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Lord Howe Seamount Chain

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which erupted 6.5 million years ago and there are other gaps in relevant knowledge of this hotspot chain. The chain has now been characterised by compositional analysis to be related at 28 million years to the South Rennell Trough spreading center as its potential initiation point with lessening
709:; historically the hotspot for the Lord Howe chain was expected to presently be beneath Flinders Seamount. but is now thought likely to be somewhat to the south of this, possibly beyond the Heemskerck and Zeehaen seamounts. Indeed the dating of this chain has only been as far south as 1457:
Seton, Maria; Williams, Simon; Mortimer, Nick; Meffre, Sebastien; Micklethwaite, Steven; Zahirovic, Sabin (2019-01-22). "Magma production along the Lord Howe Seamount Chain, northern Zealandia".
1398:
Seton, Maria; Williams, Simon; Mortimer, Nick; Meffre, Sebastien; Micklethwaite, Steven; Zahirovic, Sabin (2019). "Magma production along the Lord Howe Seamount Chain, northern Zealandia".
1619:
Knesel, Kurt M.; Cohen, Benjamin E.; Vasconcelos, Paulo M.; Thiede, David S. (August 2008). "Rapid change in drift of the Australian plate records collision with Ontong Java plateau".
718:
being erupted progressively as the younger seamounts of the hot spot were formed. On the Australian mainland, a third north-south sequence of extinct volcanoes (which includes the
1721:
The East Australian, Tasmantid and Lord Howe volcanoes : exploring the origins of three, contemporaneous, parallel chains of volcanism. (PhD thesis and appendix)
368: 1855: 1860: 1580:"Southward Drift of Eastern Australian Hotspots in the Paleomagnetic Reference Frame Is Consistent With Global True Polar Wander Estimates" 419: 1303: 1261: 1051: 965: 875: 832: 791: 750: 918: 1850: 1008: 1219: 1137: 1095: 1178: 412: 666:
of islands (17°S) to Flinders Seamount (34.7°S). It includes the officially named Nova Bank, Argo and Kelso seamounts,
1794:
Quilty, Patrick G. (1993). "Tasmantid and Lord Howe seamounts: biostratigraphy and palaeoceanographic significance".
1835: 573: 1562: 1845: 456: 1362: 719: 702: 648: 40: 604:
The Lord Howe Seamount Chain has been known under a variety of different gazetted names, including the
33: 1803: 1765: 1628: 1591: 1544: 1466: 1407: 1443: 1508: 1367: 722:) is likely to have the same origin. The Lord Howe Seamount Chain includes the following features: 593: 589: 468: 1660: 1490: 663: 1753: 1529: 1652: 1644: 1482: 868: 706: 690: 656: 337: 330: 1811: 1773: 1725: 1636: 1599: 1474: 1415: 911: 710: 686: 651:. The Tasmantid and Lord Howe seamount chains are both broadly within the Tasman basin (the 623: 316: 309: 1840: 1807: 1769: 1632: 1595: 1470: 1411: 1001: 958: 682: 678: 644: 565: 461: 295: 288: 274: 267: 1127:
Dating of seamount top sediments is consistent with expected seamount age progression
