Waves
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Strong waves erode and deposit material on shorelines over time, forming various landforms. These include sea cliffs created as wave-induced cracks in rock expand and break off pieces. Sea caves are also formed as weaker rocks are carved out by wave erosion. When erosion joins cracks close to each other, sea arches form. Further erosion can cause arch roofs to collapse, leaving behind stacks. Beaches are landforms created through the temporary deposition of sand and soil by wave action.
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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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Waves cause coastal erosion and depositional features through processes like abrasion, hydraulic action, and corrosion. As waves approach shorelines, they can form erosional landforms such as headlands, bays, wave-cut notches, and platforms. Waves also transport sediment via processes like traction, saltation, and suspension, building depositional features along coastlines through longshore drift. This can result in beaches, spits, tombolos, bars, and barrier islands.
COASTS ENM 142 Lecture 7.pptx
The document discusses coastal landforms and the processes involved in their formation. It covers both erosional and depositional coastal features. Erosional features like cliffs, arches and stacks are formed by processes like wave action, weathering and erosion concentrating on headlands. Depositional features such as beaches, spits and bars are produced by constructive waves depositing sediment transported by longshore drift. The key forces shaping the coast are waves, tides, currents and the underlying geology of the area.
Costal landforms
Coastlines are formed through erosion and sediment deposition processes. They are shaped by sea level changes and the interaction between land and ocean. A coastline includes beaches, cliffs, and other landforms at the boundary between land and sea. Coastal zones experience continuous change from tidal movements and ocean interactions with the shore. Erosional landforms like sea cliffs and arches form through destructive wave energy, while depositional landforms like beaches and barrier islands are built up from sediment deposition.
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This document discusses various types of coastal erosion and protection methods. It describes the characteristics and impacts of constructive and destructive waves. It also explains various coastal landforms that form from erosion like cliffs, arches and stacks. Additionally, it outlines different coastal management techniques like riprap, seawalls, beach replenishment and managed retreat. The advantages and disadvantages of each protection strategy are provided.
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Erosion is the process by which earth's surface is worn away by agents such as water, wind, and ice. There are several types of erosion. Water erosion includes splash erosion, sheet erosion, rill erosion, and gully erosion caused by rain and moving water. Streams erode their banks through hydraulic action, corrosion, and impact of particles. Coastal erosion is caused by the pounding of ocean waves, which carve out sea caves, arches, and sea stacks. Wind erosion occurs in deserts and polishes rocks. Glacial erosion processes include abrasion, plucking, and thrusting, which carve out valleys and leave behind moraines. Human activities like agriculture and defore
Ch 3 Our Changing Earth 2.pptx
This document discusses how the Earth's landscape is continuously changed by various forces. It describes how rivers erode landscapes to form landforms like waterfalls, meanders, ox-bow lakes, and deltas. Sea waves erode coastal areas to form sea caves, sea arches, and sea cliffs. Glaciers erode and deposit material as they move, leaving behind moraines and carving out lakes. Wind erosion forms structures like mushroom rocks and deposits materials to create sand dunes and loess. The document provides examples of different landforms shaped by these external, or exogenic, geological processes.
Erosion, weathering and mass movement
The document discusses various types of coastal erosion and mass movement processes, as well as different techniques for managing coastal erosion, including both hard and soft engineering approaches. Hard engineering techniques use man-made structures like seawalls to defend the coast, while soft techniques work with natural processes like beach nourishment. The document provides examples of techniques like groynes, gabions, revetments, rock armor, and beach replenishment.
Erosion, Weathering And Mass Movement
The document discusses various types of coastal erosion and mass movement processes, as well as different techniques for managing coastal erosion, including both hard and soft engineering approaches. Hard engineering techniques use man-made structures like seawalls to defend the coast, while soft techniques work with natural processes like beach nourishment. The document provides examples of techniques like groynes, gabions, revetments, rock armor, and beach replenishment.
3 e coasts (1)
Coasts are shaped by the dynamic forces of the sea, air, and waves. Waves erode coastlines through hydraulic action, abrasion, attrition, and corrosion. Erosion carves out coastal landforms like cliffs, headlands, and bays. Waves also transport and deposit eroded material, building up beaches and forming depositional landforms such as spits, bars, and sand dunes. Managing coastal change involves either "hard engineering" using structures, or "soft engineering" techniques like beach nourishment and managed retreat that work with natural coastal processes.
