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Gungahlin Town Centre
Gungahlin is a suburb in the Canberra, Australia district with the same name; Gungahlin. The postcode is 2912. Gungahlin is the name for the entire district, and also the town centre, but it is also the name of the suburb which Gungahlin Town Centre is in. It is next to the suburbs of Ngunnawal, Palmerston, Franklin, Harrison, Throsby, Forde and Amaroo. Burgmann Anglican School is located in the suburb. The edges of the suburb are on Horse Park Drive, Gundaroo Drive and Gungahlin Drive. Gungahlin Town Centre The commercial heart of the Gungahlin Town Centre is Hibberson St, the centre's main street, though the boundary of commercial activities in Anthony Rolfe Avenue, Gundaroo Drive and Gozzard Street. There are currently four retail anchor stores in the town centre, namely Coles, Woolworths, Aldi and Big W which are located in separate developments in Hibberson Street. There are two licensed clubs in the Town Centre: the Raiders Club located at the intersection of Hibberso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gungahlin
The District of Gungahlin () is one of the original eighteen districts of the Australian Capital Territory used in land administration. The Gungahlin Region is one of fastest growing regions within Australia. The district is subdivided into divisions ( suburbs), sections and blocks. ''Gungahlin'' is an Aboriginal word meaning either "white man's house" or "little rocky hill". Gungahlin comprised sixteen suburbs, including several currently under construction and a further suburb planned. The town of Gungahlin was part of the original 1957 plan for future development in the ACT and in 1991 was officially launched as Canberra's fourth 'town' by the ACT Chief Minister. At the time, the population of Gungahlin was just 389 residents. At the , the population of the district was 87,682. Within the district is Canberra's northernmost town centre that is situated north of Canberra city centre. The town centre is one of five satellites of Canberra, seated in Woden, Tuggeranong, Wes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gungahlin Town Centre
Gungahlin is a suburb in the Canberra, Australia district with the same name; Gungahlin. The postcode is 2912. Gungahlin is the name for the entire district, and also the town centre, but it is also the name of the suburb which Gungahlin Town Centre is in. It is next to the suburbs of Ngunnawal, Palmerston, Franklin, Harrison, Throsby, Forde and Amaroo. Burgmann Anglican School is located in the suburb. The edges of the suburb are on Horse Park Drive, Gundaroo Drive and Gungahlin Drive. Gungahlin Town Centre The commercial heart of the Gungahlin Town Centre is Hibberson St, the centre's main street, though the boundary of commercial activities in Anthony Rolfe Avenue, Gundaroo Drive and Gozzard Street. There are currently four retail anchor stores in the town centre, namely Coles, Woolworths, Aldi and Big W which are located in separate developments in Hibberson Street. There are two licensed clubs in the Town Centre: the Raiders Club located at the intersection of Hibberso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aranda, Australian Capital Territory
Aranda () is a suburb in the district of Belconnen, in the Australian capital city of Canberra. Located at the western foot of Black Mountain and bounded on two sides by nature park, the suburb is characterised by its bush setting. During the planning and development of the suburb, a large proportion of large native trees – predominantly eucalypts – were left in place. The suburb derives its name from the Arrernte tribe of Central Australia, previously known as ''Arunta'', which means 'White Cockatoo'. The streets in Aranda are named after Aboriginal tribal groups from around Australia. The suburb comprises an area of 160ha and in 1967 was the first suburb in Belconnen to be settled. A small plaque at the Aranda District playing fields near the suspension bridge over Belconnen Way marks the settlement of the suburb as the first development in the Belconnen district. It reads: Location Aranda is located in the south east of Belconnen. It is bounded by Caswell Drive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bruce, Australian Capital Territory
Bruce is a suburb of the Belconnen district of Canberra, that is located within the Australian Capital Territory, Australia. The suburb was gazetted on 6 June 1968 and named for The Viscount Bruce of Melbourne (1883–1967), the eighth Prime Minister of Australia and the first Chancellor of the Australian National University. Demographics At the , Bruce had a population of 7,520 people, an increase from 6,390 in 2011 and 3,012 in 2001. 58.1% of people were born in Australia. The next most common countries of birth were China (6.2%), India (4.9%), Nepal (3.5%), England (2.1%) and Vietnam (1.6%). 62.7% of people spoke only English at home. Other languages spoken at home included Mandarin (6.7%), Nepali (3.5%), Cantonese (2.0%) and Vietnamese (1.8%). The most common responses for religion were No Religion (44.1%) and Catholic (15.3%). 20.7% of dwellings were separate houses, 45.8% were semi-detached, row or terrace houses or townhouses and 33.4% of were units or apartments. Places ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaleen, Australian Capital Territory