1083:
Dating of seamount top sediments is consistent with expected seamount age progression
1829: 1494: 1044: 671: 652: 507: 253: 246: 1664: 659:), and lie on opposite sides of Dampier Ridge (a submerged continental fragment). 636: 482: 1815: 1777: 1604: 1579: 1478: 1419: 1088: 667: 581: 527: 492: 404: 375: 232: 225: 1648: 1486: 1318: 1305: 1276: 1263: 1234: 1221: 1193: 1180: 1152: 1139: 1110: 1097: 1066: 1053: 1023: 1010: 980: 967: 933: 920: 890: 877: 847: 834: 806: 793: 765: 752: 434: 421: 949: 628: 585: 577: 569: 532: 476: 400: 1656: 1719: 522: 517: 502: 497: 487: 1640: 1729: 1701: 1447:. New Zealand Journal of Geology and Geophysics. Vol.13 (1970) 282-291. 553: 537: 512: 1754:"Origin and evolution of Lord Howe Island, southwest Pacific Ocean" 1563:
Plate velocities in hotspot reference frame: electronic supplement
715: 674: 622: 561: 557: 16:
Seamount chain east of Australia that includes Lord Howe Island
1530:
Dampier Ridge, Tasman Sea, as a stranded continental fragment
647:, a deep-sea elevated plateau which is a submerged part of 1533:. Australian Journal of Earth Sciences 41 (1994). 395-406. 701:
The Lord Howe and Tasmantid chains each resulted from the
576:
seamount chains both run north-south through parts of the
643:
The Lord Howe Seamount Chain is on the western slope of
662:
The Lord Howe Seamount Chain extends from north of the
1545:
Biogeography of the Lord Howe Rise region, Tasman Sea
1796:
Alcheringa: An Australasian Journal of Palaeontology
467: 455: 450: 411: 396: 391: 21: 1747: 1745: 1758:Journal of the Geological Society of Australia 1713: 1711: 1548:. Deep-Sea Research Part II 58 (2011) 959–969. 1789: 1787: 8: 1752:McDougall, I; Embleton, B; Stone, D (1981). 1573: 1571: 1393: 1391: 1389: 1387: 1385: 1383: 724: 655:between Lord Howe Rise and the Australian 18: 1696: 1694: 1603: 1702:"GEBCO Undersea Feature Names Gazetteer" 1692: 1690: 1688: 1686: 1684: 1682: 1680: 1678: 1676: 1674: 1556: 1554: 1437: 1435: 1433: 1431: 1429: 1379: 1578:Hansma, Jeroen; Tohver, Eric (2020). 7: 1718:Douglas (Smethurst), Amelia (2022). 705:moving northward over a stationary 386:(yellow are seamounts, red islands) 1444:Morphology of the Tasman sea floor 14: 367: 355: 343: 336: 322: 315: 301: 294: 280: 273: 259: 252: 238: 231: 217: 205: 193: 181: 169: 157: 60: 46: 39: 32: 1560:W. J. Morgan and J. P. Morgan. 1509:"Marine Gazetteer Placedetails" 564:and is one of the two parallel 1856:Seamounts of the Pacific Ocean 1: 1441:Willem J. M. van der Linden, 568:alongside the east coast of 1861:Seamounts of the Tasman Sea 1877: 1584:Frontiers in Earth Science 1816:10.1080/03115519308619487 1778:10.1080/00167618108729154 1605:10.3389/feart.2020.544496 1479:10.1017/S0016756818000912 1420:10.1017/S0016756818000912 26: 1319:17.601454°S 158.748849°E 1277:18.736381°S 158.581567°E 550:Lord Howe Seamount Chain 435:26.376861°S 159.260528°E 384:Lord Howe Seamount Chain 