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127:. By using scientific dating methods, or examination of marine fossils found on the platform, it is possible to work out when the platform was formed, thus giving geographers and geologists information about sea levels at known times in the past. This has been used in the United Kingdom and other previously glaciated areas to calculate the rate at which land is rising now that it is no longer covered in ice.
99:, creating a wave-cut notch. This notch then enlarges into a cave. The waves undermine this portion until the roof of the cave cannot hold due to the pressure and freeze-thaw or biological weathering acting on it, and collapses, resulting in the cliff retreating landward. The base of the cave forms the wave-cut platform as
142:
According to
Trenhaile, Sunamura, and Massalink and Hughes, the term 'wave-cut platform' should no longer be used as it assumes that shore platforms are the result of wave action, which is not always true. Shore platforms, like comparable river and lake platforms, are erosional features that develop
74:
that was created by erosion. Wave-cut platforms are often most obvious at low tide when they become visible as huge areas of flat rock. Sometimes the landward side of the platform is covered by sand, forming the beach, and then the platform can only be identified at low tides or when storms move the
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122:
Ancient wave-cut platforms provide evidence of past sea and lake levels. Raised and abandoned platforms, sometimes found behind modern beaches, are evidence of higher sea levels in the geological past, and have been used to identify areas of
256:
103:
causes the collapsed material to be broken down into smaller pieces, while some cliff material may be washed into the sea. This may be deposited at the end of the platform, forming an off-shore beach.
84:
130:
Where the coastline itself is changing due to seismic action, there may be a series of platforms showing earlier sea levels and indicating the amount of uplift caused by various
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Wave-cut platforms form when destructive waves hit against the cliff face, causing an undercut between the high and low water marks, mainly as a result of abrasion,
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Wilson, M.A., Curran, H.A. and White, B. 1998: Paleontological evidence of a brief global sea-level event during the last interglacial.
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153:
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Retallack, G.J. and
Roering, J.J. 2012: Wave-cut or water-table platforms of rocky coasts and rivers? GSA Today 22(6), 4-9.
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Because of the continual wave action, a wave-cut platform represents an extremely hostile environment and only certain
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Trenhaile, A. S. 1987: The
Geomorphology of Rock Coasts. (Oxford University Press, Oxford, U.K.) 393 pp.
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421:
231:
399:
Masselink, G and Hughes, M. 2003. Introduction to
Coastal Processes and Geomorphology. Hodder Arnold
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and other debris by waves and currents leaves behind a bedrock surface below the water table.
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Wave-cut notch and submerged platform in Elet Island, Busuanga, Palawan, Philippines
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Sunamura, T., 1992. Geomorphology of rocky coasts. New York: John Wiley.
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Commonly called a 'rock platform' in
Australia, these two examples at
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234:, N.S.W, are typical of many on the coast of south-eastern Australia.
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is the narrow flat area often found at the base of a
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367:: CS1 maint: archived copy as title (
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87:The formation of a wave-cut platform
27:Narrow flat area created by erosion
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1132:Integrated coastal zone management
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1230:Region of freshwater influence
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214:Jurassic wave-cut platform at
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1:
1279:Coastal and oceanic landforms
992:Large-scale coastal behaviour
824:Beaches in estuaries and bays
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62:or along the shoreline of a
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937:Coastal biogeomorphology
138:Usage of term 'wave-cut'
118:Use of ancient examples
834:Coastal morphodynamics
186:), Utah, United States
88:
39:
1225:Physical oceanography
246:The rock platform at
178:Shore platforms from
86:
34:Wave-cut platform at
33:
1054:Submergent coastline
1007:Marine transgression
962:Discordant coastline
947:Concordant coastline
250:, N.S.W., Australia.
162:and shore platform,
125:isostatic adjustment
1158:Coastal engineering
110:can utilize such a
1127:Coastal management
967:Emergent coastline
638:Intertidal wetland
541:Continental margin
218:, southern England
198:Shore platform at
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40:
1274:Coastal geography
1261:
1260:
1089:Wave-cut platform
1002:Marine regression
546:Continental shelf
536:Coastal waterfall
445:Coastal geography
314:Terrace (geology)
304:Raised shorelines
44:wave-cut platform
38:, South Wales, UK
16:(Redirected from
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1012:Raised shoreline
987:Ingression coast
982:Graded shoreline
957:Cuspate foreland
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733:Submarine canyon
593:Freshwater marsh
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343:. Archived from
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97:hydraulic action
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997:Longshore drift
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338:"Archived copy"
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279:Bench (geology)
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56:wave-cut cliff
48:shore platform
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18:Wave-cut notch
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531:Coastal plain
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350:on 2011-01-12
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52:coastal bench
49:
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19:
1088:
1084:Volcanic arc
972:Feeder bluff
879:River mouths
844:Raised beach
839:Pocket beach
767:
738:Tidal island
728:Strand plain
673:Natural arch
404:
395:
386:
377:
352:. Retrieved
345:the original
335:31: 241-250.
332:
327:
299:Raised beach
216:Tedbury Camp
200:St Bees Head
160:Raised beach
141:
129:
121:
105:
90:
55:
51:
47:
43:
41:
36:Southerndown
1235:River plume
1049:Steep coast
1022:Rocky shore
1017:Rip current
897:River delta
869:Wash margin
864:Storm beach
854:Shell beach
819:Beach wrack
814:Beach ridge
804:Beach cusps
753:Tied island
743:Tidal marsh
466:Archipelago
184:Pleistocene
132:earthquakes
1268:Categories
1163:Grain size
1137:Submersion
1114:Management
1099:Wind fetch
1059:Surf break
977:Flat coast
907:regressive
693:Salt marsh
551:Coral reef
354:2009-10-28
320:References
309:Strandflat
1122:Accretion
1104:Wind wave
1064:Surf zone
919:Processes
892:Mouth bar
849:Recession
829:Beachrock
748:Tide pool
678:Peninsula
566:cliff-top
453:Landforms
248:Long Reef
232:Austinmer
108:organisms
101:attrition
93:corrosion
79:Formation
60:sea cliff
1253:Category
1079:Undertow
1032:Sea foam
1027:Sea cave
927:Blowhole
769:Windwatt
628:Headland
476:Avulsion
363:cite web
268:See also
166:, Norway
1203:shingle
1183:granule
1168:boulder
1146:Related
1042:peresyp
952:Current
887:Debouch
796:Beaches
763:Waituna
758:Tombolo
668:Mudflat
663:Machair
653:Isthmus
573:Estuary
516:Channel
333:Lethaia
284:Machair
145:saprock
1193:pebble
1188:gravel
1178:cobble
723:Strait
703:Skerry
658:Lagoon
643:Island
598:Fundus
501:Bodden
75:sand.
1074:Swash
1037:Shoal
718:Stack
708:Sound
698:Shoal
648:Islet
633:Inlet
623:Hapua
588:Fjord
583:Fjard
578:Firth
526:Coast
521:Cliff
496:Bight
471:Atoll
348:(PDF)
341:(PDF)
274:Beach
164:Bleik
112:niche
70:, or
54:, or
1208:silt
1198:sand
1173:clay
902:mega
713:Spit
683:Reef
613:Gulf
561:Dune
556:Cove
511:Cape
481:Ayre
369:link
202:, UK
95:and
64:lake
688:Ria
618:Gut
608:Geo
603:Gat
491:Bay
72:sea
68:bay
1270::
365:}}
361:{{
134:.
114:.
66:,
50:,
46:,
42:A
437:e
430:t
423:v
371:)
357:.
182:(
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.