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Wave-cut platform

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257: 225: 241: 193: 173: 209: 154: 31: 780: 787: 1249: 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
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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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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
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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.
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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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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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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
1103: 1063: 891: 828: 747: 677: 234:, N.S.W, are typical of many on the coast of south-eastern Australia. 92: 59: 413: 83: 1031: 1026: 853: 768: 627: 452: 107: 1167: 1041: 886: 762: 757: 667: 662: 652: 572: 144: 1192: 1187: 722: 702: 657: 642: 500: 1073: 1036: 795: 697: 647: 632: 622: 587: 582: 577: 525: 520: 470: 273: 163: 1207: 1197: 1172: 682: 612: 560: 555: 63: 687: 490: 71: 67: 58:
is the narrow flat area often found at the base of a
1265: 429: 137: 436: 422: 117: 82: 29: 14: 1266: 367:: CS1 maint: archived copy as title ( 443: 417: 87:The formation of a wave-cut platform 27:Narrow flat area created by erosion 24: 1132:Integrated coastal zone management 25: 1290: 1248: 1247: 785: 778: 255: 239: 223: 207: 191: 171: 152: 1230:Region of freshwater influence 402: 393: 384: 375: 325: 214:Jurassic wave-cut platform at 13: 1: 1279:Coastal and oceanic landforms 992:Large-scale coastal behaviour 824:Beaches in estuaries and bays 319: 78: 62:or along the shoreline of a 7: 267: 10: 1295: 1243: 1145: 1112: 917: 877: 794: 776: 451: 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 89: 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 1286: 1251: 1250: 1012:Raised shoreline 987:Ingression coast 982:Graded shoreline 957:Cuspate foreland 789: 782: 733:Submarine canyon 593:Freshwater marsh 438: 431: 424: 415: 414: 409: 406: 400: 397: 391: 388: 382: 379: 373: 372: 366: 358: 356: 355: 349: 343:. Archived from 342: 329: 259: 243: 227: 211: 195: 175: 156: 143:when removal of 97:hydraulic action 21: 1294: 1293: 1289: 1288: 1287: 1285: 1284: 1283: 1264: 1263: 1262: 1257: 1239: 1215:Intertidal zone 1141: 1108: 997:Longshore drift 942:Coastal erosion 913: 873: 809:Beach evolution 790: 784: 783: 774: 461:Anchialine pool 447: 442: 412: 407: 403: 398: 394: 389: 385: 380: 376: 360: 359: 353: 351: 347: 340: 338:"Archived copy" 336: 330: 326: 322: 279:Bench (geology) 270: 263: 260: 251: 244: 235: 228: 219: 212: 203: 196: 187: 180:Lake Bonneville 176: 167: 157: 140: 120: 81: 28: 23: 22: 15: 12: 11: 5: 1292: 1282: 1281: 1276: 1259: 1258: 1256: 1255: 1244: 1241: 1240: 1238: 1237: 1232: 1227: 1222: 1217: 1212: 1211: 1210: 1205: 1200: 1195: 1190: 1185: 1180: 1175: 1170: 1160: 1155: 1149: 1147: 1143: 1142: 1140: 1139: 1134: 1129: 1124: 1118: 1116: 1110: 1109: 1107: 1106: 1101: 1096: 1091: 1086: 1081: 1076: 1071: 1066: 1061: 1056: 1051: 1046: 1045: 1044: 1034: 1029: 1024: 1019: 1014: 1009: 1004: 999: 994: 989: 984: 979: 974: 969: 964: 959: 954: 949: 944: 939: 934: 929: 923: 921: 915: 914: 912: 911: 910: 909: 904: 894: 889: 883: 881: 875: 874: 872: 871: 866: 861: 856: 851: 846: 841: 836: 831: 826: 821: 816: 811: 806: 800: 798: 792: 791: 777: 775: 773: 772: 765: 760: 755: 750: 745: 740: 735: 730: 725: 720: 715: 710: 705: 700: 695: 690: 685: 680: 675: 670: 665: 660: 655: 650: 