Kaleen ( or ) is a suburb in the Belconnen district of Canberra, located within the Australian Capital Territory, Australia. The suburb's name means ‘water’ in the language of the Wiradjuri Aboriginal tribe of the central west region of New South Wales. Kaleen was gazetted as a suburb on 15 January 1974. The streets are named after Australian rivers. The suburb is next to Lyneham, Giralang, Lawson and Bruce. It is bordered by Baldwin Drive and Ginninderra Drive. It has several ovals; Kaleen North oval, Kaleen Enclosed oval, Kaleen District Playing Fields and Kaleen South oval, which play host to a number of sports, including soccer, cricket, and rugby. Unusually for a suburb, there are two small shopping centres in Kaleen, both bordering the main street of Maribyrnong Avenue. There is also a larger shopping centre near Kaleen's border with Giralang on Georgina Crescent. The 2XX transmitting station is also located in Kaleen, near the Barton Highway. On the east side of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crace, Australian Capital Territory
Crace () is a suburb of Canberra, Australia in the district of Gungahlin. It was named after Edward Kendall Crace an original settler in the Gungahlin area. Streets in Crace are named after parishes and land divisions from colonial times. It is bounded by the Barton Highway, Gundaroo Drive, Nudurr Drive and Gungahlin Drive. Located in the suburb is the Canberra Nature Park of Gungaderra Grasslands nature reserve. At the , it had a population of 4,459. History Development The suburb has finished development and construction. * Road construction commenced in July 2008. * The construction of 21 display homes was completed in May 2009. * By July 2012 more than half of the houses were complete. * The majority of homes were complete by 2015. The ACT government selected developers for the area as Defence Housing Australia and Canberra Investment Corporation. The developers were expected to make $60,000,000 but had to share half with the government. Some very small blocks were rele ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologic Fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syncline
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimposed smaller folds. Synclines are typically a downward fold (synform), termed a synformal syncline (i.e. a trough), but synclines that point upwards can be found when strata have been overturned and folded (an antiformal syncline). Characteristics On a geologic map, synclines are recognized as a sequence of rock layers, with the youngest at the fold's center or ''hinge'' and with a reverse sequence of the same rock layers on the opposite side of the hinge. If the fold pattern is circular or elongate, the structure is a basin. Folds typically form during crustal deformation as the result of compression that accompanies orogenic mountain building. Notable examples * Powder River Basin, Wyoming, US * Sideling Hill roadcut along Interstate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fold (geology)
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as ''fold trains''). Synsedimentary folds are those formed during sedimentary deposition. Folds form under varied conditions of stress, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (''fault bend fold''), at the tip of a propagating fault (''fault propagation fold''), by differential compaction or due to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashstone
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, W. H. Freeman, 2nd ed, 529 pp. The term ''mudstone'' is also used to describe carbonate rocks (limestone or dolomite) that are composed predominantly of carbonate mud. However, in most contexts, the term refers to siliciclastic mudstone, composed mostly of silicate minerals. The NASA Curiosity rover has found deposits of mudstone on Mars that contain organic substances such as propane, benzene and toluene. Definition There is not a single definition of mudstone that has gained general acceptance,Boggs 2006, p.143 though there is wide agreement that mudstones are fine-grained sedimentary rocks, composed mostly of silicate grains with a grain size less than . Individual grains this size are too small to be disting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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