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Lake Atna

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2254: 66: 36: 97: 435: 2266: 511: 366: 73: 43: 2242: 478:. Wiedmer's research suggested the possibility of Lake Atna being a serial generator of megafloods from glacial dam failures. One such possible flood originated from a catastrophic failure of a glacial dam 61 m (200 ft) in height at Tahneta Pass, located at the eastern end of Matanuska Valley. Wiedmer's maximum estimates of this flood place its size at a 2.0–3.3 × 10 2230: 345:(USGS). Based on sedimentary evidence, he concluded that there was a possibility of a large body of standing water being responsible for the deposits and that this could have been an arm of the sea. Alongside A. C. Spencer in 1901, he concluded – contrary to his earlier hypothesis – that these deposits occurred only in limited areas. This conclusion was supported by 458:, some distance from the Copper River Basin area. Pygmy whitefish are known to exist in remnant lakes of Lake Atna. This offered a clue as to a water connection that may have existed at some time in the past between Lake Atna and Lake George. Wiedmer also observed the presence of large, symmetrical hills in the 541:
origin deposits exist in many areas of the Copper River Basin. All major rivers present today occupy narrow valleys that have cut up to 137 m (449 ft) into the bottom of the basin. Lacustrine sediments of the lake are visible in many river bluffs throughout the basin. Several extant lakes
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into the Tok River, and down the Copper River itself. The Susitna River outburst may have been responsible for a flood three to four times more intense than the Tahneta Pass outburst, at a 7.0–11.3 × 10ms discharge rate. This flood may have discharged nearly twice as much water as the Tahneta Pass
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exist in the basin indicating sustained lake levels at a maximum of 914 m (2,999 ft) above modern sea level and other lower levels including 750 m (2,460 ft), 700 m (2,300 ft), 580 m (1,900 ft), 550 m (1,800 ft) and 490 m (1,610 ft) above
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In 1954, Fred Howard Moffit noted that topographic conditions were favorable for the possibility of a large lake, but that specific evidence was lacking at that time. By 1957, geologists Oscar J. Ferrians and H.R. Schmoll concluded the basin had been resident to a large proglacial lake during the
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indicated that Lake Atna may have been a remnant of an earlier lake called Lake Susitna. This was contradicted by Michael Wiedmer in 2011 who stated that no evidence exists for an independent Lake Susitna. The detailed history of the lake and its extent over time is a highly complex problem, as
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lacustrine, alluvial, and glacial deposits that fill the Copper River Basin. Most of the section seen in this view consists of finely laminated to indistinctly bedded sand, silt, and clay, with or without coarser material, that was deposited in glacial Lake
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forest. During the Wisconsin glaciation, a multitude of glaciers extended into and blocked drainage exits from the Copper River Basin. The lake formed at least as early as 58 ka, during the Pleistocene period as a result of
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Wiedmer's resulting research was published in a 2010 paper titled "Late Quaternary megafloods from Glacial Lake Atna, Southcentral Alaska, U.S.A.", with co-authors from the Quaternary Research Center at the
486:. The velocity estimates of this flood range from a minimum of 13 m/s (29 mph) to 57 m/s (130 mph). The flood released a maximum of 1,400 km (340 cu mi) of water into the 1250: 889: 298:. The lake existed in several forms, with several prominent shorelines observable in modern geology. At its greatest extent, the lake surface area was approximately half the size of modern-day 414:, though it may have periodically topped its glacial dams. The final draining and disappearance of the lake likely happened no later than approximately 9.4 ka through the Copper River Valley. 1006: 1329: 1668: 1301: 1826: 418:
of departing ice sheets and the draining of Lake Atna from the basin remain uncertain, as detailed study of the shorelines in the basin has not been conducted.
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During its early formation, the lake likely had no permanent outlet. The damming glaciers that created the lake became large enough that the lake was
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The highest surface level the lake achieved was 975 m (3,199 ft), based on sedimentation in the northwestern area of the basin. Multiple
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of clay and silt grains in the Anchorage area. The collapse of this stratum caused catastrophic landslides in the Anchorage area during the
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34 m (112 ft) in height, with crests of the dunes 0.8 km (0.50 mi) and more apart. The dunes still exist today.
