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Blackall Ranges
The Blackall Range is a mountain range in South East Queensland, Australia. The first European explorer in the area was Ludwig Leichhardt. It was named after Samuel Blackall, the second Governor of Queensland. The Blackall Range dominates the hinterland area of the Sunshine Coast, west of Nambour. Maleny, Mapleton, Montville and Flaxton are the main settlements located on the range. The Stanley River rises from the southern slopes. Baroon Pocket Dam is a reservoir on Obi Obi Creek which drains the north west slopes of the range. Mary Cairncross Reserve marks the site of the first settler's house on the Blackall Range. Curramore Sanctuary, Mapleton Falls National Park and Kondalilla National Park are also located on the range. A number of lookouts on the range provide views towards the coast. One of these is located at Howells Knob, a mountain which rises 561 m above sea level. Timber resources in the area attracted timber-cutters in 1860s. The last logging on the range o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mary Cairncross Reserve
The Mary Cairncross Reserve is a conservation park located on the Blackall Range east of Maleny, in the Sunshine Coast Region, Queensland, Australia. Maleny is approximately north of Brisbane and west of Caloundra. The reserve is positioned in the mountain rainforests of the Maleny region overlooking the Glass House Mountains. Geology The Region holds many of the large predominate landforms in Queensland, the most recognisable is the Glass House Mountains. The Glass House Mountains were formed thousands of years ago when the outer layer of soil and rock eroded from the extinct volcanic summit. The dirt and soil located in the region is very rich and healthy, due to the high quantity of volcanic rock decomposed in the soil. Volcanic rock contains high amounts of nutrients. History The Cairncross Reserve was given to the Landsborough Shire Council in 1941 by three Thynne sisters. They named the reserve after their mother, Mary Thynne (née Cairncross, born in 1848). Sunshine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Somerset Regional Council
The Somerset Region is a local government area located in the West Moreton region of South East Queensland, Australia, about northwest of Brisbane and centred on the town of Esk. It was created in 2008 from a merger of the Shire of Esk and the Shire of Kilcoy. It is commonly known as the Brisbane Valley, due to the Brisbane River which courses through the region, although significant parts of the region lie outside the hydrological Brisbane Valley itself. The Esk and Kilcoy Shires were amalgamated to consolidate the water catchments for the Wivenhoe and Somerset Dams. The Local Government Reform Commission identified that the long-term future of Somerset would be as a major water catchment for the SEQ region with farming being the main economic activity within a water catchment management regime. The "planning strategy and land use policies" implemented by the Somerset Regional Council are therefore "directed this end". The Somerset Regional Council, which administers the r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conondale Range
The Conondale Range is a mountain range in Queensland, located between Maleny, Kenilworth, Kilcoy and Jimna. The range is the most westerly part of the Sunshine Coast hinterland and part of the Great Dividing Range. The highest point on the range is Mount Langley reaching 868 m above sea level. This is also the highest point in the Brisbane River catchment. Lower foothills of the range around Kilcoy are used for grazing. Most of the steep forested slopes of the range are state forests and Conondale National Park. In the south, parts of Stony Creek are preserved in Bellthorpe National Park. The mountains are the source of the Brisbane River. Creeks on the south of the range drain into the Stanley River and directly into Lake Somerset. To the north creeks flow into the Mary River. History Dalla (also known as Dalambara and Dallambara) is a language of the Upper Brisbane River catchment, notably the Conondale Range. Dalla is part of the Duungidjawu language region inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brisbane River
The Brisbane River is the longest river in South East Queensland, Australia, and flows through the city of Brisbane, before emptying into Moreton Bay on the Coral Sea. John Oxley, the first European to explore the river, named it after the Governor of New South Wales, Sir Thomas Brisbane in 1823. The penal colony of Moreton Bay later adopted the same name, eventually becoming the present city of Brisbane. The river is a tidal estuary and the water is brackish from its mouth through the majority of the Brisbane metropolitan area westward to the Mount Crosby Weir. The river is wide and navigable throughout the Brisbane metropolitan area. The river travels from Mount Stanley. The river is dammed by the Wivenhoe Dam, forming Lake Wivenhoe, the main water supply for Brisbane. The waterway is a habitat for the rare Queensland lungfish, Brisbane River cod (extinct), and bull sharks. Early travellers along the waterway admired the natural beauty, abundant fish and rich vegetation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Douglas, Queensland
