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Granite Belt
The Granite Belt is an area of the Great Dividing Range in the Darling Downs region of Queensland and the New England region of New South Wales, Australia. The Granite Belt is centred on the town of Stanthorpe. The cool, high country of the granite belt is located on Queensland's southern border. It is the northernmost part of the New England Tablelands. The area gains its name from the predominantly granite rocks that distinguish it from other areas that make up much of South East Queensland. The Granite Belt is known for its spectacular flowers, and produces virtually all of Queensland's $40 million apple crop from one million trees grown by 55 orchardists. The area also lies within the Southern Downs region. Including the town of Warwick, the region has a population of 32,600 people. And is part of the Southern Downs Region local government area. The major river in the region is the Condamine River, a tributary of the Murray River. Climate The Granite Belt has a sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stanthorpe, Queensland
Stanthorpe is a rural town and locality in the Southern Downs Region, Queensland, Australia. In the , Stanthorpe had a population of 5,406 people. The area surrounding the town is known as the Granite Belt. Geography Stanthorpe lies on the New England Highway near the New South Wales border from Brisbane via Warwick, north of Tenterfield and 811 m above sea level. Stanthorpe was developed around Quart Pot Creek which meanders from south-east through the centre of town and then out through the south-west, where its confluence with Spring Creek forms the Severn River. Quart Pot Creek forms part of the south-western boundary of the locality, while the Severn River forms part of the south-western boundary. The New England Highway passes through the locality from Applethorpe in the north to Severnlea in the south. Originally it passed through the town centre along the main street, Maryland Street. However, it now bypasses to the west of the main developed area of the town ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Applethorpe, Queensland
Applethorpe is a rural town and locality in the Southern Downs Region, Queensland, Australia. In the the locality of Applethorpe had a population of 511 people. Applethorpe is on Queensland's border with New South Wales. It is well known for the production of apples. Geography The town is positioned on the New England Highway just north of Stanthorpe in the Granite Belt region at an elevation of . The Southern railway line passes through the locality from north ( The Summit & Glen Niven) to south (Stanthorpe). The town is served by the Applethorpe railway station. History The area was originally called ''Roessler'' after an early German settler, but the name was changed to Applethorpe (reflecting the apple orchards in the district) in 1915, as part of the anti-German sentiment during World War I. In 1910, the establishment of the Four Mile Stanthorpe School was given and the school was opened on 14 September 1911. However, from November 1911 to November 1916, it was ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dalveen, Queensland
Dalveen is a town and a locality in the Southern Downs Region, Queensland, Australia. It borders New South Wales. In the , Dalveen had a population of 335 people. Geography The town is located in the south of the locality. The New England Highway enters the locality from the north ( The Glen) and exits to the south ( Cottonvale); it bypasses the town just to the west. The Southern railway line enters the locality from the north-east (Silverwood) and passes through the town (being served by the Dalveen railway station ) and then exits to the south (Cottonvale). History The name ''Dalveen'' derives from locality name given by settler John Flint, who named it after Dalveen Pass in Lanark, Scotland. Stanthorpe Road Provisional School opened on 12 August 1878. In 1879 it was renamed North Maryland Provisional School. In 1892 it was renamed Dalveen State School on 18 January 1892. The section of the Southern railway line from Cherry Gully via Dalveen to Stanthorpe opened on 3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Batholith
A batholith () is a large mass of intrusive igneous rock (also called plutonic rock), larger than in area, that forms from cooled magma deep in Earth's crust. Batholiths are almost always made mostly of felsic or intermediate rock types, such as granite, quartz monzonite, or diorite (see also ''granite dome''). Formation Although they may appear uniform, batholiths are in fact structures with complex histories and compositions. They are composed of multiple masses, or ''plutons'', bodies of igneous rock of irregular dimensions (typically at least several kilometers) that can be distinguished from adjacent igneous rock by some combination of criteria including age, composition, texture, or mappable structures. Individual plutons are solidified from magma that traveled toward the surface from a zone of partial melting near the base of the Earth's crust. Traditionally, these plutons have been considered to form by ascent of relatively buoyant magma in large masses called ''p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adamellite
Quartz monzonite is an intrusive, felsic, igneous rock that has an approximately equal proportion of orthoclase and plagioclase feldspars. It is typically a light colored phaneritic (coarse-grained) to porphyritic granitic rock. The plagioclase is typically intermediate to sodic in composition, andesine to oligoclase. Quartz is present in significant amounts. Biotite and/or hornblende constitute the dark minerals. Because of its coloring, it is often confused with granite, but whereas granite contains more than 20% quartz, quartz monzonite is only 5–20% quartz. Rock with less than five percent quartz is classified as monzonite. A rock with more alkali feldspar is a syenite whereas one with more plagioclase is a quartz diorite.Classification of Igneous Rocks The fine grained |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pink Lady Apples, Thulimbah, Granite Belt, Queensland, 2015 02
