Watheroo National Park
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Watheroo National Park
Watheroo National Park is a national park in Western Australia, 187 km north of Perth. It contains Jingemia Cave. The park is situated in the Mid West region of Western Australia to the west of the Midlands Road between the towns of Badgingarra to the west and Dalwallinu to the east. The border of the park abuts Pinjarrega Nature Reserve to the north but is otherwise surrounded by farmland. Low Creek borders the park to the east, and then flows south to join Moore River. The park is mostly composed of sand plain country, which supports populations of heath, mallee and Banksia and many wildflowers. Eucalypt stands can be found to the western end of the park. Other species include spinifex, wandoo and yorm gum. Some of the wildflowers found within the park include kwongan, bush cauliflower and scarlet featherflower. The name of the park comes from the Indigenous Australian name of a nearby spring; it is also the name of a town located to the east of the park. Compose ...
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Moora, Western Australia
Moora is a townsite located 177 km north of Perth in the Wheatbelt region of Western Australia. Moora was one of the original stations on the Midland railway line to Walkaway, and the townsite was gazetted in 1895. At the , Moora had a population of 1,755. Commercial area The town is the largest wheat belt town between Geraldton and Perth. The town provides facilities and services such as commercial banks, schools, commerce and retail sectors, community recreational facilities; plus a Pharmacy, Dentist, Doctors and District Hospital. The surrounding areas produce wheat and other cereal crops. The town is a receival site for Cooperative Bulk Handling. Natural disasters The town was left underwater in 1932 when heavy rainfall inundated the town, causing severe flooding. The town was left isolated as both rail lines and roads had portions washed away. Over half the town was submerged to a depth of , and once the waters receded, was left under a thick coating of mud. Crops ...
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Verticordia Eriocephala
''Verticordia eriocephala'', commonly known as lambswool, and common, native or wild cauliflower is a flowering plant in the myrtle family, Myrtaceae and is endemic to the south-west of Western Australia. It is a shrub with one densely branching, spreading main stem, small leaves and dense heads of creamy-white flowers, giving rise to the common names "lambswool" and "cauliflower". It is widespread over its range but becoming less common because of land clearing and illegal collecting of the flowers. Description ''Verticordia eriocephala'' is a shrub which grows to a height of or more and a spread of and which has a single, highly branched stem at its base. Its leaves are elliptic in shape, dished and long, becoming shorter and broader near the flowering parts at the top. The flowers are scented and arranged in dense corymb-like groups, each flower on a stalk about long. The floral cup is hemispherical, long, constricted above the middle and hairy near its base. The sepals ...
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National Parks Of Western Australia
Western Australia is the second largest country subdivision in the world. It contains no fewer than separate Protected Areas with a total area of (land area: – 6.30% of the state’s area). Ninety-eight of these are National Parks, totalling (2.14% of the state’s area). Protected areas of Western Australia Conservation Parks As of 2014, the following 58 conservation parks are listed as part of the National Reserve System with a total area of . *Blackbutt * Boyagarring * Brooking Gorge *Burra *Camp Creek *Cane River * Coalseam *Dardanup *Devonian Reef *Geikie Gorge *Goldfields Woodlands * Gooralong *Hester *Kerr *Korijekup * Lane Poole *Laterite *Len Howard *Leschenault Peninsula * Leschenaultia * Lupton *Monte Bello Islands *Mount Manning - Helena And Aurora Ranges *Muja * Penguin Island *Rapids * Rowles Lagoon * Shell Beach *Totadgin *Unnamed WA01333 *Unnamed WA17804 *Unnamed WA23088 *Unnamed WA23920 *Unnamed WA24657 *Unnamed WA28740 *Unnamed WA29901 *U ...
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Protected Areas Of Western Australia
Western Australia is the second largest country subdivision in the world. It contains no fewer than separate Protected Areas with a total area of (land area: – 6.30% of the state’s area). Ninety-eight of these are National Parks, totalling (2.14% of the state’s area). Protected areas of Western Australia Conservation Parks As of 2014, the following 58 conservation parks are listed as part of the National Reserve System with a total area of . *Blackbutt * Boyagarring * Brooking Gorge *Burra *Camp Creek *Cane River * Coalseam *Dardanup *Devonian Reef *Geikie Gorge *Goldfields Woodlands * Gooralong *Hester *Kerr *Korijekup * Lane Poole *Laterite *Len Howard *Leschenault Peninsula * Leschenaultia * Lupton *Monte Bello Islands *Mount Manning - Helena And Aurora Ranges *Muja * Penguin Island *Rapids * Rowles Lagoon * Shell Beach *Totadgin *Unnamed WA01333 *Unnamed WA17804 *Unnamed WA23088 *Unnamed WA23920 *Unnamed WA24657 *Unnamed WA28740 *Unnamed WA29901 *U ...
