Coast 1
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The document defines various coastal landforms and processes. It describes features such as alluvium, arches, atolls, bays, beaches, berms, blowholes, caves, cliffs, and reefs. It also explains coastal erosion processes like attrition and the formation of sand. Coastal defenses like armour blocks and beach nourishment are also defined.
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Powerpoint presentation
The document discusses how sea waves cause morphological changes to shorelines through erosional and depositional processes. This leads to the formation of various landforms, including sea cliffs caused by wave-induced cracking and crumbling of coastal rocks, sea caves formed by wave erosion excavating weak coastal rocks, arches formed when sea caves erode close together, beaches created by waves depositing sand and soil, and stacks which are remnants of collapsed sea arches.
Year 10 geography 2nd lesson
Coastal features include sea stacks which are tall rock columns near the shore, rock platforms formed by wave action at the base of sea cliffs, and beaches deposited by waves. Other coastal features are bays surrounded by land, lagoons separated from the sea by barriers, tidal inlets connecting rivers and streams to the open ocean, sand dunes formed by wind, sea caves formed by wave erosion, rock arches with openings underneath, and blowholes which are vertical shafts connecting sea caves to the surface.
Coastal processes this one
This document provides information about the GCSE Geography course for Mr. Rogers' class, including details on exam dates and percentages of the final mark for different topics. It discusses rivers and coasts, economic geography, settlement and population, and hazards. It provides resources for students, including Mr. Rogers' contact information and links to online materials. Homework is assigned to produce a factfile on a place eroded by the coast.
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Strong waves erode and deposit material on shorelines over time, forming various landforms. This includes sea cliffs from cracks in rocks that widen and break off, sea caves carved out of weak rocks, sea arches formed when erosion joins cracks close together, and stacks remaining after arch roofs collapse. Beaches are also formed as waves temporarily deposit sand and soil.
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A basic presentation of the coasts, suitable for Year 9 Geography. It includes: the definition of a coast, etymology, pelagic coasts and shores, the formation of the coasts, environmental importance, human uses of a coast, coasts and tourism, coast pollution, fishing declining, coastal landforms, cliff erosion, natural arch, sea caves, stacks, stumps, wave-cut notches and wave-cut platforms.
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This document discusses coastal landforms and processes including constructive and destructive wave characteristics, erosion processes like abrasion and hydraulic action, cliff retreat and wave cut platforms. It also discusses coastal management strategies like hard engineering options such as sea walls, revetments and groynes, and soft engineering options like beach replenishment, cliff regrading and managed retreat. The document concludes with an example of coastal management at Swanage which uses beach replenishment, groynes, cliff regrading and drainage.
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Wave Erosion and Deposition Lesson Power Point
Unit 4, Lesson 2 discusses how waves form and impact coastlines. Waves are created by wind blowing over water and have a height, wavelength, and can vary in size depending on wind strength and duration. As waves approach shore they refract and change direction. Wave erosion forms coastal landforms over time like wave-cut cliffs, arches, sea stacks and deposits sediment to form beaches, spits, and barrier islands. Urban development on barrier islands increases hurricane risk. Groins and breakwaters can control sediment transport but have downsides if not planned properly.
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Powerpoint presentation
The document discusses how sea waves cause morphological changes to shorelines through erosional and depositional processes. This leads to the formation of various landforms, including sea cliffs caused by wave-induced cracking and crumbling of coastal rocks, sea caves formed by wave erosion excavating weak coastal rocks, arches formed when sea caves erode close together, beaches created by waves depositing sand and soil, and stacks which are remnants of collapsed sea arches.
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Coastal features include sea stacks which are tall rock columns near the shore, rock platforms formed by wave action at the base of sea cliffs, and beaches deposited by waves. Other coastal features are bays surrounded by land, lagoons separated from the sea by barriers, tidal inlets connecting rivers and streams to the open ocean, sand dunes formed by wind, sea caves formed by wave erosion, rock arches with openings underneath, and blowholes which are vertical shafts connecting sea caves to the surface.
Coastal processes this one
This document provides information about the GCSE Geography course for Mr. Rogers' class, including details on exam dates and percentages of the final mark for different topics. It discusses rivers and coasts, economic geography, settlement and population, and hazards. It provides resources for students, including Mr. Rogers' contact information and links to online materials. Homework is assigned to produce a factfile on a place eroded by the coast.