1359: 382:, the region saw significant tectonic uplift through which the ancestral Copper River maintained its course. Sometime before 40 35: 1231: 671:
Schrader, F. C. (1900). "A Reconnaissance of a Part of Prince William Sound and the Copper River District, Alaska, in 1898".
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modern sea level. At its greatest extent, the lake surface area was approximately half the size of modern-day
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Ferrian, Oscar J. Jr. (1957). "Extensive proglacial lake of Wisconsin Age in the Copper River Basin".
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Wisconsin glaciation. The lake was named Lake Atna by geologist D. J. Nichols of the USGS in 1965.
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Model for Late Wisconsinan Massive Outburst Flooding, Tok River Valley, Northeastern Alaska Range
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along the middle and lower valleys of the river, impounding the lake in the Copper River Basin.
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outburst. The postulated glacial dam height for this flood was 346 m (1,135 ft).
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The bluffs near the confluence of the Gakona and Copper Rivers expose nearly 300 ft of the
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Wiedmer, Michael; Montgomery, David R.; Gillespie, Alan R.; Greenberg, Harvey (2010),
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Wiedmer, Michael; Montgomery, David R.; Gillespie, Alan R.; Greenberg, Harvey (2011).
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region over the span of a week. The intensity of the release was such that it created
1896: 1393: 1320: 1193: 924: 311: 302:, and possibly much larger. The basin of the lake lay within an area bordered by the 291: 2148: 1251:"Facies architecture within a regional glaciolacustrine basin: Copper River, Alaska" 290:, an area roughly centered around 245 km (152 mi) northeast of modern-day 2234: 1989: 1934: 1885: 1870: 1273: 1181: 912: 251: 1216: 2087: 1782: 1729: 1658: 1473: 1378: 487: 447: 399: 392: 383: 283: 279: 193: 161: 1185: 1159:"Late Quaternary megafloods from Glacial Lake Atna, Southcentral Alaska, U.S.A." 916: 2246: 1999: 1994: 1842: 1831: 1811: 1806: 1739: 1714: 1663: 1627: 1622: 1530: 1483: 467: 497:
Other glacial dam outbursts may have occurred down the Susitna River, through
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A Geologic Guide to Wrangell–Saint EliasNational Park and Preserve, Alaska
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Twentieth Annual report of the United States Geological Survey, 1898–1899
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Map showing one of the possible extents (pale green) of ancient Lake Atna
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The Geological Society of America (GSA) 2010 Denver Annual Meeting
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origin. This led Wiedmer to investigate the possibility of a
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contributing to the collapse of structures built above it.
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Lake Atna may have generated several of the largest ever
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The Copper River Basin as it is now, looking east from
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University of Alaska Fairbanks – Geophysical Institute
