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Bemm River
The Bemm River is a perennial river, located in the East Gippsland region of the Australian state of Victoria. Course and features Formed by the confluence of the Errinundra and Combienbar rivers, the Bemm River rises below near Boulder Flat, northwest of the town of . The river flows generally south then south by east, through the Bemm River Scenic Reserve and the Cape Conran Coastal Park, joined by the Goolengook and McKenzie rivers and six minor tributaries, before reaching its mouth with Bass Strait via Sydenham Inlet in the Shire of East Gippsland, near the settlement of . The river descends over its course. The catchment area comprises mainly public land, including Errinundra National Park and the Lind National Park. These areas have a broad range of ecosystems including cool and warm temperate rainforest, ancient wet eucalypt forest, coastal heathland and banksia woodland. The Bemm River catchment area is managed by the East Gippsland Catchment Management Auth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Aboriginal Languages
The Indigenous languages of Australia number in the hundreds, the precise number being quite uncertain, although there is a range of estimates from a minimum of around 250 (using the technical definition of 'language' as non-mutually intelligible varieties) up to possibly 363. The Indigenous languages of Australia comprise numerous language families and isolates, perhaps as many as 13, spoken by the Indigenous peoples of mainland Australia and a few nearby islands. The relationships between the language families are not clear at present although there are proposals to link some into larger groupings. Despite this uncertainty, the Indigenous Australian languages are collectively covered by the technical term "Australian languages", or the "Australian family". The term can include both Tasmanian languages and the Western Torres Strait language, but the genetic relationship to the mainland Australian languages of the former is unknown, while the latter is Pama–Nyungan, thoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Conran Coastal Park
Cape Conran Coastal Park is a coastal reserve located near Marlo in East Gippsland in Victoria, Australia. The 11,700 hectare area was declared a coastal park under the ''National Parks Act 1975'' (Vic) in 1997. It is 420 km east of Melbourne and 530 km south of Sydney. Flora and fauna Much of the area is covered by heathland and banksia woodland which attracts nectar-feeding birds. Dolphins and whales (depending on the time of year) may be spotted off the coast. The abundant bird life includes white-bellied sea eagles and the eastern ground parrot The eastern ground parrot (''Pezoporus wallicus'') of Australia is one of only five ground-dwelling parrots in the world, the others being its closest relatives, the western ground parrot (''Pezoporus flaviventris''), the extremely rare night pa .... Recreation The area is used for a number of water-based activities including boating, fishing, swimming, diving and rock pooling. Short walks within the park include the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Gippsland Catchment Management Authority
The Catchment Management Authorities (CMAs) were established in Victoria under the ''Catchment and Land Protection Act 1994''. Originally known as Catchment and Land Protection Boards, the CMAs were changed to their present name in 1997. Catchment management authorities are unique because the area they govern corresponds to the naturally occurring drainage basins, enabling integrated catchment management. Catchment Management Authorities There are 10 CMAs covering the whole of Victoria, these are divided into a total of 39 river basins (some basins are shared by more than one CMA): * Corangamite **Barwon basin **Corangamite basin **Moorabool basin (part) **Otway basin *East Gippsland **East Gippsland basin **Mitchell basin **Snowy basin **Tambo basin * Glenelg Hopkins **Glenelg basin **Hopkins basin **Portland basin * Goulburn Broken **Broken basin **Goulburn basin * Mallee **Avoca basin (part) **Mallee basin **Wimmera basin (part) * North Central **Campaspe basin **Loddon bas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eucalypt
Eucalypt is a descriptive name for woody plants with capsule fruiting bodies belonging to seven closely related genera (of the tribe Eucalypteae) found across Australasia: ''Eucalyptus'', '' Corymbia'', '' Angophora'', ''Stockwellia'', ''Allosyncarpia'', ''Eucalyptopsis'' and ''Arillastrum''. Taxonomy For an example of changing historical perspectives, in 1991, largely genetic evidence indicated that some prominent ''Eucalyptus'' species were actually more closely related to ''Angophora'' than to other eucalypts; they were accordingly split off into the new genus ''Corymbia''. Although separate, all of these genera and their species are allied and it remains the standard to refer to the members of all seven genera ''Angophora'', ''Corymbia'', ''Eucalyptus'', ''Stockwellia'', ''Allosyncarpia'', ''Eucalyptopsis'' and ''Arillastrum'' as "eucalypts" or as the eucalypt group. The extant genera ''Stockwellia'', ''Allosyncarpia'', ''Eucalyptopsis'' and ''Arillastrum'' comprise six k ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Rainforest
Temperate rainforests are coniferous or broadleaf forests that occur in the temperate zone and receive heavy rain. Temperate rain forests occur in oceanic moist regions around the world: the Pacific temperate rain forests of North American Pacific Northwest as well as the Appalachian temperate rainforest of the Eastern U.S. Sun Belt; the Valdivian temperate rain forests of southwestern South America; the rain forests of New Zealand and southeastern Australia; northwest Europe (small pockets in Great Britain and larger areas in Ireland, southern Norway and northern Iberia); southern Japan; the Black Sea–Caspian Sea region from the southeasternmost coastal zone of the Bulgarian coast, through Turkey, to Georgia, and northern Iran. The moist conditions of temperate rain forests generally support an understory of mosses, ferns and some shrubs and berries. Temperate rain forests can be temperate coniferous forests or temperate broadleaf and mixed forests. Definition For temperat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lind National Park
The Lind National Park is a national park in the East Gippsland region of Victoria, Australia. The national park is situated approximately east of Melbourne, adjacent to the Princes Highway between Orbost and . See also * Protected areas of Victoria Victoria is the smallest mainland state in Australia. it contained separate protected areas with a total land area of (17.26% of the state's area). Of these, 45 were national parks, totalling (11.32% of the state's area). The parks are man ... References External linksLind National Park on Parks Victoria website* National parks of Victoria (Australia) Protected areas established in 1925 1925 establishments in Australia East Gippsland {{Australia-protected-area-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Errinundra National Park
The Errinundra National Park is a national park located in the Gippsland region of Victoria, Australia. The national park is situated east of Melbourne via the Princes Highway and is centred on the Errinundra Plateau, a southwards extension of the Monaro Tablelands of New South Wales. Features The Errinundra National Park preserves the largest remaining cool temperate rainforest in Victoria and supports some of south eastern Australia's most spectacular old growth forests. There are also many rare and threatened species of flora and fauna, including powerful owls, tiger quolls and long-footed potoroos. Cool and warm temperate rainforest, wet open forest, montane forests and woodlands are the dominant vegetation communities. There is also a sub-alpine wetland. The majority of the park is accessible only in the drier months. In winter, rain and snow generally make the unsealed roads impassable. There has been extensive logging of all forest types surrounding the park includin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perennial Stream
A perennial stream is a stream that has continuous flow of surface water throughout the year in at least parts of its catchment during seasons of normal rainfall, Water Supply Paper 494. as opposed to intermittent river, one whose flow is intermittent. In the absence of irregular, prolonged or extreme drought, a perennial stream is a watercourse, or segment, element or emerging body of water which continually delivers groundwater. For example, an damming, artificial disruption of stream, variability in flow or stream selection associated with the activity in hydropower installations, do not affect this status. Perennial streams do not include stagnant water (stream pool, pools and puddle, waterholes), reservoirs, oxbow lake, cutoff lakes and ponds that persist throughout the year. All other streams, or parts of them, should be considered seasonal rivers or lakes. The stream can cycle from intermittent to perpetual through multiple iterations. Stream Definition The basic conc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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