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Strong waves erode and deposit material on shorelines over time, forming various landforms. This includes sea cliffs from cracks in rocks that widen and break off, sea caves carved out of weak rocks, sea arches formed when erosion joins cracks close together, and stacks remaining after arch roofs collapse. Beaches are also formed as waves temporarily deposit sand and soil.
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This document discusses coastal landforms and processes including constructive and destructive wave characteristics, erosion processes like abrasion and hydraulic action, cliff retreat and wave cut platforms. It also discusses coastal management strategies like hard engineering options such as sea walls, revetments and groynes, and soft engineering options like beach replenishment, cliff regrading and managed retreat. The document concludes with an example of coastal management at Swanage which uses beach replenishment, groynes, cliff regrading and drainage.
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The document discusses various coastal landforms created by wave erosion and deposition along shorelines. It describes how alternating bands of hard and soft rock lead to the formation of headlands and bays through differential erosion. As waves erode the soft rock faster than the hard rock, an irregular coastline develops. Further erosion can form caves, arches, stacks, and stumps. Coves are formed when a stream cuts through a cliff, widening through erosion. Wave-cut platforms are flat terraces exposed when cliffs retreat inland. Longshore drift can build up spits, narrow accumulations of sand and gravel stretching from the shore into the sea.
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1) Headlands and bays are formed by the uneven erosion of coastlines composed of bands of rock with varying resistance. More resistant rocks like granite and basalt form headlands, while less resistant rocks like chalk, sandstone and shale erode more quickly to form bays.
2) Waves concentrate their energy at headlands, eroding them more, while weakening along wider bays where sediments are deposited.
3) Students are expected to learn about beaches, spits and tombolos from their textbook for homework, with examples of different beach gradients based on sediment coarseness.
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Spits are narrow accumulations of sand and/or shingle that extend from shore into a body of water, forming a hooked shape. They are formed through the process of longshore drift, where prevailing winds and waves carry sediments along the coastline from an original headland or coastline feature. As sediments build up, they begin to form a spit, which continues extending as longshore drift deposits more material, with larger particles collected at the spit's base and finer sands at the tip. A spit curves as the direction of longshore drift changes due to shifting prevailing winds or wave refraction around the spit's end.
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The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
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This document defines and describes several key geographical features found near bodies of water. It discusses landforms that jut into water such as headlands, areas of trapped water like lagoons, and large water areas partially enclosed by land known as gulfs and bays. Coasts, cliffs, beaches, and breakwaters that protect harbors from waves are also defined. Caves are formed by waves eroding weak areas of cliffs.
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- The Jurassic Coast exposes geology spanning millions of years, including rocks from the Jurassic period 200-140 million years ago.
- More resistant rock types like chalk erode more slowly than less resistant rocks like clay and limestone, leading to the formation of bays in softer rocks and headlands in harder rocks.
- Lulworth Cove is used as a case study, having formed from differential erosion of tilted rock layers, with the cove eroding inland until reaching
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Beaches form through the process of erosion and deposition by ocean waves. Sediment such as sand and pebbles is eroded from cliffs and shores by wave action and transported down the coast by longshore drift. This sediment is eventually deposited and builds up over time to create beaches. The size and shape of beaches depends on the type of sediment - shingle beaches are steeper while sand beaches have a more gentle slope. Features like spits, bars, and tombolos are also formed through deposition when sediment carried by longshore drift accumulates in different ways.
Swanage power point presentation (reduced)
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Coastal Processes Good
Waves are generally larger in the southwest of the British Isles than the southeast due to larger fetch, or the distance over which wind can blow over open water to generate waves. Waves break when the wavelength reaches the sea floor, causing the bottom of the wave to slow down while the top continues forward. Coastal erosion processes include abrasion by materials carried in waves, hydraulic action as waves enter cracks and cause small explosions, and corrosion as acids in sea water dissolve rocks. These processes form landforms like headlands and bays, cliffs and wave-cut platforms, and over more time, caves, arches, stacks, and stumps.
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L5 Distictive Coastal Deposition Features
Beaches form through deposition by constructive waves, building up material like sand and shingle along sheltered coastlines. Spits develop when longshore drift transports sediment along a coastline that changes direction, forming a narrow hooked landform. Bars are ridges that run parallel to the coast and can temporarily block river mouths and inlets, forming lagoons behind them that may slowly fill in with sediment over time.
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This document discusses coastal erosion processes. Hydraulic action erodes rock when air is forced into cracks by waves, exerting pressure that pulls out rock when the water falls. This type of erosion is called hydraulic action. Coastal erosion forms headlands and bays as harder rock headlands project into the sea while soft rock in between erodes back to form bays. Over time, hydraulic action can form arches, stacks, and stumps in headlands as erosion undercuts the base of cliffs.
