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Mount Cargill
Mount Cargill, known in Māori as Kapukataumahaka,Place names'' on Kāti Huirapa Runaka ki Puketeraki website, viewed 2012-01-04 is a volcanic outcrop which dominates the skyline of northern Dunedin, New Zealand. The peak is named for Captain William Cargill, an early leader of the Province of Otago. Māori legend tells of the mountain showing the profile of a prominent warrior, and indeed from Dunedin Buttar's Peak and Mount Cargill between them do form the outline of a reclining figure, with the nearby Buttar's Peak being the head and Mount Cargill the body. Panoramic views of Dunedin and its surrounding area are visible from the summit, making it a popular, if difficult to access, site. A single rough road ascends to the peak, and several popular walking tracks also ascend the slopes. Mount Cargill is topped by a telecommunications station and mast, the Mount Cargill Transmitting Station. The mast is Dunedin's tallest man-made structure. Geography Mt. Cargill is situate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Silverpeaks
The Silverpeaks (sometimes spelt Silver Peaks) is an area of rough forest and tussock and scrub covered hill country inland and to the northwest of Dunedin, New Zealand. The area is largely uninhabited; the main indication of human activity is the Taieri Gorge Railway, which preserves the route of the former Otago Central Railway that runs along the steep-sided valley of the Taieri River. Much of the area lies within the Silverpeaks Scenic Reserve. Background A network of walking tracks crisscross the area. From Pulpit Rock, trampers descend the Devil's Staircase into a lush valley just a short distance from Jubilee Hut. Access to these tracks is mainly via Double Hill Road, a rural road that leaves SH1 close to Waitati, and from several rural roads that leave SH87 between Outram and Middlemarch. Several of the peaks rise to above 600 metres. The highest points in the Silverpeaks include Silver Peak (753 m), known in Māori as Huatea,Place names'' on Kāti Huirapa Run ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waldronville
Waldronville is a coastal settlement on the Pacific Ocean coast of the South Island of New Zealand. Established in the 1950s as a commuter settlement, it is located to the southwest of Dunedin city centre, and lies within the city's limits. Waldronville was developed by Bill Waldron, when he purchased the McCraws farm in the early 1950s, initially for 200 houses. In the mid-1970s, two other streets were added to the southwest of the settlement. In the mid-1990s, Friendship Drive and Wavy Knowes developments were added to the northeast. The township of Brighton lies to the southwest of Waldronville; the tiny settlement of Westwood lies halfway between Brighton and Waldronville. Waldronville is located close to the Kaikorai Lagoon, an expanse of water at the mouth of the Kaikorai Stream protected from the ocean by a sandbar which stretches inland almost as far as the Dunedin suburb of Green Island, to the north. The lagoon is part of a research project aimed at establishing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plug
A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption. In a plinian eruption the plug is destroyed and ash is ejected. Glacial erosion can lead to exposure of the plug on one side, while a long slope of material remains on the opposite side. Such landforms are called crag and tail. If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive upstanding landform. Examples of volcanic plugs Africa Near the village of Rhumsiki in the Far North Province of Cameroon, Kapsiki Peak is an example of a volcanic plug and is one of the most photographed parts of the Mandara Mountains. Spectacular volcanic plugs are present in the center of La Gomer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyroclastic Cone
Volcanic cones are among the simplest volcanic landforms. They are built by ejecta from a volcanic vent, piling up around the vent in the shape of a cone with a central crater. Volcanic cones are of different types, depending upon the nature and size of the fragments ejected during the eruption. Types of volcanic cones include stratocones, spatter cones, tuff cones, and cinder cones. Stratocone Stratocones are large cone-shaped volcanoes made up of lava flows, explosively erupted pyroclastic rocks, and igneous intrusives that are typically centered around a cylindrical vent. Unlike shield volcanoes, they are characterized by a steep profile and periodic, often alternating, explosive eruptions and effusive eruptions. Some have collapsed craters called calderas. The central core of a stratocone is commonly dominated by a central core of intrusive rocks that range from around to over several kilometers in diameter. This central core is surrounded by multiple generations of lava f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyroclastic
Pyroclastic rocks (derived from the el, πῦρ, links=no, meaning fire; and , meaning broken) are clastic rocks composed of rock fragments produced and ejected by explosive volcanic eruptions. The individual rock fragments are known as pyroclasts. Pyroclastic rocks are a type of volcaniclastic deposit, which are deposits made predominantly of volcanic particles. 'Phreatic' pyroclastic deposits are a variety of pyroclastic rock that forms from volcanic steam explosions and they are entirely made of accidental clasts. 'Phreatomagmatic' pyroclastic deposits are formed from explosive interaction of magma with groundwater. Unconsolidated accumulations of pyroclasts are described as tephra. Tephra may become lithified to a pyroclastic rock by cementation or chemical reactions as the result of the passage of hot gases (fumarolic alteration) or groundwater (e.g. hydrothermal alteration and diagenesis) and burial, or, if it is emplaced at temperatures so hot that the soft glassy pyroc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Dome
