups' or for basement rocks into terrane ...
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Cross Section New Zealand Geology
A cross is a religious symbol consisting of two Intersection (set theory), intersecting Line (geometry), lines, usually perpendicular to each other. The lines usually run vertically and horizontally. A cross of oblique lines, in the shape of the Latin letter X, is termed a saltire in heraldic terminology. The cross shape has been widely officially recognized as an absolute and exclusive religious symbol of Christianity from an early period in that religion's history.''Christianity: an introduction''
by Alister E. McGrath 2006 pages 321-323
Before then, it was used as a religious or cultural symbol throughout Europe, in West Asia, west and south Asia (the latter, in the form of the original Swastika); and in Ancient Egypt, where the Ankh was a hieroglyph that represented "life" and was used in the wo ...
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Petrified Wood
Petrified wood (from Ancient Greek meaning 'rock' or 'stone'; literally 'wood turned into stone'), is the name given to a special type of ''fossilized wood'', the fossilized remains of terrestrial plant, terrestrial vegetation. ''Petrifaction'' is the result of a tree or tree-like plants having been replaced by stone via a mineralization process that often includes permineralization and replacement. The Carbon-based life, organic materials making up cell walls have been replicated with minerals (mostly silica in the form of opal, chalcedony, or quartz). In some instances, the original structure of the stem tissue may be partially retained. Unlike other plant fossils, which are typically impressions or compressions, petrified wood is a three-dimensional representation of the original organic material. The petrifaction process occurs underground, when wood becomes buried in water or volcanic ash. The presence of water reduces the availability of oxygen which inhibits aerobic dec ...
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Curio Bay
Curio Bay is a coastal embayment in the Southland District of New Zealand, best known as the site of a petrified wood, petrified forest some 180 million years old. It also hosts a yellow-eyed penguin colony, arguably the rarest of penguin species, with approximately 1600 breeding pairs in the extant population. The bay, along with neighbouring Porpoise Bay (New Zealand), Porpoise Bay, is home to the endemic Hector's dolphin. Southern right whales are occasionally observed offshore, as on numerous parts of the country's coast. Located near the Slope Point, southernmost point of the South Island, Curio Bay is one of the major attractions in the Catlins, attracting around 100,000 visitors per year. The town of Waikawa, Southland, Waikawa has an information centre for tourists. The now petrified logs, from ancient conifers closely related to modern kauri and Norfolk pine, were buried by ancient volcanic mud flows and gradually replaced by silica to produce the fossils now exposed ...
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Cathedral Caves
The Cathedral Caves is a large V shaped limestone sea cave located on Waipati Beach, south of Papatowai, on the Catlins Coast in the southeast corner of New Zealand's South Island. The two main entrances join together within the cliff to form one big cave. One arm of the cave has a high ceiling. Often blue penguins will emerge from the gloom at the far end of the cave. And occasionally a sealion might be around. The 199m-long cave is formed in Jurassic sandstone (about 160 million years old) of the Murihiku Terrane, though the cave itself is much younger, ten to hundreds of thousands of years old. They were named by Thomas Hocken Thomas Morland Hocken (14 January 1836 – 17 May 1910) was a New Zealand collector, bibliographer and researcher. Early life He was born in Rutlandshire on 14 January 1836, the son of Wesleyan minister Joshua Hocken, and educated at Woodhouse ... who noted how the caves reverberated noise and their resemblance to European cathedrals. The cave ...
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Harwoods Hole
Harwoods Hole is a cave system located in the northwest of the South Island of New Zealand, in the Abel Tasman National Park. At , it is New Zealand's deepest vertical shaft. It was first explored in 1958, long after it was discovered. Formation Evidence suggests that run-off from an area of approximately 20 square km converged into a stream that then flowed down a dry valley to create what is now Harwoods Hole. Since then the river appears to have changed course. Subsequently, Harwoods Hole receives water through sinkholes and surrounding dry valleys; this water then percolates through surrounding rock ensuring it becomes saturated with calcite, before entering the cave where the calcite is deposited. This second phase means that rather than expanding, Harwoods Hole is being filled in. History It is one of several important cave systems in Tākaka Hill, between Golden Bay and Tasman Bay. Starting at the surface as a diameter entrance and descending , Harwoods Hole is New Z ...