22:Lord Howe Seamount Chain 1851:Volcanoes of Zealandia 1324:-17.601454; 158.748849 1282:-18.736381; 158.581567 1067:26.66667°S 159.41667°E 981:29.56667°S 159.08333°E 934:31.55417°S 159.08500°E 891:31.35417°S 159.25167°E 848:34.59096°S 159.39376°E 807:36.27751°S 159.10809°E 766:36.33855°S 159.52079°E 640: 440:-26.376861; 159.260528 1363:Lord Howe Marine Park 720:Glass House Mountains 703:Indo-Australian Plate 635:to the north west of 626: 614:Lord Howe Rise Guyots 1340:South Rennell Trough 1256:Chesterfield Plateau 1072:-26.66667; 159.41667 986:-29.56667; 159.08333 939:-31.55417; 159.08500 896:-31.35417; 159.25167 853:-34.59096; 159.39376 812:-36.27751; 159.10809 771:-36.33855; 159.52079 726:Lord Howe Seamounts 584:. These chains have 572:; the Lord Howe and 177:Chesterfield Plateau 1808:1993Alch...17...27Q 1770:1981AuJES..28..155M 1641:10.1038/nature07138 1633:2008Natur.454..754K 1596:2020FrEaS...8..489H 1542:Przeslawski et al. 1471:2019GeoM..156.1605S 1459:Geological Magazine 1412:2019GeoM..156.1605S 1400:Geological Magazine 1368:Gifford Marine Park 1315: /  1273: /  1231: /  1190: /  1149: /  1107: /  1063: /  1024:29.45°S 159.11667°E 1020: /  977: /  930: /  887: /  844: /  803: /  786:Heemskerck Seamount 762: /  727: 627:Topographic map of 606:Lord Howe Seamounts 556:. It features many 431: /  1298:Horsehead Seamount 1235:22.18333°S 159.2°E 1153:24.76667°S 159.5°E 1111:25.0°S 159.58333°E 725: 664:Chesterfield group 641: 552:formed during the 165:Horsehead Seamount 1627:(7205): 754–757. 1527:McDougall et al, 1351: 1350: 1029:-29.45; 159.11667 827:Flinders Seamount 657:continental shelf 588:of approximately 546: 545: 351:Flinders Seamount 1868: 1820: 1819: 1791: 1782: 1781: 1749: 1740: 1739: 1737: 1736: 1730:10.7488/era/2805 1715: 1706: 1705: 1698: 1669: 1668: 1616: 1610: 1609: 1607: 1575: 1566: 1558: 1549: 1540: 1534: 1525: 1519: 1518: 1516: 1515: 1505: 1499: 1498: 1465:(9): 1605–1617. 1454: 1448: 1439: 1424: 1423: 1406:(9): 1605–1617. 1395: 1330: 1329: 1327: 1326: 1325: 1320: 1316: 1313: 1312: 1311: 1308: 1288: 1287: 1285: 1284: 1283: 1278: 1274: 1271: 1270: 1269: 1266: 1246: 1245: 1243: 1242: 1241: 1240:-22.18333; 159.2 1236: 1232: 1229: 1228: 1227: 1224: 1205: 1204: 1202: 1201: 1200: 1195: 1191: 1188: 1187: 1186: 1183: 1164: 1163: 1161: 1160: 1159: 1158:-24.76667; 159.5 1154: 1150: 1147: 1146: 1145: 1142: 1122: 1121: 1119: 1118: 1117: 1116:-25.0; 159.58333 1112: 1108: 1105: 1104: 1103: 1100: 1078: 1077: 1075: 1074: 1073: 1068: 1064: 1061: 1060: 1059: 1056: 1035: 1034: 1032: 1031: 1030: 1025: 1021: 1018: 1017: 1016: 1013: 992: 991: 989: 988: 987: 982: 978: 975: 974: 973: 970: 945: 944: 942: 941: 940: 935: 931: 928: 927: 926: 923: 912:Lord Howe Island 902: 901: 899: 898: 897: 892: 888: 885: 884: 883: 880: 859: 858: 856: 855: 854: 849: 845: 842: 841: 840: 837: 818: 817: 815: 814: 813: 808: 804: 801: 800: 799: 796: 777: 776: 774: 773: 772: 767: 763: 760: 759: 758: 