Australia: The Land Where Time Began
A biography of the Australian continentMajor Landform regions of Australia See also
The Australian continent is broadly divided into 4 major landform regions, each of which is comprised of smaller-scale constituent landform regions - eastern highlands, central lowlands, western plateau and the coastal plains.
The Eastern Highlands, the Great Divide, also called the Great Diving Range, runs for about 4,000 km from the tip of Cape York to theGrampian Ranges in Victoria. It divides the runoff into eastern and western-flowing rivers. East of the ranges the rivers empty into the Pacific Ocean. To the west the rivers tend to be centrally draining, often ending in ephemeral salt lakes. Erosion of the Great Divide has formed the Great Escarpment on their eastern, seaward, side. About half of all Australian rivers run inland, many ending is salt lakes, that are mostly dry.
The Central Lowlands, from the Murray-Darling Basin and north to the Gulf Of Carpentaria, are mostly flat, with occasional higher ground in the form of desert ranges such as the Macdonnell Ranges and the Musgrave Ranges. Also found here are a number of deserts, Sturt's Stony Desert,Strzelecki Desert and Simpson Desert, the world's largest sand ridge desert. The lowest point on the Australian continent, Lake Eyre, is also situated in this region. It also includes inselbergs such as Uluru and Kata Tjuta. About 38 % of the Australian continent is less than 200 m above sea level (so far), much of it in the Central lowlands.
The Western Plateau includes much of Western Australia, and parts of South Australia and the Northern Territory. This is the oldest part of the continent, the rocks being some of the most ancient in Australia, having been formed in the very early stages of the solidification of the Earth. They have mostly been exposed to the forces of erosion for almost the entire history of the Earth. Some of the plateaus in this region are theKimberley, Hamersley and Yilgarn. These plateaus are partly based on cratons such as the Yilgarn Craton and Pilbara Craton. As subsidence occurred, much of the area became depocentres for the mostly inward-flowing rivers, resulting in the flat topography of most of the area. The inselbergs like Uluru and Kata Tjuta gained their prominence in the landscape by the surrounding ground surface being eroded to form a flat plain, leaving the more erosion-resistant rocks of the inselbergs.
Along the east coast, from Cape York to Victoria, the area between the Great Escarpment and the sea, is mostly in the form of a flat coastal plain.
Sources & Further reading
Landforms can differ in shape and size, such as mountains being tall and narrow while plateaus are flat and raised. Landforms can vary in composition, with some being made of rock, others of soil, and others of ice. Landforms can differ in formation processes, like volcanoes being formed through volcanic activity, while canyons are carved by erosion.
Landforms can impact daily life in various ways. For example, mountainous regions can limit transportation routes and access to resources, while coastal areas may be susceptible to flooding and storms. Additionally, the availability of arable land for agriculture can be influenced by the type of landform present.
Yes, landforms continue to affect today's development in various ways, such as influencing urban planning, agricultural practices, and infrastructure construction. For example, cities may be built around natural resources like rivers or harbors, and agricultural regions are often influenced by the fertility of the landforms. Additionally, landforms can present challenges for construction, transportation, and environmental conservation efforts.
Landforms vary from place to place on Earth due to differences in geological processes, such as tectonic activity, erosion, and weathering. These processes shape the land in unique ways, creating diverse landforms like mountains, valleys, plains, and coastlines. Factors like climate, soil composition, and vegetation also contribute to the variation of landforms across different regions.
Landforms can be created through tectonic plate movement, where plates collide, separate, or slide past each other, leading to the creation of mountains, valleys, and rifts. Erosion by water, wind, or ice can also shape landforms over time, like canyons, caves, and arches. Volcanic activity can form landforms such as volcanoes, lava plateaus, and calderas when magma reaches the Earth's surface.
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what are three ways that people have changed the land in our country
Volcanoes can change the Earth's surface quickly by producing lava flows that can cover large areas in a short time, creating new landforms. They can also trigger landslides and lahars (mudflows) that rapidly reshape the landscape.
Mountains, hills, plateaus, and plains are the four major types of landforms. Minor landforms include buttes, canyons, valleys, and basins.
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List some ways to change the information in the CMOS
It affect our jobs,driving and homes.
Landforms can differ in shape and size, such as mountains being tall and narrow while plateaus are flat and raised. Landforms can vary in composition, with some being made of rock, others of soil, and others of ice. Landforms can differ in formation processes, like volcanoes being formed through volcanic activity, while canyons are carved by erosion.
maybe change of living clothes and eating.
Pressure Temperature Changes in the molecular structure(chemical change)
Two ways that you can change the sound of an instrument are tuning or adjustment of the valves. Another way to change the sound of an instrument is to change your technique of blowing or bowing technique. I am sure there are more ways but here are some ideas!
Read it on your book people. But it is relate in many ways.