Einasleigh River
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Einasleigh River
The Einasleigh River is a river in Far North Queensland, Australia. When combined with the Gilbert River, the river system is the largest river system in northern Australia. Course and features The Einasleigh River rises in the locality of Lyndhurst in the Einasleigh Uplands within the Atherton Tableland, draining the western slopes of the Great Dividing Range below Mount Remarkable. The river flows generally north, northwest and then west. The river is joined by 33 tributaries from source to mouth including the Copperfield and Etheridge rivers and numerous creeks before reaching its confluence with the Gilbert River north of . The Einasleigh River has a catchment area of . Following its confluence, the Gilbert River spills into a vast estuarine delta approximately wide that largely consists of tidal flats and mangrove swamps across the Gulf Country. The Einasleigh River descends over its course. East of the river is crossed by the Einasleigh River Bridge that carries ...
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River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ...
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Etheridge River
Etheridge may refer to: People * Bill Etheridge, a British politician, Member of the European Parliament for UKIP * Bob Etheridge (born 1941), US Representative * Chris Etheridge, British sidecarcross rider * Emerson Etheridge, late US Representative * George Etherege, English dramatist *James Etheridge, English MP * Joanne Etheridge, Australian physicist * John Etheridge, English Jazz guitarist * John Wesley Etheridge (1804–1866), English nonconformist minister and scholar * Melissa Etheridge, a singer-songwriter * Neil Etheridge, English-Filipino footballer * Robert Etheridge (1819–1903), English geologist and palaeontologist. *Robert Etheridge, Junior (1847–1920), English palaeontologist who worked extensively in Australia * Zac Etheridge: American football coach and player. Places * Shire of Etheridge The Shire of Etheridge is a local government area in Far North Queensland, Australia in what is known as the Savannah Gulf region. Its economy is based on cattle gra ...
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Wet Season
The wet season (sometimes called the Rainy season) is the time of year when most of a region's average annual rainfall occurs. It is the time of year where the majority of a country's or region's annual precipitation occurs. Generally, the season lasts at least a month. The term ''green season'' is also sometimes used as a euphemism by tourist authorities. Areas with wet seasons are dispersed across portions of the tropics and subtropics. Under the Köppen climate classification, for tropical climates, a wet season month is defined as a month where average precipitation is or more. In contrast to areas with savanna climates and monsoon regimes, Mediterranean climates have wet winters and dry summers. Dry and rainy months are characteristic of tropical seasonal forests: in contrast to tropical rainforests, which do not have dry or wet seasons, since their rainfall is equally distributed throughout the year.Elisabeth M. Benders-Hyde (2003)World Climates.Blue Planet Biomes. Retr ...
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Potomac River
The Potomac River () drains the Mid-Atlantic United States, flowing from the Potomac Highlands into Chesapeake Bay. It is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map. Retrieved August 15, 2011 with a drainage area of 14,700 square miles (38,000 km2), and is the fourth-largest river along the East Coast of the United States and the 21st-largest in the United States. Over 5 million people live within its watershed. The river forms part of the borders between Maryland and Washington, D.C. on the left descending bank and between West Virginia and Virginia on the right descending bank. Except for a small portion of its headwaters in West Virginia, the North Branch Potomac River is considered part of Maryland to the low-water mark on the opposite bank. The South Branch Potomac River lies completely within the state of West Virginia except for its headwaters, which lie in Virginia. Course The Potomac River runs ...
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Monsoon
A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is also sometimes used to describe locally heavy but short-term rains. The major monsoon systems of the world consist of the West African, Asia–Australian, the North American, and South American monsoons. The term was first used in English in British India and neighboring countries to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in the southwest bringing heavy rainfall to the area. Etymology The etymology of the word monsoon is not wholl ...
