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Glass House Mountains (Queensland)
The Glass House Mountains are a cluster of thirteen hills that rise abruptly from the coastal plain on the Sunshine Coast, Queensland, Australia. The highest hill is Mount Beerwah at 556 metres above sea level, but the most identifiable of all the hills is Mount Tibrogargan which from certain angles bears a resemblance to a gorilla facing east towards the ocean. The Glass House Mountains are located near Beerburrum State Forest and Steve Irwin Way. From Brisbane, the mountains can be reached by following the Bruce Highway north and taking the Glass House Mountains tourist drive turn-off onto Steve Irwin Way. The trip is about one hour from Brisbane. The Volcanic peaks of the Glass House Mountains rise dramatically from the surrounding Sunshine Coast landscape. They were formed by intrusive plugs, remnants of volcanic activity that occurred 26–27 million years ago. Molten rock filled small vents or intruded as bodies beneath the surface and solidified into land rocks. Million ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glass House Mountains, Queensland
Glass House Mountains is a rural hinterland town and Suburbs and localities (Australia), locality in the Sunshine Coast Region, Queensland, Australia. In the , the locality of Glass House Mountains had a population of 5,601 people. Geography The town also has a Glasshouse Mountains railway station, Queensland, train station and a North Coast railway line, Queensland, railway line that runs northwards towards Northern Queensland and southwards to Brisbane. The Bruce Highway runs along the locality's eastern border. Glass House Mountains Road (Steve Irwin Way) passes through from south to north. History Land around the Glass House Mountains railway station was auctioned by the Queensland Government on Wednesday 28 October 1903. Most of the lots were about intended for pineapple farms. The land was in the vicinity of the present-day town centre with Saraha Road, Buzaki Road, and Coonowrin Road shown (but unnamed) on the map provided. The district was referred to as Beerwah as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glass House Sunset View
Glass is an amorphous ( non-crystalline) solid. Because it is often transparent and chemically inert, glass has found widespread practical, technological, and decorative use in window panes, tableware, and optics. Some common objects made of glass are named after the material, e.g., a "glass" for drinking, "glasses" for vision correction, and a "magnifying glass". Glass is most often formed by rapid cooling (quenching) of the molten form. Some glasses such as volcanic glass are naturally occurring, and obsidian has been used to make arrowheads and knives since the Stone Age. Archaeological evidence suggests glassmaking dates back to at least 3600 BC in Mesopotamia, Egypt, or Syria. The earliest known glass objects were beads, perhaps created accidentally during metalworking or the production of faience, which is a form of pottery using lead glazes. Due to its ease of formability into any shape, glass has been traditionally used for vessels, such as bowls, vases, bottles, j ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bora (Australian)
Bora is an initiation ceremony of the Aboriginal people of Eastern Australia. The word "bora" also refers to the site on which the initiation is performed. At such a site, boys, having reached puberty, achieve the status of men. The initiation ceremony differs from Aboriginal culture to culture, but often, at a physical level, involved scarification, circumcision, subincision and, in some regions, also the removal of a tooth. During the rites, the youths who were to be initiated were taught traditional sacred songs, the secrets of the tribe's religious visions, dances, and traditional lore. Many different clans would assemble to participate in an initiation ceremony. Women and children were not permitted to be present at the sacred bora ground where these rituals were undertaken. Bora terminology The word ''Bora'' was originally taken from the Gamilaraay language spoken by the Kamilaroi people who lived in the region north of the Hunter Valley in New South Wales to souther ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gubbi Gubbi
The Kabi Kabi people, also spelt Gubbi Gubbi, Gabi Gabi, and other variants, are an Aboriginal Australian people native to South Eastern Queensland. During the Australian frontier wars of the 19th century, there were several mass killings of Kabi Kabi people by settlers. They are now classified as one of several Murri language groups in Queensland. A 2024 determination granted non-exclusive native title rights over an area of land and waters on the Sunshine Coast. Naming As is often the case, ethnonyms distinguishing one tribe from another select the word used by any one group for the concept "no", which is the meaning of ''kabi/gubi/gabi''. However, AIATSIS's Austlang database prefers Gubbi Gubbi. The name ''Gubbi Gubbi'', as shown in early history books, has been used in recent times interchangeably with ''Kabi Kabi''. AIATSIS favours ''Gubbi Gubbi'' as for the language, but also gives other spellings and name variants. but in recent publications has referred to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Traditional Owners
Native title is the set of rights, recognised by Australian law, held by Aboriginal and Torres Strait Islander groups or individuals to land that derive from their maintenance of their traditional laws and customs. These Aboriginal title rights were first recognised as a part of Australian common law with the decision of '' Mabo v Queensland (No 2)'' in 1992. The doctrine was subsequently implemented and modified via statute with the '' Native Title Act 1993''. The concept recognises that in certain cases there was and is a continued beneficial legal interest in land held by Indigenous peoples which survived the acquisition of radical title and sovereignty to the land by the Crown. Native title can co-exist with non-Aboriginal proprietary rights and in some cases different Aboriginal groups can exercise their native title rights over the same land. The Federal Court of Australia arranges mediation in relation to claims made by Aboriginal and Torres Strait Islander peoples, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glass House Mountains National Park
