New Zealand Geologic Time Scale
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New Zealand Geologic Time Scale
While also using the international geologic time scale, many nations–especially those with isolated and therefore non-standard prehistories–use their own systems of dividing geologic time into epochs and faunal stages. In New Zealand, these epochs and stages use local place names (mainly Māori in origin) back to the Permian. Prior to this time, names mostly align to those in the Australian geologic time scale, and are not divided into epochs. In practice, these earlier terms are rarely used, as most New Zealand geology is of a more recent origin. In all cases, New Zealand uses the same periods as those used internationally; the renaming only applies to subdivisions of these periods. Very few epochs and stages cross international period boundaries, and the exceptions are almost all within the Cenozoic Era. New Zealand updates will always be behind any significant international updates in the International Geological Time Scale. Although the New Zealand geologic time scale h ...
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Geologic Time Scale
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define ...
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Annum
A year or annus is the orbital period of a planetary body, for example, the Earth, moving in its orbit around the Sun. Due to the Earth's axial tilt, the course of a year sees the passing of the seasons, marked by change in weather, the hours of daylight, and, consequently, vegetation and soil fertility. In temperate and subpolar regions around the planet, four seasons are generally recognized: spring, summer, autumn and winter. In tropical and subtropical regions, several geographical sectors do not present defined seasons; but in the seasonal tropics, the annual wet and dry seasons are recognized and tracked. A calendar year is an approximation of the number of days of the Earth's orbital period, as counted in a given calendar. The Gregorian calendar, or modern calendar, presents its calendar year to be either a common year of 365 days or a leap year of 366 days, as do the Julian calendars. For the Gregorian calendar, the average length of the calendar year (the mea ...
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Kumara, New Zealand
Kumara is a town on the West Coast of the South Island of New Zealand. It is located south of Greymouth, close to the western end of , which leads across Arthur's Pass to Christchurch. The Taramakau River flows past to the north. The population was 285 in the 2018 census, a decrease of 24 (7.76%) from 2013. The name may come from the Māori language Kohe mara, which is the blossom of the tātarāmoa, or bush lawyer. The Coast to Coast annual multisport race starts at Kumara Beach. History Kumara was founded and became one of the country's chief gold mining centres following the discovery of gold at Dillmanstown, about to the south-east, in 1876. The tramline from Greymouth to Paroa was extended to Kumara the following year. The population was 4,220 in October 1877. The town became a borough in 1877.Dollimore, Edward Stewart. "Kumara, Westland" - ''Encyclopedia of New Zealand (1966)''. Kumara Hospital was operating by 1881 and continued into the twentieth century. In 1 ...
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Taranaki
Taranaki is a region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano of Mount Taranaki, also known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is home to more than 65 per cent of the population of Taranaki. New Plymouth is in North Taranaki along with Inglewood and Waitara. South Taranaki towns include Hāwera, Stratford, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is the second highest mountain in the North Island, and the dominant geographical feature of the region. A Māori legend says that Mount Taranaki previously lived with the Tongariro, Ngaur ...
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Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ...
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Wairoa
Wairoa is a town and territorial authority district in New Zealand's North Island. The town is the northernmost in the Hawke's Bay region, and is located on the northern shore of Hawke Bay at the mouth of the Wairoa River and to the west of Māhia Peninsula. It is on State Highway 2, northeast of Napier, and southwest of Gisborne. Wairoa is the nearest town to the Te Urewera protected area and former national park that is accessible from Wairoa via State Highway 38. It is the largest town in the district of Wairoa, and is one of three towns in New Zealand where Māori outnumber other ethnicities, with 62.29% of the population identifying as Māori. History Early history Te Wairoa was originally a Māori settlement. The ancestral waka (canoe) Tākitimu travelled up the river and landed at Mākeakea, near where Tākitimu meeting house stands today. The Wairoa river (full name: Te Wairoa Hōpūpū Hōnengenenge Matangirau) was an important source of food as well as a t ...
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Waverley, Taranaki
Waverley is a town located in the South Taranaki District in New Zealand. It is 44 km northwest of Whanganui. Patea is 17 km to the west, and Waitōtara is 10 km to the southeast. State Highway 3 and the Marton - New Plymouth Line railway run through the town. History and culture Waverley was an important colonial stronghold during the New Zealand Wars of the 1860s, during which time the town was called Wairoa. The town is well known for its farming and thoroughbred stables. The race horse Kiwi was trained in the paddocks of a Waverley sheep farm by owner Snow Lupton and went on to go from last on the final bend to win the 1983 Melbourne Cup. Marae The local Te Wairoa-iti Marae and Maruata meeting house are a meeting place for Ngāti Tai, a hapū of Ngā Rauru Kītahi. Ironsand mining and renewable energy The Waipipi onshore ironsand mine operated near Waverley from 1971 to 1987, producing a total of 15.7 million tonnes of concentrate for export. The Waipip ...
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