The document summarizes various marine erosion processes that form coastal landforms. It describes hydraulic action, corrasion, attrition, and corrosion as processes that slowly wear away cliff rock. These processes can form features like wave-cut notches, platforms, caves, arches, stacks, and stumps. The document also explains how alternating resistant and soft rock layers along coastlines can form headlands and bays through differential erosion.
Every continent or island is bordered by a long or short coastline. Coastline is the line separating the land and sea. Coastal zones are the transition zones between terrestrial and marine habitat. They form an interface between land and oceanic natural processes. Coastal areas also are varied in their topography, climate and vegetation. Some are sandy beaches, rocky shores, with or without tidal inlets. The climate of a coast are controlled by the land and sea breezes and the humidity controlled by marine water. Waves are powerful tools for constructive and destructive activities. Hence. the geomorphology of beach, materials and processes are always not constant due to the impact of everlasting action of tides, waves and currents.
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Every continent or island is bordered by a long or short coastline. Coastline is the line separating the land and sea. Coastal zones are the transition zones between terrestrial and marine habitat. They form an interface between land and oceanic natural processes. Coastal areas also are varied in their topography, climate and vegetation. Some are sandy beaches, rocky shores, with or without tidal inlets. The climate of a coast are controlled by the land and sea breezes and the humidity controlled by marine water. Waves are powerful tools for constructive and destructive activities. Hence. the geomorphology of beach, materials and processes are always not constant due to the impact of everlasting action of tides, waves and currents.
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
This is my second presentation. Me and my friend created this presentation. This presentation tropic is Indian shoreline classification. So all people watch this tropic and comment my fault for this tropic. And comments for new tropic name so i am help for help for any geography subject related tropic. THANK YOU
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
This is my second presentation. Me and my friend created this presentation. This presentation tropic is Indian shoreline classification. So all people watch this tropic and comment my fault for this tropic. And comments for new tropic name so i am help for help for any geography subject related tropic. THANK YOU
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
A2 CAMBRIDGE GEOGRAPHY: CHARACTERISTICS AND FORMATION OF COASTAL LANDFORMSGeorge Dumitrache
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.
GEOGRAPHY YEAR 10: COASTAL LANDFORMS. It contains: coastal landforms, depositional landforms, beaches, attrition, spits, longshore drift, tombolos, cliffs, the procesa of cliff erosion, headlands and bays, caves, arches, stacks and stumps.
Erosion is when wind, water, and ice take sediments away.
Erosion on coasts by wind and water.
Water is major agent of erosion.
About 21% of all erosion in done by coastal erosion.
Similar to Marine Erosion Process And Erosional Landforms (20)
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4. Hydraulic Action The force of waves hitting a cliff (or sea wall) compresses water and air into cracks and joints. This can be equivalent to 30,000kg per square metre. This increase in pressure may lead to cracks widening and pieces of rock breaking off.
5. Corrasion (abrasion) Rock fragments may be picked up by waves and thrown against the rock face of cliffs by subsequent waves. The effectiveness of the corrasion depends on the strength of the wave, the nature of its ‘load’ and the resistance of the rock in the cliff face. Corrasion is most effective at the base of cliffs
6. Attrition Rock fragments which have become detached by hydraulic action and corrasion are worn down into smaller and more rounded pieces. Currents and tidal movements cause the fragments to be swirled around and to grind against each other. This type of erosion produces pebble beaches.
7. Corrosion (solution) Salts and acids in sea water can react with rocks , slowly dissolving them away. The photo shows this process on a cliff of Portland limestone which has been chemically attacked by carbonic acid and other chemicals in sea water.
8.
9. Coastlines of Erosion 1. Headlands and bays 2. Cliffs and wave cut platforms 3. Headland erosion and the formation of caves, blowholes, arches, stacks and stumps
20. Caves Caves usually develop from widening and deepening of notches where there are weaknesses in the cliff face This large cave at Arbroath is fault guided. Can you see the fault?
21. Erosive waves may blast their way vertically through lines of weakness in the roofs of caves. This produces a blowhole on the cliff top. In stormy conditions sea spray may spout from blowholes. Blowholes
22. This huge blowhole is the Gaylet Pot near Auchmithie. The tractor on the skyline is at the top of the cliffs.
23. Arches These are formed by the wearing away of narrow headlands often by two back-to-back cave systems joining. Durdle Door The waves continue to erode at the foot of the arch widening it. Eventually the roof of the arch can no longer be supported and it will collapse.
24. Here a cave and arch are forming on the same headland at Auchmithie
25. Stacks and stumps Stacks often represent the seaward remnant of a collapsed arch. These tall, isolated pillars of rock such as ‘The Pinnacles’ on the Dorset coast, are reduced by further wave action to stumps.
26. The ‘Deil’s Heid’ stack at Arbroath is interesting because sea level has fallen since it was formed. There is very little erosion around its base so it is unlikely to become a stump for a very long time.
27. We can now imagine how the headland at Durdle Door might be evolving Durdle Door in the past………