755: 745:Zeehaen Seamount 728: 711:Lord Howe Island 687:Lord Howe Island 610:Lord Howe Guyots 542: 479: 446: 445: 443: 442: 441: 436: 432: 429: 428: 427: 424: 377: 371: 364: 359: 358: 352: 347: 346: 340: 333: 326: 325: 319: 312: 310:Lord Howe Island 305: 304: 298: 291: 284: 283: 277: 270: 263: 262: 256: 249: 242: 241: 235: 228: 221: 220: 214: 209: 208: 202: 197: 196: 190: 185: 184: 178: 173: 172: 166: 161: 160: 154: 149: 144: 139: 134: 129: 124: 119: 114: 109: 104: 99: 94: 89: 84: 79: 74: 69: 64: 63: 57: 50: 49: 43: 36: 19: 1876: 1875: 1871: 1870: 1869: 1867: 1866: 1865: 1836:Seamount chains 1826: 1825: 1824: 1823: 1793: 1792: 1785: 1764:(1–2): 155–76. 1751: 1750: 1743: 1734: 1732: 1717: 1716: 1709: 1700: 1699: 1672: 1618: 1617: 1613: 1577: 1576: 1569: 1559: 1552: 1541: 1537: 1526: 1522: 1513: 1511: 1507: 1506: 1502: 1456: 1455: 1451: 1440: 1427: 1397: 1396: 1381: 1376: 1359: 1353: 1333:27.24 ± 0.24 Ma 1323: 1321: 1317: 1314: 1309: 1306: 1304: 1302: 1301: 1281: 1279: 1275: 1272: 1267: 1264: 1262: 1260: 1259: 1239: 1237: 1233: 1230: 1225: 1222: 1220: 1218: 1217: 1198: 1196: 1194:23.25°S 159.5°E 1192: 1189: 1184: 1181: 1179: 1177: 1176: 1157: 1155: 1151: 1148: 1143: 1140: 1138: 1136: 1135: 1115: 1113: 1109: 1106: 1101: 1098: 1096: 1094: 1093: 1071: 1069: 1065: 1062: 1057: 1054: 1052: 1050: 1049: 1028: 1026: 1022: 1019: 1014: 1011: 1009: 1007: 1006: 985: 983: 979: 976: 971: 968: 966: 964: 963: 938: 936: 932: 929: 924: 921: 919: 917: 916: 895: 893: 889: 886: 881: 878: 876: 874: 873: 852: 850: 846: 843: 838: 835: 833: 831: 830: 811: 809: 805: 802: 797: 794: 792: 790: 789: 770: 768: 764: 761: 756: 753: 751: 749: 748: 699: 618:Middleton Chain 602: 566:seamount chains 541: 540: 535: 530: 525: 520: 515: 510: 505: 500: 495: 490: 485: 474: 473: 439: 437: 433: 430: 425: 422: 420: 418: 417: 387: 385: 382: 381: 380: 379: 378: 374: 372: 365: 362: 360: 356: 353: 350: 348: 344: 341: 334: 329: 327: 323: 320: 313: 308: 306: 302: 299: 292: 287: 285: 281: 278: 271: 266: 264: 260: 257: 250: 245: 243: 239: 236: 229: 224: 222: 218: 215: 212: 210: 206: 203: 200: 198: 194: 191: 188: 186: 182: 179: 176: 174: 170: 167: 164: 162: 158: 155: 152: 150: 147: 145: 142: 140: 137: 135: 132: 130: 127: 125: 122: 120: 117: 115: 112: 110: 107: 105: 102: 100: 97: 95: 92: 90: 87: 85: 82: 80: 77: 75: 72: 70: 67: 65: 61: 58: 55: 53: 51: 47: 44: 37: 17: 12: 11: 5: 1874: 1872: 1864: 1863: 1858: 1853: 1848: 1846:Hotspot tracks 1843: 1838: 1828: 1827: 1822: 1821: 1783: 1741: 1707: 1670: 1611: 1567: 1550: 1535: 1520: 1500: 1449: 1425: 1378: 1377: 1375: 1372: 1371: 1370: 1365: 1358: 1355: 1349: 1348: 1346: 1343: 1341: 1337: 1336: 1334: 1331: 1299: 1295: 1294: 1292: 1289: 1257: 1253: 1252: 1250: 1247: 1215: 1211: 1210: 1208: 1206: 1174: 1170: 1169: 1167: 1165: 1133: 1129: 1128: 1125: 1123: 1091: 1085: 1084: 1081: 1079: 1047: 1041: 1040: 1038: 1036: 1004: 1002:Middleton Reef 998: 997: 995: 993: 961: 959:Elizabeth Reef 955: 954: 952: 946: 914: 908: 907: 905: 903: 871: 869:Ball's Pyramid 865: 864: 862: 860: 828: 824: 823: 821: 819: 787: 783: 782: 780: 778: 746: 742: 741: 738: 735: 732: 698: 695: 691:Ball's Pyramid 645:Lord Howe Rise 633:Lord Howe Rise 601: 598: 596:respectively. 