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No2b) four Characteristics of the lithosphere
1- Rigid components
2- Predominance of sedimentary rocks
3- Soil of organic and inorganic substances
4- Division of plates
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3a)
Outwash Plain
Also called a sandur, an outwash plain is formed by glaciers. Such a plain is formed when a glacier deposits sediments at its terminus. As a glacier moves, it erodes the bedrock and carries the eroded sediments downstream. These sediments are deposited by the meltwater of the glacier at the snout. Outwash plains are a common landform in Iceland. The Skeiðarársandur in Iceland is the world’s largest outwash plain with an area of 1,300 square km.
Till Plain
A till plain is also a plain formed by glacial action. Such plains are formed by the deposition of glacial till (unsorted glacial sediment). When a sheet of glacial ice gets detached from the main glacier and melts in place, the sediments are deposited on the ground to result in the formation of a till plain. Such plains can be seen in northern Ohio where they were created by the Wisconsin glaciation.
Scroll Plain
Scroll plains are formed in areas where a river meanders across a low gradient. Deposition of sediments at such locations results in the formation of a plain. Oxbow lakes are common occurrences in such areas. The Taieri River forms a spectacular scroll plain near Paerau in New Zealand.
1- Rigid components
2- Predominance of sedimentary rocks
3- Soil of organic and inorganic substances
4- Division of plates
===========
===========
3a)
Outwash Plain
Also called a sandur, an outwash plain is formed by glaciers. Such a plain is formed when a glacier deposits sediments at its terminus. As a glacier moves, it erodes the bedrock and carries the eroded sediments downstream. These sediments are deposited by the meltwater of the glacier at the snout. Outwash plains are a common landform in Iceland. The Skeiðarársandur in Iceland is the world’s largest outwash plain with an area of 1,300 square km.
Till Plain
A till plain is also a plain formed by glacial action. Such plains are formed by the deposition of glacial till (unsorted glacial sediment). When a sheet of glacial ice gets detached from the main glacier and melts in place, the sediments are deposited on the ground to result in the formation of a till plain. Such plains can be seen in northern Ohio where they were created by the Wisconsin glaciation.
Scroll Plain
Scroll plains are formed in areas where a river meanders across a low gradient. Deposition of sediments at such locations results in the formation of a plain. Oxbow lakes are common occurrences in such areas. The Taieri River forms a spectacular scroll plain near Paerau in New Zealand.
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