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Acacia Bay
Acacia Bay is a community on a small inlet on the western shores of Tapuaeharuru Bay, Lake Taupō in New Zealand. There are four main beach areas. It is located approximately 2 miles west of Taupō. Demographics Acacia Bay covers and had an estimated population of as of with a population density of people per km2. Acacia Bay had a population of 1,653 at the 2018 New Zealand census, an increase of 228 people (16.0%) since the 2013 census, and an increase of 420 people (34.1%) since the 2006 census. There were 660 households, comprising 825 males and 825 females, giving a sex ratio of 1.0 males per female. The median age was 50.8 years (compared with 37.4 years nationally), with 264 people (16.0%) aged under 15 years, 180 (10.9%) aged 15 to 29, 783 (47.4%) aged 30 to 64, and 420 (25.4%) aged 65 or older. Ethnicities were 94.9% European/Pākehā, 9.8% Māori, 0.5% Pacific peoples, 1.8% Asian, and 1.8% other ethnicities. People may identify with more than one ethnicity. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taupō
Taupō (), sometimes written Taupo, is a town on the north-eastern shore of Lake Taupō, New Zealand's largest lake, in the central North Island. It is the largest urban area of the Taupō District, and the second-largest urban area in the Waikato, Waikato region, behind Hamilton, New Zealand, Hamilton. It has a population of Taupō was constituted as a borough in 1953. It has been the seat of Taupō District Council since the council was formed in 1989. Naming The name ''Taupō'' is from the Māori language and is a shortened version of ''Taupō-nui-a-Tia''. The longer name was first given to the cliff at Pākā Bay, on the eastern shore of the lake, and means the "great cloak of Tia". It was named for Tia (Māori explorer), Tia, the Māori explorer who discovered the lake. Māori later applied the name to the lake itself. In 2019 the official name of the town was changed from ''Taupo'' to ''Taupō''. Although the English pronunciation "tow-po" (, New Zealand English, NZE ) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Islam In New Zealand
Islam in New Zealand is a religious affiliation representing about 1.3% of the total population. Small numbers of Muslim immigrants from South Asia and eastern Europe settled in New Zealand from the early 1900s until the 1960s. Large-scale Muslim immigration began in the 1970s with the arrival of Fiji Indians, followed in the 1990s by refugees from various war-torn countries. The first Islamic centre in New Zealand opened in 1959 and there are now several mosques and two Islamic schools. The majority of Muslims in New Zealand are Sunni, with significant Shia and Ahmadiyya minorities. The Ahmadiyya Community has translated the Qur'an into the Māori language. History Early migration, 19th century The earliest Muslim presence in New Zealand dates back to the late 19th century. The first Muslims in New Zealand were an Indian family who settled in Cashmere, Christchurch, in the 1850s. The 1874 government census reported 15 Chinese Muslim gold diggers working in the Dunstan gold ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suburbs Of Taupō
A suburb (more broadly suburban area) is an area within a metropolitan area, which may include commercial and mixed-use, that is primarily a residential area. A suburb can exist either as part of a larger city/urban area or as a separate political entity. The name describes an area which is not as densely populated as an inner city, yet more densely populated than a rural area in the countryside. In many metropolitan areas, suburbs exist as separate residential communities within commuting distance of a city (cf "bedroom suburb".) Suburbs can have their own political or legal jurisdiction, especially in the United States, but this is not always the case, especially in the United Kingdom, where most suburbs are located within the administrative boundaries of cities. In most English-speaking countries, suburban areas are defined in contrast to central or inner city areas, but in Australian English and South African English, ''suburb'' has become largely synonymous with what i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taupō District
Taupō District is a territorial authority district in New Zealand. It covers 6,333 km² of land, and a further 610 km² of lake area, including Lake Taupō, New Zealand's largest lake, and Lake Rotoaira. The district stretches from the small town of Mangakino in the northwest to the Tongariro National Park in the south, and east into the Kaingaroa Forest. The district's population is largely located in the two main centres, Taupō and Tūrangi. Local government The district is governed by Taupō District Council. The vast majority of the district also falls within the jurisdiction of Waikato Regional Council, although parts are within the jurisdiction of the Bay of Plenty Regional Council and Manawatū-Whanganui Regional Council, and a tiny sliver is within the territory of the Hawke's Bay Regional Council. History Little is known about early Māori settlement near Taupō, although Ngāti Tūwharetoa have been the main iwi of the area for several hundred years. Major ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ignimbrite
Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ''ignimbrite'' from the Latin ''igni-'' [fire] and ''imbri-'' [rain]. Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when Lithification, lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli-tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oruanui Eruption