544: 543: 536: 531: 526: 521: 516: 511: 506: 501: 496: 491: 486: 481: 480: 471: 465: 464: 462:Seamount chain 459: 453: 452: 448: 447: 415: 409: 408: 398: 394: 393: 389: 388: 383: 373: 366: 361: 354: 349: 342: 335: 331:Ball's Pyramid 328: 321: 314: 307: 300: 293: 289:Elizabeth Reef 286: 279: 272: 268:Middleton Reef 265: 258: 251: 244: 237: 230: 223: 216: 211: 204: 199: 192: 187: 180: 175: 168: 163: 156: 151: 146: 141: 136: 131: 126: 121: 116: 111: 106: 101: 96: 91: 86: 81: 76: 71: 66: 59: 52: 45: 38: 31: 30: 29: 28: 27: 24: 23: 15: 13: 10: 9: 6: 4: 3: 2: 1873: 1862: 1859: 1857: 1854: 1852: 1849: 1847: 1844: 1842: 1839: 1837: 1834: 1833: 1831: 1817: 1813: 1809: 1805: 1802:(1): 27–53}. 1801: 1797: 1790: 1788: 1784: 1779: 1775: 1771: 1767: 1763: 1759: 1755: 1748: 1746: 1742: 1731: 1727: 1723: 1722: 1714: 1712: 1708: 1703: 1697: 1695: 1693: 1691: 1689: 1687: 1685: 1683: 1681: 1679: 1677: 1675: 1671: 1666: 1662: 1658: 1654: 1650: 1646: 1642: 1638: 1634: 1630: 1626: 1622: 1615: 1612: 1606: 1601: 1597: 1593: 1589: 1585: 1581: 1574: 1572: 1568: 1565: 1564: 1557: 1555: 1551: 1547: 1546: 1539: 1536: 1532: 1531: 1524: 1521: 1510: 1504: 1501: 1496: 1492: 1488: 1484: 1480: 1476: 1472: 1468: 1464: 1460: 1453: 1450: 1446: 1445: 1438: 1436: 1434: 1432: 1430: 1426: 1421: 1417: 1413: 1409: 1405: 1401: 1394: 1392: 1390: 1388: 1386: 1384: 1380: 1373: 1369: 1366: 1364: 1361: 1360: 1356: 1354: 1347: 1344: 1342: 1339: 1338: 1335: 1332: 1328: 1300: 1297: 1296: 1293: 1291:28.1 ± 1.0 Ma 1290: 1286: 1258: 1255: 1254: 1251: 1248: 1244: 1216: 1213: 1212: 1209: 1207: 1203: 1199:-23.25; 159.5 1175: 1172: 1171: 1168: 1166: 1162: 1134: 1131: 1130: 1126: 1124: 1120: 1092: 1090: 1087: 1086: 1082: 1080: 1076: 1048: 1046: 1045:Gifford Guyot 1043: 1042: 1039: 1037: 1033: 1005: 1003: 1000: 999: 996: 994: 990: 962: 960: 957: 956: 953: 951: 947: 943: 915: 913: 910: 909: 906: 904: 900: 872: 870: 867: 866: 863: 861: 857: 829: 826: 825: 822: 820: 816: 788: 785: 784: 781: 779: 775: 747: 744: 743: 739: 736: 733: 730: 729: 723: 721: 717: 712: 708: 704: 696: 694: 692: 688: 684: 680: 676: 673: 669: 665: 660: 658: 654: 653:abyssal plain 650: 646: 638: 634: 630: 625: 621: 619: 615: 611: 607: 599: 597: 595: 591: 587: 583: 579: 575: 571: 567: 563: 559: 555: 551: 539: 534: 529: 524: 519: 514: 509: 504: 499: 494: 489: 484: 478: 472: 470: 466: 463: 460: 458: 454: 449: 444: 426:159°15′37.9″E 416: 414: 410: 406: 402: 399: 395: 390: 376: 370: 339: 332: 318: 311: 297: 290: 276: 269: 255: 248: 247:Gifford Guyot 234: 227: 42: 35: 25: 20: 1799: 1795: 1761: 1757: 1733:. Retrieved 1720: 1624: 1620: 1614: 1587: 1583: 1561: 1543: 1538: 1528: 1523: 1512:. Retrieved 1503: 1462: 