Coastal Geomorphology Landforms Of Wave Erosion & Deposition
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.
Coastal land forms .erosional and depositional landforms
1) Coastal landforms are shaped by wave erosion and deposition. Waves erode cliffs and deposit sediment to form features like beaches, bars, and spits.
2) Erosional landforms include sea cliffs, arches, stacks, and caves which are carved out of rock by wave action. Depositional landforms are beaches, bars, barriers and hooks built up from sediment deposited by waves and currents.
3) Tides and currents influence coastal landforms by transporting sediment and changing the level and reach of wave energy along the shoreline.
Coastal Processes handout
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.
A report on a field trip
The document summarizes an educational field trip taken by geography students from the University of Education, Winneba to coastal areas in the Western Region of Ghana. The trip aimed to provide visual examples of coastal landforms and geomorphological processes. Key stops included Komenda Beach, Shama Beach, and Nkontompo. At each location, lecturers described various landforms formed by wave erosion, such as cliffs, notches, caves, blowholes, arches, stacks, bays, and headlands. The trip gave students practical experience seeing coastal features that they had previously only read about theoretically. Overall, the excursion provided a valuable learning experience for the geography students.
Wave Cut Platform
A wave-cut platform is a narrow, flat area formed at the base of sea cliffs due to erosion from destructive waves during storms. Destructive waves undermine the cliff face through hydraulic action and corrasion, creating a wave-cut notch. Continued erosion enlarges the notch until the cliff above collapses, exposing a flat terrace known as a wave-cut platform. As the cliff continues retreating inland, the platform grows wider.
Marine Systems
The document summarizes coastal processes and features. It discusses how waves erode, transport, and deposit material, shaping coastlines. Coastal landforms like cliffs, headlands, bays, beaches, and sand dunes are formed through erosion or deposition. Coastal management considers both human uses of coasts and techniques to address physical processes like erosion.
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS
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.
Landform Notes
The document summarizes the key layers that make up Earth's structure, from crust to inner core. It then discusses plate tectonics and how the movement and convergence of tectonic plates results in one plate being pushed under another. Evidence of past tectonic motion comes from matching rock types and fossils on opposite sides of oceans.
Coastal
The coastline marks the meeting point between land and sea which is constantly changing due to erosion, transport and deposition processes driven by wave energy. Waves transfer energy from wind to water, changing shape as they reach shallow areas, and can both erode coastlines through processes like abrasion or build them up through deposition. Sediment is transported alongshore and across shorelines by processes like longshore drift, forming coastal features such as beaches, spits and bars. Coastal management uses various methods like sea walls, beach replenishment or groynes to protect shorelines from erosion.
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Coastal geography waves, features of erosion and deposition, longshore drift
Coastal geography waves, features of erosion and deposition, longshore drift
Coastal Geomorphology Landforms Of Wave Erosion & Deposition
Coastal Geomorphology Landforms Of Wave Erosion & Deposition
Coastal land forms .erosional and depositional landforms
Coastal land forms .erosional and depositional landforms
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMS
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Waves
- 2. Submitted by SARA MOL SOCIAL SCIENCE REG. NO.: 13367015
- 4. Strong waves cause changes on the shores through the erosional and depositional processes. This leads to the conformation of different land forms. Sea cliff Sea caves Sea arches Stacks Beaches
- 5. Due to the force of the waves racks occur to the rocks to the rocks which are situated near to the shore in coarse of time these cracks becomes bigger and pieces tall away in to the ocean. This causes steep slopes to form on the shores. They are called sea cliffs.
- 6. Due to erosion by the waves, weak rocks by the side of the sea are carved out and sea caves are formed
- 7. Some times due to the weathering and erosion caused by the waves which are close to each other are joined are arches are formed.
- 8. When the size of the caves increases further due to the continued erosional processes, the roofs of the arches would collapse. The structure that remain after these are called stacks.
- 9. These are formed due to the depositional work of the waves. The sand and soil brought by the waves are temporarily deposited to from beachers.