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Igcse coastal geomorph
 

Igcse coastal geomorph

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    Igcse coastal geomorph Igcse coastal geomorph Presentation Transcript

    • Coastal GeomorphologyThe shape of the coast and its landforms is a direct result of:Geology + Marine processes + Sub-aerial processes + Man + (Climate)
    • Marine processes
    • Constructive waves  These are depositional waves as they lead to sediment build up, and are most common where a large fetch exists.  They tend to have a low gradient, a larger swash than backwash, low energy and an elliptical orbit.  The wave period is long, with 6-8 waves breaking in a minute.
    • Destructive waves  These act as agents of erosion, because backwash is greater than swash.  They are most common where fetch is short, have a mainly circular orbit, a steep gradient, and plunge onto the beach.  The wave period is short, with 12- 14 waves breaking per minute.
    • Wave definitions  Wave fetch: The distance of open water over which a wave has passed. Maximum fetch is the distance from one coastline to the next landmass, it often coincides with prevailing wind direction (South West in the UK).  Wave crest: Highest point of a wave.  Wave trough: Lowest point of a wave.  Wave height: Distance between trough and crest.  Wave length: Distance between one crest/trough and the next.  Swash: Water movement up a beach.  Backwash: Water movement down a beach.
    • Wave refraction It is very rare for waves to approach a regular uniform coastline, as most have a variety of bays, beaches and headlands. Because of these features, the depth of water around a coast varies and as a wave approaches a coast its progress is modified due to friction from the seabed, halting the motion of waves. As waves approach a coast they are refracted so that their energy is concentrated around headlands but reduced around bays. Waves then tend to approach coastline parallel to it, and their energy decreases as water depth decreases.
    • Discordant coastline
    • Concordant
    • Summary of coastal erosionprocesses
    • Coastal erosionAbrasion/corrasion: When waves approach the coastline they are carrying material such as sand, shingle, pebbles and boulders. Abrasion occurs when this material is hurled against cliffs as waves hit them, wearing the cliff away.Hydraulic pressure: Cliffs and rocks contain many lines of weakness in the form of joints and cracks. A parcel of air can become trapped/compressed in these cracks when water is thrown against it. The increase in pressure leads to a weakening/cracking of the rock.Corrosion/solution: Seawater contains carbonic acid, which is capable of dissolving limestone. The evaporation of salts in seawater produces crystals and their formation can lead to the disintegration of rocks.Sub-aerial: Coastal erosional processes that are not linked to the action of the sea. Erosion occurs via rain, weathering by wind and frost. Its impact is often seen in soil creep, slumping and landslides.Human activity: Much building and recreation occurs at the coast, and this increases pressure on cliff tops, making them more liable to erosion and subsidence. The building of sea defences upsets the dynamic equilibrium of the coastline.
    • Influences on the rate oferosion The rate at which a stretch of coastline is eroded is related to the following factors:  The point at which the wave breaks - (if at the foot of a cliff, the cliff is subject to maximum energy and most erosion).  Steepness of the wave.  Depth of sea, fetch, aspect.  Amount of beach material - (a wide beach protects a cliff more than an arrow beach).  Rock type and structure - (hard rock such as granite is far more resistant to erosion than soft rocks, such as clay).
    • The sub-aerial processes
    • Sub-aerial processes Sub-aerial processes = weathering + mass movement + humans*Weathering = physical + chemicalMass movement = falls + flows + slides + slumps + creep*Pressure on cliffs (construction work) Sea Defences (although designed to reduce erosion - in some instances (e.g. the use of groynes) can increase erosion by starving down stream areas of sediment