1458: 1452: 1442: 1403: 1399: 1352: 700: 661: 642: 632: 617: 613: 609: 605: 603: 549: 547: 475:28–6.4  423:26°22′36.7″S 1322: / 1310:158°44′56″E 1280: / 1268:158°34′54″E 1238: / 1226:159°12′00″E 1197: / 1156: / 1144:159°30′00″E 1114: / 1102:159°35′00″E 1070: / 1058:159°25′00″E 1027: / 1015:159°07′00″E 984: / 972:159°05′00″E 948:6.9 to 6.4 937: / 925:159°05′06″E 894: / 882:159°15′06″E 851: / 839:159°23′38″E 810: / 798:159°06′29″E 769: / 757:159°31′15″E 637:New Zealand 469:Age of rock 438: / 413:Coordinates 1830:Categories 1735:2023-03-30 1724:(Thesis). 1514:2017-02-20 1374:References 1307:17°36′05″S 1265:18°44′11″S 1223:22°11′00″S 1141:24°46′00″S 1132:Kelso Bank 1099:25°00′00″S 1089:Capel Bank 1055:26°40′00″S 1012:29°27′00″S 969:29°34′00″S 922:31°33′15″S 879:31°21′15″S 836:34°35′27″S 795:36°16′39″S 754:36°20′19″S 586:longitudes 582:Tasman Sea 363:Heemskerck 226:Capel Bank 213:Kelso Bank 1649:0028-0836 1495:134379148 1487:0016-7568 1214:Nova Bank 1173:Argo Bank 683:Elizabeth 679:Middleton 649:Zealandia 639:labelled. 631:with the 629:Zealandia 600:Geography 578:Coral Sea 574:Tasmantid 570:Australia 201:Argo Bank 189:Nova Bank 1657:18685705 1357:See also 1185:159°30′E 734:Location 731:Seamount 616:and the 560:-capped 397:Location 392:Location 56:500miles 1804:Bibcode 1766:Bibcode 1665:4427792 1629:Bibcode 1592:Bibcode 1590:: 489. 1467:Bibcode 1408:Bibcode 1182:23°15′S 707:hotspot 697:Geology 685:reefs, 672:Gifford 554:Miocene 451:Geology 68:Zeehaen 1841:Guyots 1663:  1655:  1647:  1621:Nature 1493:  1485:  740:Notes 675:guyots 562:guyots 405:Tasman 1661:S2CID 1491:S2CID 1345:28 Ma 1249:23 Ma 716:magma 668:Capel 594:156°E 590:159°E 558:coral 401:Coral 54:800km 1653:PMID 1645:ISSN 1483:ISSN 689:and 681:and 670:and 592:and 580:and 548:The 483:PreꞒ 457:Type 407:seas 403:and 1812:doi 1774:doi 1726:doi 1637:doi 1625:454 1600:doi 1475:doi 1463:156 1416:doi 1404:156 737:Age 1832:: 1810:. 1800:17 1798:. 1786:^ 1772:. 1762:28 1760:. 1756:. 1744:^ 1710:^ 1673:^ 1659:. 1651:. 1643:. 1635:. 1623:. 1598:. 1586:. 1582:. 1570:^ 1553:^ 1489:. 1481:. 1473:. 1461:. 1428:^ 1414:. 1402:. 1382:^ 950:Ma 693:. 677:, 620:. 612:, 608:, 533:Pg 477:Ma 1818:. 1814:: 1806:: 1780:. 1776:: 1768:: 1738:. 1728:: 1704:. 1667:. 1639:: 1631:: 1608:. 1602:: 1594:: 1588:8 1517:. 1497:. 1477:: 1469:: 1422:. 1418:: 1410:: 538:N 528:K 523:J 518:T 513:P 508:C 503:D 498:S 493:O 488:Ꞓ 153:s 148:t 143:n 138:u 133:o 128:m 123:a 118:e 113:S 108:e 103:w 98:o 93:H 88:d 83:r 78:o 73:L

Index

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Capel Bank
Capel Bank
Gifford Guyot
Gifford Guyot
Middleton Reef
Middleton Reef
Elizabeth Reef
Elizabeth Reef
Lord Howe Island
Lord Howe Island
Ball's Pyramid
Ball's Pyramid


Coral
Tasman
Coordinates
26°22′36.7″S 159°15′37.9″E / 26.376861°S 159.260528°E / -26.376861; 159.260528
Type
Seamount chain
Age of rock
Ma
PreꞒ

O
S
D
C

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