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Stratigraphy Of New Zealand
This is a list of the units into which the 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 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 terranes. Not all of these hierarchical layers are necessarily present within a part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cross Section New Zealand Geology
A cross is a geometrical figure consisting of two intersecting lines or bars, 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 has been widely recognized as a symbol of Christianity from an early period.''Christianity: an introduction'' by Alister E. McGrath 2006 pages 321-323 However, the use of the cross as a religious symbol predates Christianity; in the ancient times it was a pagan religious symbol throughout Europe and western Asia. The effigy of a man hanging on a cross was set up in the fields to protect the crops. It often appeared in conjunction with the female-genital circle or oval, to signify the sacred marriage, as in Egyptian amule ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waipapa Composite Terrane
Waipapa is a small town in the Bay of Islands, Northland, New Zealand. It is around 10 minutes drive from Kerikeri, the nearest urban centre to Waipapa, located on State Highway 10. Waipapa itself has no school and most people travel into Kerikeri on a daily basis. It is governed by the Far North District council. Demographics Statistics New Zealand describes Waipapa as a rural settlement. It covers . The settlement is part of the larger Waipapa statistical area. Waipapa settlement had a population of 174 at the 2018 New Zealand census, an increase of 3 people (1.8%) since the 2013 census, and an increase of 45 people (34.9%) since the 2006 census. There were 51 households, comprising 81 males and 93 females, giving a sex ratio of 0.87 males per female. The median age was 28.1 years (compared with 37.4 years nationally), with 57 people (32.8%) aged under 15 years, 42 (24.1%) aged 15 to 29, 60 (34.5%) aged 30 to 64, and 21 (12.1%) aged 65 or older. Ethnicities were 65.5% E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Catlins
The Catlins (sometimes referred to as The Catlins Coast) comprises an area in the southeastern corner of the South Island of New Zealand. The area lies between Balclutha and Invercargill, straddling the boundary between the Otago and Southland regions. It includes the South Island's southernmost point, Slope Point. A rugged, sparsely populated area, the Catlins features a scenic coastal landscape and dense temperate rainforest, both of which harbour many endangered species of birds, most notably the rare yellow-eyed penguin. The coast attracts numerous marine mammals, among them New Zealand fur seals and Hooker's sea lions. In general terms the area enjoys a maritime temperate climate. Its exposed location leads to its frequently wild weather and heavy ocean swells, which are an attraction to big-wave surfers, and have also caused numerous shipwrecks. People have lived in the area since around 1350 AD. Prior to European settlement, the region was sparsely inhabited by nomadi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petrified Wood
Petrified wood, also known as petrified tree (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 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 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-saturated sediment or volcanic ash. The presence of water reduces the availability of oxygen which inhibits ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Curio Bay
Curio Bay is a coastal embayment in the Southland District of New Zealand, best known as the site of a 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, 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 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 has an information center 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 by the sea. The fossilised forest grew at a time of semi-tropical clima ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cathedral Caves
The Cathedral Caves are two connected limestone sea caves located on Waipati Beach, south of Papatowai, on the Catlins Coast in the southeast corner of New Zealand's South Island. The two main cave systems join together within the cliff and one has a high ceiling. Often blue penguins and fur seals will emerge from the gloom at the far end of the cave. 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 caves are only accessible for an hour either side of low tide. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harwood 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 / Te Tai-o-Aorere. Starting at the surface as a diameter entrance and descending , Har ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takaka Terrane
The Takaka 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 Takaka Terrene between the late 1880s and 1917. The Takaka Terrane is highly deformed and has been intruded by many batholiths. Description The Takaka 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 Volcanics Grou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 administrator * H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brook Street Terrane
A brook is a small river or natural stream of fresh water. It may also refer to: Computing *Brook, a programming language 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, Indiana, United States * Brook, Isle of Wight, England * Brook, Kent, England * Brook, Surrey, England * Brook, a hamlet in the parish of Albury, Surrey * Brook Islands, Australia * Brook House Immigration Re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Murihiku Terrane
The Southland Syncline is a major geological structure located in the Southland Region of New Zealand's South Island. The syncline folds the Mesozoic greywackes of the Murihiku Terrane. The northern limb of the fold is steep to overturned, while the southern limb dips shallowly to the northeast. The axial plan dips to the northeast and the axis plunges to the southeast. The Murihiku Terrane is formed predominantly from Permian to Jurassic sedimentary rocks with minor igneous intrusions, and is marked by prominent strike ridges particularly on its northern limb due to the steeper dip. These are created from the erosion of alternating strata of sandstone and mudstone. The northern edge of this fold system is marked by the Murihiku Escarpment, at the southern extreme of the Waimea Plains. Many of the names of stages and epochs in the Permian, Triassic, and Jurassic periods in the New Zealand geologic time scale are named for places within or close to the Southland Syncline and Murih ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