Coasts: Headlands and Bays
This document provides information about headlands and bays, including:
1) Headlands and bays are formed by the uneven erosion of coastlines composed of bands of rock with varying resistance. More resistant rocks like granite and basalt form headlands, while less resistant rocks like chalk, sandstone and shale erode more quickly to form bays.
2) Waves concentrate their energy at headlands, eroding them more, while weakening along wider bays where sediments are deposited.
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The document discusses coastal landforms created by erosion. Softer rocks erode more quickly than harder rocks, creating bays where soft rocks were. Harder rocks remain as headlands exposed to erosion, which cracks and enlarges them over time, eventually forming caves. As caves erode further they can form arches that eventually collapse, leaving stacks and stumps.
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This document discusses various coastal landforms and processes. It defines coastal geomorphology and describes how waves, longshore currents, rip currents, and tides shape coastal areas and transport sediment. It then lists and describes specific coastal landforms like headlands, bays, sea cliffs, beaches, bars, spits, tombolos, sand dunes, salt marshes, and more. For each landform, it provides a brief definition and example photo. Coastal erosion processes like abrasion, hydraulic action, corrosion, and attrition are also outlined.
land forms formed by seawaves
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
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This document discusses various coastal geological processes. It describes how coastal erosion occurs through hydraulic action, abrasion, attrition, and solution, forming features like wave-cut cliffs, platforms, sea caves, arches, and stacks. Coastal deposition happens when waves lose energy and drop sediment, forming features like spits, baymouth bars, sand bars, and barrier islands. Coastal inundation, or flooding, can result from storm surges, sea level rise, or tsunamis overtopping or breaching natural or man-made barriers. Coastal subsidence is also discussed, which is the sinking of coastal land caused by various geological processes.
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The document provides information about different types of coastal erosion and how they can be represented through "Kung Fu" gestures. It includes descriptions of four erosion processes - hydraulic action, abrasion, attrition, and corrosion. Students are asked to create gestures to symbolize each process. The document also contains sample exam questions about coastal erosion processes and features formed by erosion.
Beaches AS
Beaches are depositional landforms that form along coastlines where sand and shingle accumulate faster than they are removed by waves. Beaches represent accumulated material deposited between low and high tides. Beach material comes from cliff erosion, offshore sources, and rivers. Sand produces gently sloped beaches below 5 degrees, while shingle produces steeper beaches from 10-20 degrees. Factors like wave energy, type, and longshore drift influence beach profiles.
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This document discusses various coastal landforms and processes, their impacts on people, and methods for managing the coastline and tourist activities. It specifically describes rotational landsliding, longshore drift, and different hard and soft engineering options for reducing coastal erosion, including beach nourishment, groynes, riprap, and planting vegetation. It also addresses managing tourist access through designating protected areas, limiting visitor numbers, and building infrastructure like footpaths, fences, and visitors centers.
Spits
Spits are narrow accumulations of sand and/or shingle that extend from shore into a body of water, forming a hooked shape. They are formed through the process of longshore drift, where prevailing winds and waves carry sediments along the coastline from an original headland or coastline feature. As sediments build up, they begin to form a spit, which continues extending as longshore drift deposits more material, with larger particles collected at the spit's base and finer sands at the tip. A spit curves as the direction of longshore drift changes due to shifting prevailing winds or wave refraction around the spit's end.
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The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
Geografical features
This document defines and describes several key geographical features found near bodies of water. It discusses landforms that jut into water such as headlands, areas of trapped water like lagoons, and large water areas partially enclosed by land known as gulfs and bays. Coasts, cliffs, beaches, and breakwaters that protect harbors from waves are also defined. Caves are formed by waves eroding weak areas of cliffs.
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A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS. It contains: the formation of erosional landforms: cliffs and wave-cut platforms, caves, arches and stacks
Learners should be able to explain the formation of depositional landforms: beaches in cross section (profile) and plan, swash and drift aligned beaches, simple and compound spits, tombolos, offshore bars, barrier beaches, coastal dunes, tidal sedimentation in estuaries, coastal saltmarshes and mangroves, the role of sea level change in the formation of coastal landforms.
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This document provides information about coastal landforms and erosion along the Jurassic Coast in Dorset, England. It discusses how the underlying geology influences erosion rates and the formation of different landforms. Key points covered include:
- The Jurassic Coast exposes geology spanning millions of years, including rocks from the Jurassic period 200-140 million years ago.
