|
Glen Eden
Glen Eden is a suburb of West Auckland, New Zealand, West Auckland, New Zealand, located at the foothills of the Waitākere Ranges. Originally known as Waikumete, the suburb gained the name Glen Eden in 1921. The suburb is in the Waitākere Ward, one of the thirteen administrative areas of Auckland governed by Auckland Council. Part of the rohe of Te Kawerau ā Maki, the area was developed into orchards during the Colony of New Zealand, Colonial era of New Zealand. The Glen Eden railway station opened in 1880, linking the area to central Auckland along the Western Line (Auckland), Western Line, and leading to the development of the Waikumete Cemetery. Suburban housing was built in the area in the 1950s and 1960s. Geography The Glen Eden area is located at the foothills of Waitākere Ranges, north of Titirangi. The Waikumete Stream flows north from Titirangi, forming a valley in the centre of the suburb. Glen Eden forms a part of the Waitematā-Waitākere foothills ecologic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Eden Playhouse Theatre
The Playhouse Theatre is a performing arts centre situated in Glen Eden, New Zealand. The building was constructed in 1937 following a fire that destroyed the Glen Eden Town Hall that was on the site at the time. The Theatre has continued to serve West Auckland, initially for civic and community functions and events, moving into cinema and theatre productions by the 1970s when the name of the building officially changed to The Playhouse Theatre. Various theatre groups that had used the venue eventually amalgamated as the Waitakere Playhouse Theatre Trust in 1997. After considerable fundraising, the building was upgraded and in 2003 reopened as a modern performing arts facility. History In 1901, at the site of the Glen Eden Playhouse Theatre, Glen Eden's first public hall was opened by local MP John Bollard. The social life of the Glen Eden community (then known as Waikumete) revolved around the hall, which was used to show films and hold town boards meetings, dances and po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitākere Ward
Waitākere is a locality name in West Auckland, New Zealand. It most commonly refers to: * Waitākere, Auckland, a rural town north-west of Auckland *Waitakere City, a former territorial authority which existed from 1989 to 2010 *Waitākere Ranges, a mountain range in West Auckland Waitākere may also refer to: *Waitakere City FC, a football club *Waitākere College, a school in Henderson, New Zealand *Waitakere (New Zealand electorate), a former parliamentary electorate * Waitakere railway station in Waitākere town *Waitākere Reservoir in the Waitākere Ranges *Waitākere River in the Waitākere Ranges *Waitākere volcano The Waitākere volcano, also known as the Manukau volcano, was a Miocene era volcano that formed off the west coast of the modern Auckland Region of New Zealand's North Island. Erupting intermittently between 23 million and 15 million years ago, ..., a former volcano in the Miocene era * Waitākere ward, a district of Auckland Council {{Disambig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), 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 followed the Oligocene and preceded 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 distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and Ape, hominoids into Eurasia. During the late Miocene, the conn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silver Fern
''Alsophila tricolor'', Synonym (taxonomy), synonym ''Cyathea dealbata'', commonly known as the silver fern or silver tree-fern, or as ponga or punga (from Māori language, Māori or ),The Māori word , pronounced , has been borrowed into New Zealand English as a generic term for tree ferns. It is also used to refer to tree fern logs when used for landscaping purposes. English speakers generally pronounce the word . is a species of medium-sized tree fern, endemism, endemic to New Zealand. The fern is usually recognisable by the silver-white colour of the under-surface of mature fronds. It is a symbol commonly associated with the country both overseas and by New Zealanders themselves. ''Alsophila tricolor'' is the correct name for ''Cyathea dealbata'' in ''Alsophila'' because the epithet ''dealbata'' is preoccupied by ''Alsophila dealbata'' C.Presl (now a synonym of ''Sphaeropteris glauca''). Description This fern is known to grow to heights of or more (though it occasional ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhopalostylis Sapida
''Rhopalostylis sapida'', commonly known as nīkau, is a palm tree endemic to New Zealand, and the only palm native to mainland New Zealand. Etymology is a word borrowed from the Māori language; cognates of this word in the closely related Eastern Polynesian languages of the tropical Pacific refer to the fronds or the midrib of the coconut palm (). Distribution The nīkau palm is the only palm species endemic to mainland New Zealand. Its natural range is coastal and lowland forest on the North Island, and on the South Island as far south as Ōkārito (43°20′S) in the west and Banks Peninsula (43°5′S) in the east. It also occurs on Chatham Island and Pitt Island/Rangiauria to the south-east of New Zealand, where it is the world's southernmost palm at 44° 18'S latitude.Esler, A. E. 'The Nikau Palm', ''New Zealand's Nature Heritage'', Vol.2 Part 19 p.532, 1974 Description Nīkau grow up to 15 m tall, with a stout, green trunk which bears grey-green leaf scars. The t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dacrydium Cupressinum
''Dacrydium cupressinum'', commonly known as rimu, is a species of tree in the family Podocarpaceae. It is a dioecious evergreen conifer, reaching heights of up to , and can have a stout trunk up to in diameter. It is endemic to New Zealand; its range covers the North, South, and Stewart Islands, and it typically inhabits lowland to montane forests. ''D. cupressinum'' has an estimated lifespan of 600–800 years, although it may live as long as 1,200 years. ''D. cupressinum'' grows in an erect (sometimes forked), and usually a monopodial manner. ''D. cupressinum'' is a tall species emerging above the main canopy, usually at about in height. ''D. cupressinum'' was first described in 1786 by Daniel Solander and was later given a full description in 1803 by Aylmer Lambert. ''D. cupressinum''s fruits are consumed by various birds such as: bellbirds, kererū, and the tūī. Its fruits also provide an important source of food and vitamins for the endemic flightless parrot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phyllocladus Trichomanoides