645: 640: 635: 630: 625: 620: 615: 610: 605: 600: 595: 590: 585: 580: 575: 570: 569: 568: 558: 553: 548: 543: 538: 533: 528: 523: 518: 513: 508: 506:Brackish marsh 503: 498: 493: 488: 486:Barrier island 483: 478: 473: 468: 463: 457: 455: 449: 448: 441: 440: 433: 426: 418: 411: 410: 401: 392: 383: 374: 323: 321: 318: 317: 316: 311: 306: 301: 296: 294:Paleoshoreline 291: 289:Marine terrace 286: 281: 276: 269: 266: 265: 264: 261: 254: 252: 245: 238: 236: 229: 222: 220: 213: 206: 204: 197: 190: 188: 177: 170: 168: 158: 151: 139: 136: 119: 116: 80: 77: 56:wave-cut cliff 48:shore platform 26: 18:Wave-cut notch 9: 6: 4: 3: 2: 1291: 1280: 1277: 1275: 1272: 1271: 1269: 1254: 1246: 1245: 1242: 1236: 1233: 1231: 1228: 1226: 1223: 1221: 1220:Littoral zone 1218: 1216: 1213: 1209: 1206: 1204: 1201: 1199: 1196: 1194: 1191: 1189: 1186: 1184: 1181: 1179: 1176: 1174: 1171: 1169: 1166: 1165: 1164: 1161: 1159: 1156: 1154: 1153:Bulkhead line 1151: 1150: 1148: 1144: 1138: 1135: 1133: 1130: 1128: 1125: 1123: 1120: 1119: 1117: 1115: 1111: 1105: 1102: 1100: 1097: 1095: 1094:Wave shoaling 1092: 1090: 1087: 1085: 1082: 1080: 1077: 1075: 1072: 1070: 1069:Surge channel 1067: 1065: 1062: 1060: 1057: 1055: 1052: 1050: 1047: 1043: 1040: 1039: 1038: 1035: 1033: 1030: 1028: 1025: 1023: 1020: 1018: 1015: 1013: 1010: 1008: 1005: 1003: 1000: 998: 995: 993: 990: 988: 985: 983: 980: 978: 975: 973: 970: 968: 965: 963: 960: 958: 955: 953: 950: 948: 945: 943: 940: 938: 935: 933: 932:Cliffed coast 930: 928: 925: 924: 922: 920: 916: 908: 905: 903: 900: 899: 898: 895: 893: 890: 888: 885: 884: 882: 880: 876: 870: 867: 865: 862: 860: 859:Shingle beach 857: 855: 852: 850: 847: 845: 842: 840: 837: 835: 832: 830: 827: 825: 822: 820: 817: 815: 812: 810: 807: 805: 802: 801: 799: 797: 793: 788: 781: 771: 770: 766: 764: 761: 759: 756: 754: 751: 749: 746: 744: 741: 739: 736: 734: 731: 729: 726: 724: 721: 719: 716: 714: 711: 709: 706: 704: 701: 699: 696: 694: 691: 689: 686: 684: 681: 679: 676: 674: 671: 669: 666: 664: 661: 659: 656: 654: 651: 649: 646: 644: 641: 639: 636: 634: 631: 629: 626: 624: 621: 619: 616: 614: 611: 609: 606: 604: 601: 599: 596: 594: 591: 589: 586: 584: 581: 579: 576: 574: 571: 567: 564: 563: 562: 559: 557: 554: 552: 549: 547: 544: 542: 539: 537: 534: 532: 531:Coastal plain 529: 527: 524: 522: 519: 517: 514: 512: 509: 507: 504: 502: 499: 497: 494: 492: 489: 487: 484: 482: 479: 477: 474: 472: 469: 467: 464: 462: 459: 458: 456: 454: 450: 446: 439: 434: 432: 427: 425: 420: 419: 416: 405: 396: 387: 378: 370: 364: 350:on 2011-01-12 346: 339: 334: 328: 324: 315: 312: 310: 307: 305: 302: 300: 297: 295: 292: 290: 287: 285: 282: 280: 277: 275: 272: 271: 258: 253: 249: 242: 237: 233: 226: 221: 217: 210: 205: 201: 194: 189: 185: 181: 174: 169: 165: 161: 155: 150: 149: 148: 146: 135: 133: 128: 126: 115: 113: 109: 104: 102: 98: 94: 85: 76: 73: 69: 65: 61: 57: 53: 52:coastal bench 49: 45: 37: 32: 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:)

Index

Wave-cut notch

Southerndown
sea cliff
lake
bay
sea

corrosion
hydraulic action
attrition
organisms
niche
isostatic adjustment
earthquakes
saprock
Raised beach and shore platform, Bleik, Norway
Raised beach
Bleik
Shore platforms from Lake Bonneville (Pleistocene), Utah, United States
Lake Bonneville
Pleistocene
Shore platform at St Bees Head, UK
St Bees Head
Jurassic wave-cut platform at Tedbury Camp, southern England
Tedbury Camp
Commonly called a 'rock platform' in Australia, these two examples at Austinmer, N.S.W, are typical of many on the coast of south-eastern Australia.
Austinmer
The rock platform at Long Reef, N.S.W., Australia.
Long Reef

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