- More resistant rock types like chalk erode more slowly than less resistant rocks like clay and limestone, leading to the formation of bays in softer rocks and headlands in harder rocks.
- Lulworth Cove is used as a case study, having formed from differential erosion of tilted rock layers, with the cove eroding inland until reaching
Transportation Deposition
Beaches form through the process of erosion and deposition by ocean waves. Sediment such as sand and pebbles is eroded from cliffs and shores by wave action and transported down the coast by longshore drift. This sediment is eventually deposited and builds up over time to create beaches. The size and shape of beaches depends on the type of sediment - shingle beaches are steeper while sand beaches have a more gentle slope. Features like spits, bars, and tombolos are also formed through deposition when sediment carried by longshore drift accumulates in different ways.
Swanage power point presentation (reduced)
Swanage beach experiences longshore drift that moves sediment from south to north. The Banjo Pier was built perpendicular to the beach to contain river runoff, but it also blocks sediment from reaching the northern beach area. As a result, the northern beach is now narrower and the cliff face there is more prone to landslips as sediment deposition has decreased since the pier was constructed. Groynes and sea walls have been installed to manage erosion issues.
Beaches (teach)
A short description of beach formations and how they most commonly are formed. For elementary science students.
Dawlish Warren
Dawlish Warren is a spit located in Devon, England that is actively managed to prevent erosion. The spit is formed from sand and shingle eroded from Langstone Rock and transported down coast by longshore drift. Vegetation and engineering structures like revetments, sea walls, groynes and rock armor have been installed to stabilize the spit and protect infrastructure like a car park, promenade and lifeboat ramp. Ongoing management includes replanting marram grass, fencing off rehabilitation plots, and using soft techniques like Christmas trees to encourage sand accretion.
Coastal Processes Good
Waves are generally larger in the southwest of the British Isles than the southeast due to larger fetch, or the distance over which wind can blow over open water to generate waves. Waves break when the wavelength reaches the sea floor, causing the bottom of the wave to slow down while the top continues forward. Coastal erosion processes include abrasion by materials carried in waves, hydraulic action as waves enter cracks and cause small explosions, and corrosion as acids in sea water dissolve rocks. These processes form landforms like headlands and bays, cliffs and wave-cut platforms, and over more time, caves, arches, stacks, and stumps.
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- 1. alluvium Any material (usually silt, gravel and sand) deposited by a river or the sea.
- 2. arch A curved 'bridge' of rock created by the continued erosion of a cave, eventually breaking through the headland. Durdle Door Dorset
- 3. armour blocks Large boulders which are piled on a beach to reduce erosion.
- 4. atol Low islands found in tropical oceans, usually formed from the remnants of subsided extinct volcanoes and covered with coral growth.
- 5. attrition A type of erosion caused by rock particles rubbing together as they are pushed around by the sea. Particles of rock become smaller and smaller until sand is produced and deposited on the beach.
- 6. backwash Seawater moving down the beach, to return to the sea. backwash
- 7. backwash Seawater moving down the beach, to return to the sea. backwash
- 8. barrier beach A beach created by a spit reaching across a shallow bay, e.g. Chesil Bank, Dorset.
- 9. barrier reef An extended area of coral reefs formed in shallow tropical seas where the water temperature remains above 18ºC. Great Barrier Reef
- 10. bay A wide recess in the line of the coast between headlands.
- 11. beach An area of mud, sand, shingle or pebbles along the coastline.
- 12. beach nourishment Replacing the beach material, lost through erosion.
- 13. berm Ridges of sand or shingle on the beach, formed by successive wave action. The highest result from storm waves. berm
- 14. blow hole A hole in a cliff through which air escapes. It is created by strong air pressure pushing against a weak cave roof.
- 15. boulder A large stone or rock usually detached from its origin.
- 16. break The falling of the crest of a wave.
- 17. breaker A large mass of turbulent water causing erosion of the shore, resulting from the breaking of large waves.
- 18. cave A large hollow cavity at the foot of a cliff, caused by water erosion. Fingal's Cave in Staffa.
- 19. chalk A soft, white, fine-grained limestone which is prone to coastal features such as caves, arches, blowholes and stacks.
- 20. clay A fine-textured sedimentary rock formed from tiny particles.
- 21. cliff A steep rock face caused by the eroding effect of waves.
- 22. coast The narrow area where the land meets the sea.