''Phyllocladus trichomanoides'', commonly known as the tānekaha or celery pine, is a Pinophyta, coniferous tree Endemism, endemic to New Zealand. Description Tānekaha is a medium-sized forest tree growing up to in height and 1 m trunk (botany), trunk diameter. The main structural shoots are green-skinned for 2–3 years, then turn brown as the bark thickens. The leaves are sparse, tiny, scale-like, 2–3 mm long, and only green (photosynthetic) for a short time, soon turning brown. Most photosynthesis is performed by phylloclades, highly modified, leaf-like short shoots; these are arranged alternately, 10–15 on a shoot, the individual phylloclades rhombic, 1.5–2–5 cm long. The seed conifer cone, cones are Berry (botany), berry-like, with a fleshy white aril surrounding but not fully enclosing the single seed. Distribution In the North Island, this species is found in lowland forests from Te Paki to 40°S. In the South Island, this species is found in nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Agathis Australis
''Agathis australis'', commonly known as kauri, is a species of coniferous tree in the family Araucariaceae, found north of 38°S in the northern regions of New Zealand's North Island. It is the largest (by volume) but not tallest species of tree in New Zealand, standing up to tall in the emergent layer above the forest's main canopy. The tree has smooth bark and small narrow leaves. Other common names to distinguish ''A. australis'' from other members of '' Agathis'' are southern kauri and New Zealand kauri. With its podsolization capability and regeneration pattern it can compete with faster growing angiosperms. Because it is such a conspicuous species, forest containing kauri is generally known as kauri forest, although kauri need not be the most abundant tree. In the warmer northern climate, kauri forests have a higher species richness than those found further south. Kauri even act as a foundation species that modify the soil under their canopy to create unique plan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasman Sea
The Tasman Sea is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about across and about from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known person to cross it. British explorer Lieutenant James Cook later extensively navigated the Tasman Sea in the 1770s during his three voyages of exploration. The Māori people of New Zealand call this sea ''Te Moana-a-Rehua'' meaning 'the sea of Rehua' which clashes with the Pacific waters named ''Te Tai-o-Whitirea'' ('the sea of Whitirea') – after Whitirea, Rehua's lover – at Cape Reinga, the northernmost tip of North Island. Climate The south of the sea is passed over by depressions going from west to east. The northern limit of these westerly winds is near to 40th parallel south, 40°S. During the southern winter, from April to October, the northern branch of these winds from the west changes its direction toward th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikumete Stream
The Waikumete Stream is a stream of the Auckland Region of New Zealand's North Island. It flows north from its sources in Titirangi, before joining the Oratia Stream. Both bodies are tributaries of Te Wai-o-Pareira / Henderson Creek, which flows into the western Waitematā Harbour. The stream passes through the suburbs of Titirangi, Kaurilands, Glen Eden and Sunnyvale, and since the mid-2000s has been forested with native flora. Description The stream begins north of Titirangi township, flowing north through the suburbs of Kaurilands and Glen Eden. At Glen Eden, the stream changes course, flowing north-west towards Parrs Park. The stream finishes its course at Millbrook Esplanade in the suburb of Sunnyvale, where it flows into the Oratia Stream. The stream has one tributary, the Hibernia Stream, which flows parallel to the Waikumete Stream to the west, flowing through Wirihana Park and Kowhai Reserve, meeting the Waikumete Stream at Ceramco Park. The stream is a habitat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikumete Cemetery
Waikumete Cemetery, originally Waikomiti Cemetery, is New Zealand's largest cemetery. It occupies a site of 108 hectares in Glen Eden, Auckland, and also contains a crematorium in the south-west corner of the cemetery. History Waikumete Cemetery was established in 1886 and is the final resting place for over 70,000 people. It was established after the Symonds Street Cemetery was surrounded by residential housing, and its location was decided by the proximity of the nearby Glen Eden railway station, as access by railway was desired. Passengers would travel to Waikumete on the same train as their loved ones in special train services held on Sundays. The funeral carriage was separated from passengers, and used a separate platform. The Chapel of Faith in the Oaks was built in 1886 as a mortuary chapel and was used until the larger chapel was built in 1952. The Chapel of Faith in the Oaks were shared between local Methodist, Anglican and Pentecostal communities for church services, un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Line (Auckland)
The Western Line in Auckland, New Zealand, is the name given to suburban rail services that operate between Britomart and Swanson via Newmarket. Routing From Waitematā to Newmarket, Western Line services travel on the Newmarket Line, then follow the North Auckland Line to Swanson, the current northernmost station on the network. The Western and Eastern Lines will be merged into the East-West Line once the City Rail Link project is finished, with an additional service travelling on the former Western Line and then joining the Onehunga line bound for Onehunga. History In 1877, New Zealand Railways called for tenders for the construction of a railway between Newmarket and Waikomiti (the former name of Glen Eden). Larkins and O'Brien were contracted to construct the rail line and a tunnel cutting through Scroggy Hill (located at modern-day Pleasant Road, West Coast Road and Rua Road). Locals in the area opposed the construction of a tunnel, leading to the railway being co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