In volcanology, a lava dome is a circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. Around 6% of eruptions on Earth are lava dome forming. The geochemistry of lava domes can vary from basalt (e.g. Semeru, 1946) to rhyolite (e.g. Chaiten, 2010) although the majority are of intermediate composition (such as Santiaguito, dacite-andesite, present day) The characteristic dome shape is attributed to high viscosity that prevents the lava from flowing very far. This high viscosity can be obtained in two ways: by high levels of silica in the magma, or by degassing of fluid magma. Since viscous basaltic and andesitic domes weather fast and easily break apart by further input of fluid lava, most of the preserved domes have high silica content and consist of rhyolite or dacite. Existence of lava domes has been suggested for some domed structures on the Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phonolite
Phonolite is an uncommon extrusive rock, of intermediate chemical composition between felsic and mafic, with texture ranging from aphanitic (fine-grained) to porphyritic (mixed fine- and coarse-grained). Phonolite is a variation of the igneous rock trachyte that contains nepheline or leucite rather than quartz. Its intrusive equivalent is nepheline syenite. Phonolite is typically fine grained and compact. The name ''phonolite'' comes from the Ancient Greek meaning "sounding stone" due to the metallic sound it produces if an unfractured plate is hit; hence, the English name ''clinkstone'' is given as a synonym. Formation Unusually, phonolite forms from magma with a relatively low silica content, generated by low degrees of partial melting (less than 10%) of highly aluminous rocks of the lower crust such as tonalite, monzonite and metamorphic rocks. Melting of such rocks to a very low degree promotes the liberation of aluminium, potassium, sodium and calcium by melting of f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nepheline
Nepheline, also called nephelite (), is a rock-forming mineral in the feldspathoid groupa silica-undersaturated aluminosilicate, Na3 K Al4 Si4 O16, that occurs in intrusive and volcanic rocks with low silica, and in their associated pegmatites. It is used in glass and ceramic manufacturing and other industries, and has been investigated as an ore of aluminium. Description and properties Nepheline crystals are rare and belong to the hexagonal system, usually having the form of a short, six-sided prism terminated by the basal plane. The crystals appear to have more symmetry than they actually possess, but unsymmetrical etched figures produced artificially on the prism faces indicate that the crystals are hemimorphic and tetartohedral, the only element of symmetry being a polar hexad axis. Nepheline is found in compact, granular aggregates, and can be white, yellow, gray, green, or reddish. Its hardness on the Mohs scale is 5.5–6, and its specific gravity 2.60–2.65. It i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunedin Volcano
The Dunedin Volcano is an extensively eroded multi-vent shield volcano that was active between 16 and 10 million years ago. It originally extended from the modern city of Dunedin, New Zealand to Aramoana about 25 km away. Extensive erosion has occurred over the last 10 million years and Otago Harbour now fills the oldest parts of the volcano. The remnants of the volcano form the hills around Otago Harbour (including Mount Cargill, Flagstaff, Saddle Hill, Signal Hill, and Otago Peninsula). Volcanism began in a shallow marine environment. The volcano became larger with flows of basalt and minor trachyte creating the bulk of the volcano. The final phase of eruptions are preserved as phonolite domes around Mount Cargill. Traces of the old Dunedin Volcano are best seen in the Dunedin Botanic Garden's geology walk, the cliffs at Aramoana and the geomorphology of Mount Cargill which has preserved lava domes. Basaltic columns are also to be found as prominent features above Second B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Peninsula
The Otago Peninsula ( mi, Muaūpoko) is a long, hilly indented finger of land that forms the easternmost part of Dunedin, New Zealand. Volcanic in origin, it forms one wall of the eroded valley that now forms Otago Harbour. The peninsula lies south-east of Otago Harbour and runs parallel to the mainland for 20 km, with a maximum width of 9 km. It is joined to the mainland at the south-west end by a narrow isthmus about 1.5 km wide. The suburbs of Dunedin encroach onto the western end of the peninsula, and seven townships and communities lie along the harbourside shore. The majority of the land is sparsely populated and occupied by steep open pasture. The peninsula is home to many species of wildlife, notably seabirds, pinnipeds, and penguins; several ecotourism businesses operate in the area. Geography The peninsula was formed at the same time as the hills facing it across the harbour, as part of the large, long-extinct, Dunedin Volcano. Several of the peninsula' ... [...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] |
Palmerston, New Zealand
The town of Palmerston, in New Zealand's South Island, lies 50 kilometres to the north of the city of Dunedin. It is the largest town in the Waihemo Ward of the Waitaki District, with a population of 890 residents. Palmerston grew at a major road junction: State Highway 1 links Dunedin and Waikouaiti to the south with Oamaru and Christchurch to the north, while State Highway 85 (known colloquially as "The Pigroot") heads inland to become the principal highway of the Maniototo. The Main South Line railway passes through the town and the Seasider tourist train travels from Dunedin to Palmerston and back once or twice a week. From 1880 until 1989, the town acted as the junction between the main line and a branch line that ran inland, the Dunback and Makareao Branches. Palmerston stands near the banks of the Shag River, five kilometres inland from the Pacific coast. Between it and the sea stands the lone hill of Puketapu (Māori for ''sacred hill'', known by Southerners as Holy Hil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