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Tākaka Terrane
The Tākaka terrane is a Paleozoic terrane that outcrops in the South Island of New Zealand. It is most extensively exposed within the Kahurangi National Park in the Tasman District. The terrane is mostly made up of marble and volcanic rocks, but is highly variable in composition. It ranges in age from mid-Cambrian to Devonian time (510–400 Ma), including New Zealand's oldest rocks, which are found in the Cobb Valley in north-west Nelson. The Cobb Valley is also the location of "Trilobite Rock", a glacial dropstone made from the moulted exoskeletons of trilobites. Asbestos was mined in the Cobb Valley from the Tākaka Terrene between the late 1880s and 1917. The Tākaka terrane is highly deformed and has been intruded by many batholiths. Description The Tākaka terrane has two main igneous units, the arc-related Devil River Volcanics Group (Middle to Late Cambrian) and the rift‐related Gendarme Dolerite (latest Cambrian to Early Ordovician age). The Devil River Volcani ...
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Buller Terrane
Buller is an English surname. It may refer to: People * Anthony Buller (1613–1679), English soldier and Member of Parliament * Sir Anthony Buller (1780–1866), English lawyer and Member of Parliament * Arthur Henry Reginald Buller (1874–1944), British/Canadian mycologist * Charles Buller (1806–1848), English politician * David Buller (born 1959), American philosopher of science * Sir Edward Buller, 1st Baronet (1764–1824) * Ed Buller, British musician * Eric Buller (1894–1973), cricketer and British army officer * Francesca Buller (b. 1964), British actress * Francis Buller (Parliamentarian) English politician * Francis Buller (c 1630–1682), English politician * Sir Francis Buller, 1st Baronet (1746–1800) * Fred Buller (1914–1994), Canadian aeronautical engineer, sailboat designer * George Buller (MP) (1607–c. 1646), English politician * Sir George Buller (1802–1884), British Army General * Georgiana Buller (1884–1953), British hospital administr ...
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Brook Street Terrane
Brook may refer to: Computing *Brook, a programming language A programming language is a system of notation for writing computer programs. Programming languages are described in terms of their Syntax (programming languages), syntax (form) and semantics (computer science), semantics (meaning), usually def ... for GPU programming based on C *Brook+, an explicit data-parallel C compiler * BrookGPU, a framework for GPGPU programming People * Brook (surname) *People with the given name Brook, or nickname ** Brook Benton (1931–1988), American singer and songwriter ** Brook Hannah (1874–1961), Australian rules footballer and missionary ** Brook Mahealani Lee (born 1971), former Miss USA and Miss Universe (1997) from Hawaii, U.S. ** Brook Lopez, American basketball player ** Brook Taylor (1685–1731), English mathematician of Taylor series fame **Brook, a persona of Mary J. Blige **Brook, a fictional character in the manga and anime '' One Piece'' Places * Brook (hydrology ...
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Murihiku Terrane
Murihiku is a region of the South Island in New Zealand, as used by the Māori people. Traditionally it was used to describe the portion of the South Island below the Waitaki River, but now is mostly used to describe the province of Southland. The name means 'the tail end (of the land)' (literally , 'the end of'; , 'tail'). In 1861, when Southland became a province, the settler population wanted to retain the name "Murihiku", but this wish was ignored by Governor Thomas Gore Browne Colonel Sir Thomas Robert Gore Browne (3 July 1807 – 17 April 1887) was a British colonial administrator, who was Governor of St Helena, Governor of New Zealand, Governor of Tasmania and Governor of Bermuda. Early life Browne was born on .... This was "much to the inhabitants' indignation and disgust". References Further reading * Southland Region {{Maori-stub ...
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Dun Mountain–Maitai Terrane
The Dun Mountain–Maitai terrane comprises the Dun Mountain ophiolite belt (also called the mineral belt), Maitai group, and Patuki mélange. The Dun Mountain Ophiolite is an ophiolite of Permian age located in New Zealand's South Island. Prehistorically this ophiolite was quarried by Māori for both metasomatized argillite and pounamu (jade) which was used in the production of tools and jewellery. In the late 1800s, the Dun Mountain ophiolite belt was surveyed for its economic potential. During this time the rock types dunite and rodingite (after Dun Mountain and the Roding River) were first named. Discovery of economic deposits of chromite near Nelson lead to the building of New Zealand’s first railway, however, extraction only occurred between 1862 and 1866. In the 20th century, serpentinite was mined for fertiliser and the ophiolite remains one of New Zealand's main sources of pounamu (jade), but all other mineral exploration has failed to find economic deposits. Descr ...
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