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Comboyne Parish (Macquarie County), New South Wales
Comboyne is a village on the Mid North Coast region of New South Wales. It is situated on the Comboyne Plateau, some 60 km south-west of Port Macquarie, 35 km west of Kew and 54 km north-west of Taree. It is an attractive agricultural area with fertile soils and a high rainfall. The word "Comboyne" is a corruption of the local Biripi people's name for "a place of kangaroos" (Gambuyn). At the , Comboyne had a population of 453. The Birpai (also known as Birrbay) people have lived in this area for more than 40,000 years. Previously, the area was covered in sub-tropical rainforest which has almost all been cleared by the early 20th century. The early explorers originally sought the valuable timber of the Australian Red Cedar. The second oldest natural reserve in the state is at nearby Boorganna Nature Reserve which preserves a remnant of sub-tropical rainforest. The Antarctic beech has been recorded at four sites in the Comboyne area. Geology and climate The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Macquarie-Hastings Council
Port Macquarie-Hastings Council is a local government area in the Mid North Coast region of New South Wales, Australia. The area is located adjacent to the Hastings River, the Pacific Highway, the Oxley Highway and the North Coast railway line. Major population centres in the local government area are Port Macquarie, Camden Haven, Wauchope, Lake Cathie and Kendall. The mayor of the Port Macquarie-Hastings Council since 4 August 2017 is Cr. Peta Pinson, an independent politician. Port Macquarie suburbs * Blackmans Point * Port Macquarie CBD (not a suburb) * Fernbank Creek * Flynns Beach * Innes View * Lake Innes * Limeburners Creek * North Shore * Port Macquarie * Port Macquarie West * Sancrox * Sovereign Hills * Tacking Point * The Hatch * Thrumster Towns and localities Towns and localities (including Port Macquarie suburbs) in the Port Macquarie-Hastings Council are: Demographics At the 2011 Census, there were people in the Port Macquarie-Hastings local gove ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lophozonia Moorei
''Nothofagus moorei'', commonly known as Antarctic beech, is an important Gondwana relict of the rainforests of the southern hemisphere. It occurs in wet, fire-free areas at high altitude in eastern Australia. The Antarctic beech group (Nothofagaceae) is an ancient type of tree, of significance to southern hemisphere botanical distribution. Plants in the Nothofagaceae are currently found in southern South America (Chile, Argentina) and Australasia (east and southeast Australia, New Zealand, New Guinea and New Caledonia). Taxonomy Ferdinand von Mueller described the Antarctic beech in 1866, from material collected near the Bellinger River by Charles Moore. Once referred to as 'negrohead beech', but now as 'Antarctic beech' (not to be confused with its South American relative, ''Nothofagus antarctica'') is an evergreen tree native to the eastern highlands of Australia. ''N. moorei'' proposed to be renamed ''Lophozonia moorei'' in 2013. The change in name from ''Nothofagu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Podzol
In soil science, podzols are the typical soils of coniferous or boreal forests and also the typical soils of eucalypt forests and heathlands in southern Australia. In Western Europe, podzols develop on heathland, which is often a construct of human interference through grazing and burning. In some British moorlands with podzolic soils, cambisols are preserved under Bronze Age barrows (Dimbleby, 1962). Term Podzol means "under-ash" and is derived from the Russian под (pod) + зола́ (zola); the full form is "подзо́листая по́чва" (podzolistaya pochva, "under-ashed soil"). The term was first given in middle of 1875 by Vasily Dokuchaev. It refers to the common experience of Russian peasants of plowing up an apparent under-layer of ash (leached or E horizon) during first plowing of a virgin soil of this type. Characteristics Podzols can occur on almost any parent material but generally derive from either quartz-rich sands and sandstone or sedimentary debri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Podsolisation
Podsolisation is an extreme form of leaching which causes the eluviation of iron and aluminium sesquioxides. The process generally occurs in areas where precipitation is greater than evapotranspiration. The minerals are removed by a process known as leaching. When organic material is broken down nutrients are released, but at the same time organic acids are released. These organic acids are known as chelating agents. Many podsol soils form underneath coniferous forests, the fact that pine trees are evergreen causes a very thin litter layer inhibiting the production of humus. As a result an acidic (pH 4.5) mor humus is produced which provides a greater amount of chelating agents.Rode A. A. To the problem of the degree of podzolization of soils // Studies in the genesis and geography of soils. M.: Acad. Sci. USSR, 1935. P. 55-70. The A Horizon In podsolisation, chelating agents break down clay and release minerals such as iron and aluminium. When iron and aluminium are hydrated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Dividing Range