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Seismic Survey
Reflection seismology (or seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth's subsurface from reflection (physics), reflected seismic waves. The method requires a controlled seismic source of energy, such as dynamite or Tovex blast, a specialized Seismic source#Air gun, air gun or a seismic vibrator. Reflection seismology is similar to sonar and acoustic location, echolocation. This article is about surface seismic surveys; for vertical seismic profiles, see vertical seismic profile, VSP. History Reflections and refractions of seismic waves at geologic Interface (matter), interfaces within the Earth were first observed on recordings of earthquake-generated seismic waves. The basic model of the Earth's deep interior is based on observations of earthquake-generated seismic waves transmitted through the Earth's interior (e.g., Mohorovičić, 1910). The use of human-generated seismic waves to map ...
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Gas Field
A petroleum reservoir or oil and gas reservoir is a subsurface accumulation of hydrocarbons contained in porous or fractured rock formations. Such reservoirs form when kerogen (ancient plant matter) is created in surrounding rock by the presence of high heat and pressure in the Earth's crust. Petroleum reservoirs are broadly classified as ''conventional'' and '' unconventional'' reservoirs. In conventional reservoirs, the naturally occurring hydrocarbons, such as crude oil or natural gas, are trapped by overlying rock formations with lower permeability, while in unconventional reservoirs, the rocks have high porosity and low permeability, which keeps the hydrocarbons trapped in place, therefore not requiring a cap rock. Reservoirs are found using hydrocarbon exploration methods. Oil field An oil field is an area of accumulation of liquid oil underground in multiple (potentially linked) reservoirs, trapped as it rises by impermeable rock formations. In industrial terms, an ...
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Environmental Protection Authority Of Western Australia
The Environmental Protection Authority of Western Australia (EPA) is a statutory authority within the Government of Western Australia, established on 1 January 1972, which acts as the primary provider of independent environmental advice to the government. Since 27 November 2009 it has been supported administratively by the Office of the Environmental Protection Authority (OEPA), which was amalgamated with the Department of Environment Regulation and the Department of Water to form the Department of Water and Environmental Regulation on 1 July 2017. It operates under the ''Environmental Protection Act 1986''. The EPA provides advice to the Minister for Environment through various reports, as well as releasing statements to the public detailing significant environmental matters. Its role also includes formulation of environmental protection policies. History On 27 November 2009 the Western Australian Government formed a dedicated department to support the EPA, known as the Of ...
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Darling Scarp
The Darling Scarp, also referred to as the Darling Range or Darling Ranges, is a low escarpment running north–south to the east of the Swan Coastal Plain and Perth, Western Australia. The escarpment extends generally north of Bindoon, to the south of Pemberton. The adjacent Darling Plateau goes easterly to include Mount Bakewell near York and Mount Saddleback near Boddington. It was named after the Governor of New South Wales, Lieutenant-General Ralph Darling. History The feature was first recorded as General Darling Range by Charles Fraser, Government Botanist with Captain James Stirling aboard in March 1827. Maps from the 1830s show the scarp labelled " General Darlings Range"; this later became Darling Range, a name by which the formation was still commonly known in the late 20th century despite common understanding of it being an escarpment. There is also a tendency to identify the locations on or to the east of the scarp as being in the "Perth Hills" (or simpl ...
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Dandaragan Plateau
Dandaragan plateau is a feature between the Darling Scarp and Gingin scarp in Western Australia. Dandaragan locality and Shire of Dandaragan council of the same name occur on the plateau. The integrity of the Boonanarring reserve on the plateau is notable due to its sustaining animals that are lost on the Swan Coastal Plain The Swan Coastal Plain in Western Australia is the geographic feature which contains the Swan River as it travels west to the Indian Ocean. The coastal plain continues well beyond the boundaries of the Swan River and its tributaries, as a geol .... The geology and flora of the plateau has been studied and reported for some time. References {{reflist, 30em Geology of Western Australia Shire of Dandaragan ...
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Laterite
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods. Tropical weathering (''laterization'') is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Cancer and Capricorn. Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to calls for the term to be abandoned alto ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ...
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