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Summary coastal landforms

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This document provides a concise yet informative summary of various landforms found across the globe. From towering mountains to expansive plains, winding rivers to rugged coastlines, this resource offers a comprehensive exploration of Earth's diverse geological features. Readers will gain a deeper...

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  • September 6, 2023
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  • 2023/2024
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Cliffs

Formation of Cliffs:

- Several erosion processes, including weathering, abrasion, hydraulic action, and corrasion,
work together to wear down the rock surfaces.Softer rocks erode more quickly, while harder,
more resistant layers remain intact. This differential erosion creates the steep, vertical, or
near-vertical faces characteristic of cliffs.

Factors Influencing Cliff Formation:

- The type of rock strongly influences cliff formation. The hardness, resistance to weathering,
and composition of the rocks determine how quickly erosion processes can shape the
landscape into cliffs. For example, cliffs formed from hard, durable rocks like granite tend to
be more enduring.

Processes Involved in Cliff Formation:

- Weathering, which includes both physical processes like freeze-thaw cycles and chemical
processes, gradually breaks down rock into smaller particles. Erosion processes, such as
abrasion, hydraulic action, and corrasion, wear away the rock surfaces over time.

Example: The White Cliffs of Dover in England: These iconic coastal cliffs are made primarily of pure
white chalk and are formed by a combination of geological factors and marine erosion processes.




Wave - cut platform
Formation of Wave-Cut Platforms:

- The primary process behind the formation of wave-cut platforms is wave erosion, especially
the action of waves carrying sand, pebbles, and larger rock fragments. Over time, constant
wave action causes abrasion, as these particles are hurled against the rock surface. This
process gradually wears away the rock, forming a flat, horizontal surface, known as the
wave-cut platform.

Factors Influencing Wave-Cut Platform Formation:

, - The type of rock present along the coastline significantly influences the formation of wave-cut
platforms. Hard, erosion-resistant rock types are more likely to withstand the relentless wave
action, resulting in the development of these platforms.
- The energy and frequency of waves are determined by factors such as the wind, ocean
currents, and the depth of the water. Coastal areas exposed to high-energy waves and
frequent storms are more likely to experience substantial wave erosion, leading to the
formation of more extensive wave-cut platforms.

Processes Involved in Wave-Cut Platform Formation:

- Waves carry sand, pebbles, and larger rock fragments. As these particles are repeatedly
thrown against the rocky shoreline, they act as natural abrasives, wearing away the rock
surface over time.

Example: The Jurassic Coast in England, particularly the area around Lulworth Cove.




Caves

Formation of Caves:

- As the rock dissolves, it creates voids or cavities within the rock mass. These voids can
enlarge through various erosional processes, such as mechanical weathering and hydraulic
action . Additionally, cave formation can involve the deposition of minerals, such as calcium
carbonate, which precipitate out of the water and gradually build up formations like stalactites
and stalagmites.

Factors Influencing Cave Formation:

- The rate of cave formation is influenced by climate and the availability of water. Regions with
higher rainfall or significant groundwater flow are more conducive to cave development
because they provide a continuous source of water that can dissolve and erode the rock over
time.

Processes Involved in Cave Formation:

- The dissolution of soluble rocks by slightly acidic water, often containing carbonic acid, is the
primary process driving cave formation. Over time, this chemical reaction eats away at the
rock, creating voids and openings within the rock mass.
- Erosional processes, such as mechanical weathering and hydraulic action, can enlarge
existing cavities within the rock. Additionally, the deposition of minerals, such as calcium

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