The Great Dividing Range, also known as the East Australian Cordillera or the Eastern Highlands, is a cordillera system in eastern Australia consisting of an expansive collection of mountain ranges, plateaus and rolling hills, that runs roughly parallel to the east coast of Australia and forms the fifth-longest land-based mountain chain in the world, and the longest entirely within a single country. It is mainland Australia's most substantial topographic feature and serves as the definitive watershed for the river systems in eastern Australia, hence the name. The Great Dividing Range stretches more than from Dauan Island in the Torres Strait off the northern tip of Cape York Peninsula, running the entire length of the eastern coastline through Queensland and New South Wales, then turning west across Victoria before finally fading into the Wimmera plains as rolling hills west of the Grampians region. The width of the Range varies from about to over .Shaw, John H., ''Col ... [...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] |
Lismore, New South Wales
Lismore is a city in northeastern New South Wales, Australia and the main population centre in the City of Lismore Local government in Australia, local government area; it is also a regional centre in the Northern Rivers region of the State. It is situated on a low flood plain on the banks of the Wilsons River (New South Wales), Wilsons River near the latter's junction with Leycester Creek, both tributaries of the Richmond River which enters the Pacific Ocean at Ballina, New South Wales, Ballina, to the east. The original settlement initially developed as a grazing property in the 1840s, then became a timber and agricultural town and inland port based around substantial river traffic, which prior to the development of the road and rail networks was the principal means of transportation in the region. Use of the river for transport declined and then ceased around the mid-twentieth century, however by that time Lismore (which was elevated to city status in 1946) had become well est ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Beech At Comboyne
''Nothofagus moorei'', commonly known as Antarctic beech, is an important Gondwana relict of the rainforests of the southern hemisphere. It occurs in wet, fire-free areas at high altitude in eastern Australia. The Antarctic beech group (Nothofagaceae) is an ancient type of tree, of significance to southern hemisphere botanical distribution. Plants in the Nothofagaceae are currently found in southern South America (Chile, Argentina) and Australasia (east and southeast Australia, New Zealand, New Guinea and New Caledonia). Taxonomy Ferdinand von Mueller described the Antarctic beech in 1866, from material collected near the Bellinger River by Charles Moore. Once referred to as 'negrohead beech', but now as 'Antarctic beech' (not to be confused with its South American relative, ''Nothofagus antarctica'') is an evergreen tree native to the eastern highlands of Australia. ''N. moorei'' proposed to be renamed ''Lophozonia moorei'' in 2013. The change in name from ''Nothofagu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boorganna Nature Reserve
The Boorganna Nature Reserve is a protected nature reserve located northwest of Taree on the Comboyne Plateau in New South Wales, Australia. The reserve, managed by the NSW National Parks & Wildlife Service, was gazetted in 1904 and is the second oldest nature reserve in the state. The reserve features various forest types, including stands of sub tropical rainforest of which the large rosewood, yellow carabeen and small leaf fig are particularly noteworthy. The reserve is a remnant of the former extensive rainforest on the Comboyne Plateau. The plateau was cleared between 1900 and 1925. Australian red cedar was logged in the area in the nineteenth century. Originally proposed to be part of the world heritage rainforest group. The exploration, knowledge, uses and history of this area by Indigenous Australians is not well known in the present day. Boorganna Nature Reserve was proposed, but rejected for inclusion on the UNESCO World Heritage, due to being geographically isolated ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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