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Map showing geographic features related to Lake Atna
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undertook a study of the Copper River Basin for the
260: 254: 442:In 2005, Michael Wiedmer, then a biologist at the 223:8,900–24,000 km (3,400–9,300 sq mi) 751: 542:in the basin are remnants of the lake, including 421:In 2006, John Jangala, an archaeologist with the 2283: 1322:Geoarchaeology of Glacial Lakes Susitna and Atna 1217:"Glacial Lake Atna, Copper River Basin, Alaskan" 117: 789: 787: 785: 670: 231:2,300–6,000 km (550–1,440 cu mi) 1360: 1068:Hubbard, Trent D.; Reger, Richard D. (2010). 806: 804: 802: 482:ms (2.0–3.3 million cubic meters per second) 353:deposits in the central region of the basin. 294:. The lake formed, and dispersed, during the 1067: 840: 838: 836: 834: 782: 1039: 1037: 1035: 821: 819: 704: 702: 700: 593: 591: 1367: 1353: 992: 990: 988: 799: 654: 652: 650: 648: 646: 633: 631: 629: 627: 625: 1124: 996: 831: 714: 1214: 1032: 816: 793: 708: 697: 588: 509: 470:down the valley from ancient Lake Atna. 433: 364: 1290: 1248: 1100: 985: 844: 810: 776: 757: 643: 622: 505: 282:that initially formed approximately 58 2284: 770: 760:Geological Society of America Bulletin 720: 1348: 1318: 1307:from the original on 20 February 2017 1203:from the original on 15 December 2017 944: 600:"Spillways of an ancient Alaska lake" 360: 1237:from the original on 31 January 2017 1082:from the original on 31 January 2017 1009:from the original on 1 February 2017 973:from the original on 3 February 2017 739:from the original on 31 January 2017 685:from the original on 31 January 2017 610:from the original on 31 January 2017 429: 239:975 m (3,199 ft) (maximum) 1264:(20–22), Elsevier Inc.: 2237–2279, 426:further investigation is required. 13: 2302:Glacial lakes of the United States 1328:, Alaska Journal of Anthropology, 1125:Stricherz, Vince (29 April 2010). 997:Stricherz, Vince (29 April 2010). 964:Alaska Department of Fish and Game 859:"Searching for signs of Lake Atna" 606:. University of Alaska Fairbanks. 597: 454:. This lake sits near the face of 444:Alaska Department of Fish and Game 14: 2338: 2292:Former lakes of the United States 1230:, U.S. Geological Survey: 85–88, 869:from the original on 23 July 2012 72: 42: 2264: 2252: 2240: 2228: 1332:from the original on 1 July 2021 250: 95: 71: 64: 41: 34: 1224:U.S. Geological Survey Circular 1215:Ferrians, Oscar J. Jr. (1989), 1118: 1106: 1094: 1061: 1049: 1021: 949: 938: 881: 856: 850: 522:. Lake Atna covered this basin. 343:United States Geological Survey 664: 450:which had been collected from 1: 1576:Proglacial lakes of Minnesota 1278:10.1016/S0277-3791(02)00027-6 1172:(3), Elsevier Inc.: 413–424, 581: 446:, was shown the carcass of a 349:in 1905, who had studied the 1249:Bennett, Matthew R. (2002), 1005:. University of Washington. 721:Moffit, Fred Howard (1954). 407:, and possibly much larger. 332: 323:glacial lake outburst floods 286:(thousand years ago) in the 7: 1186:10.1016/j.yqres.2010.02.005 917:10.1016/j.yqres.2010.09.003 569: 10: 2343: 1446:West Siberian Glacial Lake 1258:Quaternary Science Reviews 1149: 1133:. University of Washington 730:Geological Survey Bulletin 16:Prehistoric lake in Alaska 2322:Pleistocene United States 2317:Natural history of Alaska 2223: 2215:List of prehistoric lakes 2207: 2199:Great Tehuelche Paleolake 2141: 2119: 2086: 2018: 1977: 1953: 1924: 1894: 1840: 1796: 1772: 1738: 1608: 1584: 1550: 1543: 