Port Douglas is a coastal town and locality in the Shire of Douglas, Queensland, Australia, approximately 60 km north of Cairns. In the , Port Douglas had a population of 3,504 people. The town's population can often double, however, with the influx of tourists during the peak tourism season from May to September. The town is named in honour of a former Premier of Queensland, John Douglas. Port Douglas developed quickly based on the mining industry. Other parts of the area were established with timber cutting occurring in the area surrounding the Daintree River and with settlement starting to occur on lots around the Mossman River by 1880. Previous names for the town included Terrigal, Island Point, Port Owen and Salisbury. The town is situated adjacent to two World Heritage areas, the Great Barrier Reef and the Daintree Rainforest. Port Douglas was No. 3 on Australian Traveller magazine's list of 100 Best Towns in Australia."100 Best Towns in Australia". Retrieved 21 July 201 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Noosa, Queensland
The Shire of Noosa is a Local government in Australia, local government area about north of Brisbane in the Sunshine Coast, Queensland, Sunshine Coast district of South East Queensland, Australia. The shire covers an area of . It existed as a local government entity from 1910 until 2008, when it was Merger (politics), amalgamated with the Shire of Maroochy and City of Caloundra to form the Sunshine Coast Region. The shire was re-established on 1 January 2014. History Geological history The Noosa Hinterland was formed during the Oligocene, Oligocene era around 25-30 million years ago when Volcanism, volcanic activity created the ranges. By the beginning of the Neolithic, Neolithic era, Noosa's coast experienced a change in sea level rises when its beaches and waterways began to take shape. Ancient history The Noosa area was originally home to several Indigenous Australian, Aboriginal groups. They primarily include the ''Undumbi'' tribe to the south, the ''Dulingbara'' to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queensland Government
The Queensland Government is the democratic administrative authority of the Australian state of Queensland. The Government of Queensland, a parliamentary constitutional monarchy was formed in 1859 as prescribed in its Constitution, as amended from time to time. Since the Federation of Australia in 1901, Queensland has been a State of Australia, with the Constitution of Australia regulating the relationships between all state and territory governments and the Australian Government. Under the Australian Constitution, all states and territories (including Queensland) ceded powers relating to certain matters to the federal government. The government is influenced by the Westminster system and Australia's federal system of government. The Governor of Queensland, as the representative of Charles III, King of Australia, holds nominal executive power, although in practice only performs ceremonial duties. In practice executive power lies with the Premier and Cabinet. The Cabinet of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Araucaria Bidwillii
''Araucaria bidwillii'', commonly known as the bunya pine and sometimes referred to as the false monkey puzzle tree, is a large evergreen coniferous tree in the plant family Araucariaceae. It is found naturally in south-east Queensland Australia and two small disjunct populations in north eastern Queensland's World Heritage listed Wet Tropics. There are many old planted specimens in New South Wales, and around the Perth, Western Australia metropolitan area. They can grow up to . The tallest presently living is one in Bunya Mountains National Park, Queensland which was reported by Robert Van Pelt in January 2003 to be in height. The bunya pine is the last surviving species of the Section ''Bunya'' of the genus ''Araucaria''. This section was diverse and widespread during the Mesozoic with some species having cone morphology similar to ''A. bidwillii'', which appeared during the Jurassic. Fossils of Section ''Bunya'' are found in South America and Europe. The scientific name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunya Mountains
The Bunya Mountains are a distinctive set of peaks forming an isolated section of the Great Dividing Range in southern Queensland. The mountain range forms the northern edge of the Darling Downs in the locality also called Bunya Mountains near Bell and Dalby. The mountains are south of Kingaroy and just to the south west of Nanango. The range is the remains of a shield volcano which was built from numerous basalt lava flows about 23-24 million years ago. In 2009 as part of the Q150 celebrations, the Bunya Mountains was announced as one of the Q150 Icons of Queensland for its role as a "Natural attraction". Landforms The range rises to an average elevation of 975 m; however the two tallest mountains on the range, Mount Kiangarow and Mount Mowbullan, rise to over 1,100 m. Slopes facing the north east are part of the Burnett River catchment, those on the south east make up part of the Brisbane River catchment, while those facing the south west belong to the Conda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