Glass House Mountains National Park is a heritage-listed national park at Glass House Mountains, Queensland, Glass House Mountains, Sunshine Coast Region, Queensland, Australia. It is also known as Beerburrum Forest Reserve 1. It is north of Brisbane and consists of a flat plain punctuated by rhyolite and trachyte volcanic plugs, the cores of extinct volcanoes that formed 26 million to 27 million years ago. The mountains would once have had pyroclastic rock, pyroclastic exteriors, but these have eroded away. The national park was established in 1994. On 23 June 2010 the Queensland Government announced the expansion of the park to include an additional . It was added to the Queensland Heritage Register on 3 May 2007. Facilities Camp grounds are available at Glass House Mountains township and Coochin Creek, west of Beerwah, Queensland, Beerwah. Lookouts have been built at several of the summits. Walking tracks allow access to the summits of Mount Beerwah, Mount Tibroga ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glass House Mountains
The Glass House Mountains are a cluster of thirteen hills that rise abruptly from the coastal plain on the Sunshine Coast, Queensland, Sunshine Coast, Queensland, Australia. The highest hill is Mount Beerwah at 556 metres above sea level, but the most identifiable of all the hills is Mount Tibrogargan which from certain angles bears a resemblance to a gorilla facing east towards the ocean. The Glass House Mountains are located near Beerburrum State Forest and Steve Irwin Way. From Brisbane, the mountains can be reached by following the Bruce Highway north and taking the Glass House Mountains tourist drive turn-off onto Steve Irwin Way. The trip is about one hour from Brisbane. The Volcanic peaks of the Glass House Mountains rise dramatically from the surrounding Sunshine Coast landscape. They were formed by intrusive plugs, remnants of volcanic activity that occurred 26–27 million years ago. Molten rock filled small vents or intruded as bodies beneath the surface and solidified ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subvolcanic Rock
A subvolcanic rock, also known as a hypabyssal rock, is an intrusive igneous rock that is emplaced at depths less than within the crust, and has intermediate grain size and often porphyritic texture between that of volcanic rocks, which are extrusive igneous rocks, and plutonic rocks, which form much deeper in the ground. Subvolcanic rocks include diabase (also known as dolerite) and porphyry. Common examples of subvolcanic rocks are diabase, quartz dolerite, microgranite, and diorite. See also * Cone sheet * Dike (geology) * Igneous intrusion In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and com ... * Sill (geology) References Igneous petrology Volcanology {{igneous-petrology-stub he:סלע געשי#סלעים תת-געשיים ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fracture (geology)
A fracture is any separation in a geologic formation, such as a Joint (geology), ''joint'' or a Fault (geology), ''fault'' that divides the Rock (geology), rock into two or more pieces. A fracture will sometimes form a deep fissure or crevice in the rock. Fractures are commonly caused by Stress (physics), stress exceeding the rock strength, causing the rock to lose cohesion along its weakest plane. Fractures can provide Permeability (fluid), permeability for fluid movement, such as water or hydrocarbons. Highly fractured rocks can make good aquifers or Oil reservoir, hydrocarbon reservoirs, since they may possess both significant Permeability (fluid), permeability and fracture porosity. Brittle deformation Fractures are forms of brittle deformation. There are two types of primary brittle deformation processes. Tensile fracturing results in ''joints''. ''Shear fractures'' are the first initial breaks resulting from shear forces exceeding the cohesive strength in that plane. Aft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plug
A volcanic plug, also called a volcanic neck or lava neck, is a volcano, volcanic object created when magma hardens within a Volcanic vent, vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising Volatile (astrogeology)#Igneous petrology, 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. Glaciation, 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 Region (Cameroon), Far North Province of Cameroon, Kapsiki Peak is an example of a volcanic plug and is one of the most phot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Comendite
Comendite is a hard, peralkaline igneous rock, a type of light blue grey rhyolite. Phenocrysts are sodic sanidine with minor albite and bipyramidal quartz. Iddings, Joseph Paxson, 1913, ''Igneous rocks: composition, texture and classification'', v. 2, pp. 94-96 The blue colour is caused by very small crystals of riebeckite or arfvedsonite. The 1903 eruption of Baekdu Mountain, Changbaishan volcano in northeast China erupted comendite pumice. Comendite derives its name from the area of Le Commende on San Pietro Island in Italy, where the rock type is found.Cioni, R. and Funedda, A., (2005) ''Structural geology of crystal-rich, silicic lava flows: A case study from San Pietro Island (Sardinia, Italy)'' in Manga, M. and Ventura, G. (editors) (2005) ''Kinematics and Dynamics of Lava Flows'', Geological Society of America Special Paper 396, pages 1 to 14. Comendite also occurs in the Glass House Mountains of southeast Queensland, Australia, as well as in Sardinia, Corsica, Ascension Is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
