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headlands along an embayed coastline(passive) caused bywave refraction
prevailing winds from the Northresultin wave refraction
Teachit Geography CONSTRUCTIVE OR DESTRUCTIVE WAVES Coastal Erosion Homework Sheet Headlandscausewave refraction
the oscillations moving through shallower water on an angle(passive) are caused byRefraction waves
Scatteringmay causerefraction of the wave
hence the propagation speedcausingsound wave refraction
accommodation T Higher order aberration values(passive) may be influenced bywavefront refraction
the jetty 's boulderscausinga refraction wave
segments of the wave moving at different speeds as the water depth along the peak varies(passive) is caused byrefraction Wave refraction
segments of the wave moving at different speeds as the water depth along the crest varies(passive) is caused byWave refraction
bird island(passive) caused byall the wave refraction
the pocketswill causewave refraction
the Earth 's core(passive) caused byThe P wave refraction
a slowly varying depth - uniform current(passive) caused bywave shoaling / refraction
nearshore and(passive) created bywave refraction
Transmissioncausesrefraction of the wave
ccausingwave refraction ( d
the contourscausingwave refraction
important submarine features , such as river mouth bars and ebb tidal delta complexesinfluencewave refraction
A large ebb - tidal deltacauseswave refraction
up ... bank itself and net onshore transport by wave - induced currents ( including kelp - rafted shingle(passive) set ... bywave refraction
Depositional ) Coastal Features Tombolos Occur where spit growth extends to an offshore island Islandoften influenceswave field refraction
The test scores with the younger forceleadsthe wave refraction
a low - energy environment leading to depositioncreatesa low - energy environment leading to deposition
wavefronts to be parallel to the shape of the coastline as they approach the shorecauseswavefronts to be parallel to the shape of the coastline as they approach the shore
An increase in longshore drift(passive) caused byAn increase in longshore drift
such famous surfing breaks as Malibu in California or Jeffrey ’s Bay in South Africacausessuch famous surfing breaks as Malibu in California or Jeffrey ’s Bay in South Africa
the depth of water to be irregular around the coastcausethe depth of water to be irregular around the coast
waves to focus into headlands and away from bays , resulting in rapid erosion of headlands and deposition in bayscauseswaves to focus into headlands and away from bays , resulting in rapid erosion of headlands and deposition in bays
problems in regions where the resolution of the bathymetry is insufficientcan causeproblems in regions where the resolution of the bathymetry is insufficient
the long , smooth , gently curved shoreline that unwinds from both ends towards the middlehas createdthe long , smooth , gently curved shoreline that unwinds from both ends towards the middle
a zone where no p - waves are recorded ( shadow zonecreatesa zone where no p - waves are recorded ( shadow zone
The reflection and/or(passive) are createdThe reflection and/or
erosion of the headlands Compare refraction and diffractioncauseserosion of the headlands Compare refraction and diffraction
the deposition of sand where the waves meet around the islandoriginatesthe deposition of sand where the waves meet around the island
waves to strike as nearcauseswaves to strike as near
a wave to bend and become more parallel to the shorecausesa wave to bend and become more parallel to the shore
water wave energy to converge at cape and causing erosioncauseswater wave energy to converge at cape and causing erosion
a general decrease in the angle of incidence of the waves ... resulting in wave power vectors that are closer to being perpendicular to bathymetric contours as the waves travel toward the shorecausesa general decrease in the angle of incidence of the waves ... resulting in wave power vectors that are closer to being perpendicular to bathymetric contours as the waves travel toward the shore
water and sandcauseswater and sand
alongshore currents and convergence of energy(passive) caused byalongshore currents and convergence of energy
the rear region(passive) influenced bythe rear region
waves to focus their energy on headlands and lose their energy going into bayscauseswaves to focus their energy on headlands and lose their energy going into bays
wave energy to converge at cape and resulting erosionalso causeswave energy to converge at cape and resulting erosion
waves to ... arrive nearly parallel to the shore sedimentcauseswaves to ... arrive nearly parallel to the shore sediment
a wave crest that approaches a coastline at an angle to bend round so that it becomes almost parallel to the coastlineactually causesa wave crest that approaches a coastline at an angle to bend round so that it becomes almost parallel to the coastline
the water to slow and bend in shallow watercausethe water to slow and bend in shallow water
the Langmuir waves to be shifted out of resonance with the electron beam , suppressing the bump - in - tail instabilitycausesthe Langmuir waves to be shifted out of resonance with the electron beam , suppressing the bump - in - tail instability
the bay shape to formcausesthe bay shape to form
energy to be concentrated at headlands ( on high energy coastscausesenergy to be concentrated at headlands ( on high energy coasts
Sedimentation(passive) caused bySedimentation
more erosion on these landformscausesmore erosion on these landforms
errors in radar measurements ... mainly of a target 's range and spatial angles ( elevation and azimuthcan causeerrors in radar measurements ... mainly of a target 's range and spatial angles ( elevation and azimuth
erosion on three sidesis causingerosion on three sides
headlands to be eroded and covescausesheadlands to be eroded and coves
adjustments in the flux of sediment leaving the control cell ( Qoutcausingadjustments in the flux of sediment leaving the control cell ( Qout
a concentration of energy at headlands ( A ) and a distribution of wave energy in bays ( Bcausesa concentration of energy at headlands ( A ) and a distribution of wave energy in bays ( B
an increase in wave heightcan causean increase in wave height
concentrated erosion River Estuary at Southampton water transports fluvial sediment to the Isle of Wight Input at Chesil Beach = sand which causes deposition which forms a tombolo Hard strategies being used Threat of flooding and erosion retreating at an average of 2 mm per year Sediment cell number 2 Subtidal erosion Subtidal siltation Intertidal siltation Inputs and outputs balancedcausesconcentrated erosion River Estuary at Southampton water transports fluvial sediment to the Isle of Wight Input at Chesil Beach = sand which causes deposition which forms a tombolo Hard strategies being used Threat of flooding and erosion retreating at an average of 2 mm per year Sediment cell number 2 Subtidal erosion Subtidal siltation Intertidal siltation Inputs and outputs balanced
wave energies to be concentrated at headlands and dispersed at bayscauseswave energies to be concentrated at headlands and dispersed at bays
directlyinfluencesdirectly
an unusual chirping against the stone of the pyramidcreatesan unusual chirping against the stone of the pyramid
lots of erosioncauseslots of erosion