|
Duntroon, Australian Capital Territory
Duntroon is a suburb of the city of Canberra in the Australian Capital Territory. History Robert Campbell's property Duntroon was situated on the limestone plains of New South Wales in the area that is now covered by the ACT. Given government compensation for the loss of his ship the while under government charter, Robert Campbell, sent James Ainslie to collect 700 sheep from the government flocks at Bathurst and to go southward looking for suitable pasture. Ainslie reached the Limestone Plains and selected a site on the slopes above the Molonglo River where the Royal Military College now stands. In 1825 Campbell applied for and received his grant, naming it "Duntroon" after the family castle, Duntrune Castle on Loch Crinan in Argyll, Scotland. Duntrune Castle on Loch Crinan in Argyll, Scotland was sold to clan Malcolm in 1792, long before this. In 1833, Campbell built "Duntroon House" out of stone with wide verandahs. In 1862 Robert's son George added a large two-sto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duntroon 1870 , also in Scotland
{{disambig ...
Duntroon may refer to: * Royal Military College, Duntroon, in Canberra, Australia * Duntroon, Australian Capital Territory, Robert Campbell's property in the suburb of Campbell, Canberra * Duntroon, Ontario, Canada * Duntroon, New Zealand * Duntroon, Scotland * MV ''Duntroon'', a passenger liner operated from 1935 to 1973, including wartime service as a troopship See also *Duntrune Castle Duntrune Castle is located on the north side of Loch Crinan and across from the village of Crinan in Argyll, Scotland. It is thought to be the oldest continuously occupied castle on mainland Scotland. The castle is a category B listed building. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scotland
Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast and east, and the Irish Sea to the south. It also contains more than 790 islands, principally in the archipelagos of the Hebrides and the Northern Isles. Most of the population, including the capital Edinburgh, is concentrated in the Central Belt—the plain between the Scottish Highlands and the Southern Uplands—in the Scottish Lowlands. Scotland is divided into 32 administrative subdivisions or local authorities, known as council areas. Glasgow City is the largest council area in terms of population, with Highland being the largest in terms of area. Limited self-governing power, covering matters such as education, social services and roads and transportation, is devolved from the Scott ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz. Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline volcanic rock, subalkaline tholeiite, tholeiitic and calc-alkaline magma series. Composition Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form rhyodacite, transitions to the rhyolites. The rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...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] |
Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Changi Chapel March 2013 2
Changi () is a planning area located in the geographical region of Tanah Merah in the East Region of Singapore. Sharing borders with Pasir Ris and Tampines to the west, Changi Bay to the southeast, the South China Sea to the east and the Serangoon Harbour to the north. Changi, excluding the two water catchments and islands of Singapore, is the largest planning area by land size. Today, Changi is an aviation hub. It is the location of both the Changi Airport and Changi Air Base. Also located within Changi is Singapore's largest prison, Changi Prison. It was used as a Japanese prisoner-of-war camp during the occupation of Singapore in World War II. The prison is Singapore's oldest operating internment facility, and is the location of Singapore's death row. Etymology The early Malay place name of Changi was Tanjong Rusa (English: Deer cape), as written in the 1604 Godinho de Eredia map of Singapore. The name Changi was known in the early 19th century. In the 1828 map by F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Changi Museum
The Changi Chapel and Museum is a war museum dedicated to Singapore's history during the Second World War and the Japanese occupation of Singapore. After the British army was defeated by the Imperial Japanese Army in the Battle of Singapore, thousands of prisoners-of-war (POWs) were imprisoned in Changi prison camp for three and a half years. While interned there, the POWs built numerous chapels, one of which was named St George's Church. History During the Japanese occupation of Singapore, there were a number of chapels built and rebuilt within and around the Changi Prison, where Allied prisoners of wars were interned. The Japanese did not restrict the POWs' religious activities, and thus the POWs converted existing buildings and utilised scrap materials to build altars and furniture. Among these chapels, the Roman Catholic Our Lady of Christians Chapel was dismantled after the war and moved to Australia, where it was reconstructed and unveiled in 1988 as part of the Prisoner ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horatio Kitchener, 1st Earl Kitchener
Horatio Herbert Kitchener, 1st Earl Kitchener, (; 24 June 1850 – 5 June 1916) was a senior British Army officer and colonial administrator. Kitchener came to prominence for his imperial campaigns, his scorched earth policy against the Boers, his expansion of Lord Roberts' concentration camps during the Second Boer War and his central role in the early part of the First World War. Kitchener was credited in 1898 for having won the Battle of Omdurman and securing control of the Sudan for which he was made Baron Kitchener of Khartoum. As Chief of Staff (1900–1902) in the Second Boer War he played a key role in Roberts' conquest of the Boer Republics, then succeeded Roberts as commander-in-chief – by which time Boer forces had taken to guerrilla fighting and British forces imprisoned Boer civilians in concentration camps. His term as Commander-in-Chief (1902–1909) of the Army in India saw him quarrel with another eminent proconsul, the Viceroy Lord Curzon, who eventua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duntrune Castle
Duntrune Castle is located on the north side of Loch Crinan and across from the village of Crinan in Argyll, Scotland. It is thought to be the oldest continuously occupied castle on mainland Scotland. The castle is a category B listed building. History It was originally built by the MacDougall clan in the 13th century, along with several other castles in the area, including the MacDougall stronghold of Dunollie Castle near Oban. Duntrune Castle was eventually taken by the Clan Campbell. In the 17th century the castle was besieged by the rival MacDonalds, under Alasdair Mac Colla. The Campbells sold Duntrune in 1792, to the Malcolms of Poltalloch. The castle is now owned by Robin Neill Malcolm, current clan chief of the Clan Malcolm. The curtain wall of the castle dates from the 13th century, although the tower house which forms the main part of the castle is of the 17th century. The castle was renovated in 1954. Popular culture The gateposts of Skyfall lodge, James Bond's ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