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Gulf Developmental Road
Gulf Developmental Road is an Australian highway linking the Cairns and Normanton regions in northern Queensland, Australia. It is the only sealed (asphalt) road linking these two regions. In the east, the road begins at an unnamed junction on the southern edge of Forty Mile Scrub National Park, 241 km south-west of Cairns. The Gulf Developmental Road runs west before terminating at its junction with the Burke Developmental Road 7 km south of Normanton, a total distance of 442 km. Towns along the route include Mount Surprise, Georgetown and Croydon. There are no other communities along the route, but it passes through the ghost town of Cumberland. The road is sealed for its full length, but as of 2018 there are many sections of the road which are only single lane bitumen. These sections require caution when passing other traffic as the shoulders are gravel and vehicles need to move partly onto the shoulders. They extend between points about 55 kilometres west of ...
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Einasleigh River Bridge
The Einasleigh River Bridge is a road bridge over the Einasleigh River on the Gulf Developmental Road, in the Far North Queensland, Australia, located east of Georgetown and west of Mount Surprise. The bridge is part of the only sealed (asphalt) road linking Cairns and Normanton in the Gulf Savannah region. The new high set bridge was constructed to flood-proof the Gulf Country. It replaced an existing low level bridge which was designed for inundation. The old bridge was flooded in every wet season. In 2009 it was under water for 40 days after the biggest flood on record. During flooding of the old Einasleigh River Bridge, most communities across the Gulf Shires were inaccessible by road and the emergency supplies had to be provided by helicopter. The bridge was built by the Etheridge Shire Council and was funded through the Australian Government's Regional and Local Community Infrastructure Program. It was opened on 20 January 2011 by Simon Crean Simon Findlay Cr ...
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Watercourse
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater (spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwater ...
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Gulf Country
The Gulf Country is the region of woodland and savanna grassland surrounding the Gulf of Carpentaria in north western Queensland and eastern Northern Territory on the north coast of Australia. The region is also called the Gulf Savannah. It contains large reserves of zinc, lead and silver. The Gulf Country is crossed by the Savannah Way highway. Location and description The Gulf Country is a block of dry savanna between the wetter areas of Arnhem Land and the Top End of the Northern territory to the west and the Cape York Peninsula of Far North Queensland to the east, while to the south and east lie upland plains of Mitchell grasses and the Einasleigh Uplands. The Northern Territory side of the area is the Gulf Fall area of sandstone slopes and gorges draining the interior uplands into the gulf. The main land uses in the Gulf Country are beef cattle and mining. The region covers an area of . The landscape is generally flat and low-lying tropical savannah cut through with ri ...
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Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ...
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Mangrove
A mangrove is a shrub or tree that grows in coastal saline water, saline or brackish water. The term is also used for tropical coastal vegetation consisting of such species. Mangroves are taxonomically diverse, as a result of convergent evolution in several plant families. They occur worldwide in the tropics and subtropics and even some temperate coastal areas, mainly between latitudes 30° N and 30° S, with the greatest mangrove area within 5° of the equator. Mangrove plant families first appeared during the Late Cretaceous to Paleocene epochs, and became widely distributed in part due to the plate tectonics, movement of tectonic plates. The oldest known fossils of Nypa fruticans, mangrove palm date to 75 million years ago. Mangroves are salt-tolerant trees, also called halophytes, and are adapted to live in harsh coastal conditions. They contain a complex salt filtration system and a complex root system to cope with saltwater immersion and wave action. They are ad ...
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Bureau Of Meteorology (Australia)
The Bureau of Meteorology (BOM or BoM) is an executive agency of the Australian Government responsible for providing weather services to Australia and surrounding areas. It was established in 1906 under the Meteorology Act, and brought together the state meteorological services that existed before then. The states officially transferred their weather recording responsibilities to the Bureau of Meteorology on 1 January 1908. History The Bureau of Meteorology was established on 1 January 1908 following the passage of the ''Meteorology Act 1906''. Prior to Federation in 1901, each colony had had its own meteorological service, with all but two colonies also having a subsection devoted to astronomy. In August 1905, federal home affairs minister Littleton Groom surveyed state governments for their willingness to cede control, finding South Australia and Victoria unwilling. However, at a ministerial conference in April 1906 the state governments agreed to transfer responsibility for m ...
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