    • Weathering – basic summary Weathering Processes: Weathering is the breaking up of rock in situ Freeze-thaw processes (as water freezes and thaws in cracks in cliffs, the expansion and contraction forces the rock open, making them more susceptible to the action of waves). Chemical weathering - water running down the face of cliffs, either from surface runoff from above or from rainfall can result in solution so that rock cracks are enlarged, leaving the remaining rock loosened Biological weathering - burrowing organisms and roots of vegetation forces open cracks, making them more susceptible to wave erosion) [NOT sub-aerial] Human Activity
    • The weathering processes Physical WeatheringDefinition: Form of weathering responsible for the mechanical breakdown of rocks but involving no chemical change.Forces acting on rock exposed on the Earths surface open up any weak points in the rock and cause pieces to be broken off.Piles of jagged rock fragments called scree are formed.Freeze-thaw ( a fatigue process) Salt crystallisation Insolation weathering↑ 9% on freezing. ↑ Volume not accretion In presence of H2O only – granular7-15kg/cm2 (2115 kgcm-2 @ -22oC) Sedimentary more than igneous disintegrationPossibility of granular disintegrationSurface unloading (exfoliation) HydrationPressure release Water absorption – clays - kaolinite e.g. SiO2 + 2H2O i Si(OH)4
    • The weathering processes Chemical WeatheringDefinition: Form of weathering brought about by chemical attack on rocks, usually in the presence of water. Chemicalweathering involves the breakdown of the original minerals within a rock to produce new minerals (such as clayminerals, bauxite, and calcite).Solution - the general term for chemical dissolving of rock mineralsHydrolysis Oxidation Carbonation•H+ ion - e.g. the hydrolysis of feldspars •O2 in gaseous form or dissolved in •CO2 + H2O → H2CO3 leads toe.g. orthoclase feldspar produces clay water will reacts with metal ions; •CaCO3 + H2O → CO2 + Ca (HCO3 ) 2minerals such as kaolinite,+ H+ and •Particularly significant on sedimentarysilicic acid. •4FeO + 3H2O + O2 → 2Fe2O3.3H2O rocks eg. Limestone and chalk of the•Particularly significant on igneous Jurassic coastrocks eg. Basalts of Northern Ireland
    • Sub-aerial processes Mass Movement
    • Cliffs – erosional landformFactors determining cliff formation Geological. Sub-aerial. Marine. Meteorological. Human activity. The rule of thumb! Cliffs are steep if removal of material at its base is greater than supply.Cliffs are shallow if the supply of material is greater than removal.
    • Mass movement
    • Mass Movement This is a combination of a rockfall & earthflow
    • Types of cliff
    • Soft Geology Cliff Fairlight Cove is mostly softer unconsolidated rocks. These rocks are less resistant to erosion & landslips are common Typical of NE England
    • Cliff & Wave Cut Platform Wave attack constantly erodes the cliff base, creating a Wave Cut Notch. As the cliff is undercut, it collapses, leaving rockfalls on the beach below. As the cliff retreats it leaves behind a gently sloping platform – Wave Cut Platform
    • Rotational Slumping The full extent of (rotational) slumping can be seen on the west side of the cove.
    • Coastal transportCoastal TransportWeathering and erosion at the coast produces large amounts of material which ismoved along the coast line and out to sea by the action of waves.Up and down the beach: Material is moved up the beach in the swash and backdown the beach in the backwash. Constructive waves move large amounts ofmaterial up the beach as they have a strong swash, whereas destructive wavesmove large amounts of material down the beach due to their strong backwash.The movement of material by waves: The movement of material within the wavesthemselves depends on (i) the size of the material and (ii) the energy available fortransporting the material. There are four possible types of transport within thewater:Solution - material carried dissolved in the waterSuspension - fine material carried suspended within the water itselfSaltation - material which is too heavy to be continuously held in suspension isbounced along the sea bed.Traction - the heaviest material is simply rolled along the sea bed
    • Coastal transport 1. Waves break on the beach at an angle controlled by the prevailing wind direction. Material is moved up the beach in the swash. 2. Material then moves straight back down the beach in the backwash under the influence of gravity. 3. As the processes continues material moves along the coast in a zig-zag movement.