The Oruanui eruption of New Zealand's Taupō Volcano (also known as the Kawakawa eruption or Kawakawa/Oruanui event) was the world's most recent Supervolcano#Known supereruptions, supereruption.} Eruption With a Volcanic Explosivity Index of 8, it is one of the largest eruptions ever to occur in New Zealand. It occurred about 26,500 years ago in the Late Pleistocene and generated approximately of pyroclastic fall deposits, of pyroclastic density current (PDC) deposits (mostly ignimbrite) and of primary intracaldera material, equivalent to of magma, totaling of total deposits. The eruption is divided into 10 different phases on the basis of nine geological map, mappable fall strata, units and a tenth, poorly preserved but volumetrically dominant fall unit. Modern-day Lake Taupō, in area and deep, partly fills the caldera generated during this eruption. A structural collapse is concealed beneath Lake Taupō, while the lake outline at least partly reflects volcano-tectonic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hatepe Eruption
The Hatepe eruption, named for the Hatepe Plinian pumice tephra layer, sometimes referred to as the Taupō eruption or Horomatangi Reef Unit Y eruption, is dated to 232 CE ± 10 and was Taupō Volcano's most recent major eruption. It is thought to be New Zealand's largest eruption within the last 20,000 years. The eruption ejected some of material, of which just over was ejected in a few minutes. This makes it one of the largest eruptions in the last 5,000 years, comparable to the Minoan eruption in the 2nd millennium BCE, the 946 eruption of Paektu Mountain, the 1257 eruption of Mount Samalas, and the 1815 eruption of Mount Tambora. Stages of the eruption The eruption went through several stages, with six distinct marker horizons identified. Despite the uniform composition of the erupted magma, a wide variety of eruptive styles were displayed, including weak phreatomagmatism, Plinian eruptions, and a huge pyroclastic flow. Rhyolitic lava domes were extruded some ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whakamaru Caldera
The Whakamaru Caldera which was created in a massive eruption with a VEI of 8 is approximately in size and is located in the North Island of New Zealand. It now contains active geothermal areas as well as the later Maroa Caldera. Geography The Whakamaru Caldera covers an area larger than the younger Taupō Volcano to its south and indeed the rims overlap. To its north the more recent eruptive centres have sometimes been grouped as the Mokai Ring Complex or Maroa Volcanic Centre. It contains to its north east the more recently active Maroa Caldera with the Ben Lomond Dome being outside the southern border of the Maroa Caldera but definitely a feature of the Whakamaru Caldera. Domes within the caldera include the Western Dome Complex, including Pokuru which defines its north western borders (which likely overlap with those of the older Mangakino caldera complex), Forest Road Dome, Puketarata (which is the last Maroa Caldera eruption at 14,000 years ago), Ngangiho which is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent to granite. Rhyolitic magma is extremely viscous, due to its high silica content. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been extensively used for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil amendment. Description Rhyolite i ... [...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] |
Order Of The Golden Dawn
The Hermetic Order of the Golden Dawn ( la, Ordo Hermeticus Aurorae Aureae), more commonly the Golden Dawn (), was a secret society devoted to the study and practice of occult Hermeticism and metaphysics during the late 19th and early 20th centuries. Known as a magical order, the Hermetic Order of the Golden Dawn was active in Great Britain and focused its practices on theurgy and spiritual development. Many present-day concepts of ritual and magic that are at the centre of contemporary traditions, such as Wicca and Thelema, were inspired by the Golden Dawn, which became one of the largest single influences on 20th-century Western occultism. The three founders, William Robert Woodman, William Wynn Westcott and Samuel Liddell Mathers, were Freemasons. Westcott appears to have been the initial driving force behind the establishment of the Golden Dawn. The Golden Dawn system was based on hierarchy and initiation, similar to Masonic lodges; however, women were admitted on an equal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stella Matutina
The Stella Matutina (Morning Star) was an initiatory magical order dedicated to the dissemination of the traditional occult teachings of the earlier Hermetic Order of the Golden Dawn. Originally, the outer order of the Stella Matutina was known as ''Mystic Rose'' or ''Order of the M.R. in the Outer''.King, 1989, page 96 When occult writer Israel Regardie released documents of the Golden Dawn to the public it was the teachings of the Stella Matutina that he revealed, not those of the original order. The Stella Matutina was one of several daughter organisations into which the Hermetic Order of the Golden Dawn fragmented, including the Alpha et Omega led by John William Brodie-Innes and Macgregor Mathers, the Isis-Urania Temple led by A.E. Waite, and others. Origins After a revolt of London Adepts against the then-head of the Order ( Samuel MacGregor Mathers) in early 1900, the Order segmented into two new groups. Those who remained loyal to Mathers took on the name Alpha et Omega, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