Pink is the color of a namesake flower that is a pale tint of red. It was first used as a color name in the late 17th century. According to surveys in Europe and the United States, pink is the color most often associated with charm, politeness, sensitivity, tenderness, sweetness, childhood, femininity, and romance. A combination of pink and white is associated with chastity and innocence, whereas a combination of pink and black links to eroticism and seduction. In the 21st century, pink is seen as a symbol of femininity, though this has not always been true; in the 1920s, pink was seen as a color that reflected masculinity. In nature and culture File:Color icon pink v2.svg, Various shades of pink File:Dianthus.jpg, The color pink takes its name from the flowers called pinks, members of the genus ''Dianthus''. File:Rosa Queen Elizabeth1ZIXIETTE.jpg, In most European languages, pink is called ''rose'' or ''rosa'', after the rose flower. File:Cherry blossoms in the Tsu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wine Tourism
Enotourism, oenotourism, wine tourism, or vinitourism refers to tourism whose purpose is or includes the tasting, consumption or purchase of wine, often at or near the source. Where other types of tourism are often passive in nature, enotourism can consist of visits to wineries, tasting wines, vineyard walks, or even taking an active part in the harvest. History Enotourism is a relatively new form of tourism. Its history varies greatly from region to region, but in places such as the Napa Valley AVA and Wine Country, it saw heavy growth once a concerted marketing effort was implemented in 1975 that was given a further boost by the 1976 Judgment of Paris. Other regions, such as Catalonia, Spain have only started marketing enotourism starting in the mid-2000s, primarily focusing on how it is an alternative form of tourism to the beach for which Spain is overall known. There was also a rise in the profile of enotourism among English speakers with the 2004 release of the film, Sid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South East Queensland
South East Queensland (SEQ) is a bio-geographical, metropolitan, political and administrative region of the state of Queensland in Australia, with a population of approximately 3.8 million people out of the state's population of 5.1 million. The area covered by South East Queensland varies, depending on the definition of the region, though it tends to include Queensland's three largest cities: the capital city Brisbane; the Gold Coast; and the Sunshine Coast. Its most common use is for political purposes, and covers and incorporates 11 local government areas, extending from Noosa in the north to the Gold Coast and New South Wales border in the south (some sources include Tweed Heads, New South Wales which is contiguous as an urban area with Brisbane/Gold Coast), and west to Toowoomba (which is simultaneously considered part of the Darling Downs region). South East Queensland was the first part of Queensland to be settled and explored by Europeans. Settlements initially aro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rain And Snow Mixed
Rain and snow mixed is precipitation composed of a mixture of rain and partially melted snow. Unlike ice pellets, which are hard, and freezing rain, which is fluid until striking an object where it fully freezes, this precipitation is soft and translucent, but it contains some traces of ice crystals from partially fused snowflakes, also called slush. In any one location, it usually occurs briefly as a transition phase from rain to snow or vice versa, but hits the surface before fully transforming. Its METAR code is RASN or SNRA. Terminology This precipitation type is commonly known as sleet in most Commonwealth countries. However, the United States National Weather Service uses the term ''sleet'' to refer to ice pellets instead. In Ithaca, NY, the term Ithacating is used to describe precipitation made of a mix of rain and snow. Formation This precipitation occurs when the temperature in the lowest part of the atmosphere is slightly above the freezing point of water The dept ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frost
Frost is a thin layer of ice on a solid surface, which forms from water vapor in an above-freezing atmosphere coming in contact with a solid surface whose temperature is below freezing, and resulting in a phase change from water vapor (a gas) to ice (a solid) as the water vapor reaches the freezing point. In temperate climates, it most commonly appears on surfaces near the ground as fragile white crystals; in cold climates, it occurs in a greater variety of forms. The propagation of crystal formation occurs by the process of nucleation. The ice crystals of frost form as the result of fractal process development. The depth of frost crystals varies depending on the amount of time they have been accumulating, and the concentration of the water vapor (humidity). Frost crystals may be invisible (black), clear (translucent), or white; if a mass of frost crystals scatters light in all directions, the coating of frost appears white. Types of frost include crystalline frost (hoar fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_taken_from_Mt_Marlay_lookout%2C_Lock_Street_Stanthorpe_Queensland_Australia.jpg "Click for more on -> Stanthorpe, Queensland")