1513: 1497: 1461: 1454: 1423: 1407: 1386: 1291:Winkler, Gary R. (2000), 576:List of prehistoric lakes 423:Bureau of Land Management 416:Isostatic rebound effects 235: 227: 219: 215: 175: 167: 155: 116: 106: 94: 85:Show map of North America 28: 23: 1319:Smith, Gerad M. (2019), 476:University of Washington 347:Walter Curran Mendenhall 1669:Lake Houghton (glacial) 1911:Kankakee Outwash Plain 1827:Glacial Lake Sammamish 564:1964 Alaska earthquake 523: 439: 375: 339:Frank Charles Schrader 327:1964 Alaska earthquake 314:to the south, and the 140:62.28444°N 145.75000°W 1876:Lake Jordan (Montana) 1764:Glacial Lake Missoula 1754:Glacial Lake Columbia 1694:Nipissing Great Lakes 1674:Glacial Lake Iroquois 513: 437: 368: 2235:Geography portal 2005:Lake Nantucket Sound 1822:Glacial Lake Russell 506:Remnants and effects 296:Wisconsin glaciation 278:) was a prehistoric 208:depending on period. 145:62.28444; -145.75000 1270:2002QSRv...21.2237B 1178:2010QuRes..73..413W 1166:Quaternary Research 1113:Wiedmer et al. 2010 1056:Wiedmer et al. 2010 1044:Wiedmer et al. 2010 1028:Wiedmer et al. 2010 966:. State of Alaska. 909:2011QuRes..75..303W 897:Quaternary Research 826:Wiedmer et al. 2010 766:(12, part 2): 1726. 659:Wiedmer et al. 2010 638:Wiedmer et al. 2010 316:Talkeetna Mountains 136: /  111:Southcentral Alaska 2247:History portal 1700:Early Lake Ontario 524: 440: 376: 361:Geological history 308:Wrangell Mountains 306:to the north, the 288:Copper River Basin 171:Copper River Basin 55:Show map of Alaska 2297:Geology of Alaska 2279: 2278: 2271:Oceans portal 2137: 2136: 1807:Glacial Lake Hood 1696:(Multiple basins) 1630:(Multiple basins) 1539: 1538: 1394:Lake Makgadikgadi 957:"Pygmy Whitefish" 430:Megaflood history 312:Chugach Mountains 310:to the east, the 292:Anchorage, Alaska 243: 242: 236:Surface elevation 2334: 2327:Proglacial lakes 2269: 2268: 2259:Lakes portal 2257: 2256: 2255: 2245: 2244: 2243: 2233: 2232: 2231: 2111:Lake San Agustín 1990:Lake Connecticut 1935:Lake Monongahela 1886:Lake Musselshell 1871:Lake Great Falls 1548: 1547: 1459: 1458: 1381:and related seas 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2069: 2066: 2064: 2063:Lake Panamint 2061: 2059: 2056: 2054: 2051: 2049: 2046: 2044: 2041: 2039: 2036: 2034: 2033:Lake Corcoran 2031: 2029: 2028:Lake Cahuilla 2026: 2025: 2023: 2021: 2017: 2011: 2008: 2006: 2003: 2001: 1998: 1996: 1993: 1991: 1988: 1986: 1985:Lake Cape Cod 1983: 1982: 1980: 1976: 1970: 1967: 1965: 1962: 1961: 1959: 1956: 1952: 1946: 1943: 1941: 1938: 1936: 1933: 1932: 1930: 1927: 1923: 1917: 1914: 1912: 1909: 1907: 1906:Lake Kankakee 1904: 1903: 1901: 1898: 1893: 1887: 1884: 1882: 1881:Lake McKenzie 1879: 1877: 1874: 1872: 1869: 1867: 1866:Lake Glendive 1864: 1862: 1861:Lake Cut Bank 1859: 1857: 1854: 1852: 1851:Lake Chouteau 1849: 1848: 1846: 1844: 1839: 1833: 1830: 1828: 1825: 1823: 1820: 1818: 1817:Lake Puyallup 1815: 1813: 1810: 1808: 1805: 1804: 1802: 1799: 1795: 1789: 1788:Lake Lahontan 1786: 1784: 1781: 1780: 1778: 1775: 1771: 1765: 1762: 1760: 1757: 1755: 1752: 1750: 1747: 1746: 1744: 1741: 1737: 1731: 1728: 1726: 1723: 1721: 1718: 1716: 1713: 1711: 1708: 1706: 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1225: 1218: 1213: 1199: 1195: 1191: 1187: 1183: 1179: 1175: 1171: 1167: 1160: 1155: 1154: 1132: 1128: 1121: 1115:, p. 417 1114: 1109: 1102: 1097: 1081: 1077: 1073: 1072: 1064: 1058:, p. 421 1057: 1052: 1046:, p. 423 1045: 1040: 1038: 1036: 1029: 1024: 1008: 1004: 1000: 993: 991: 989: 969: 965: 958: 952: 946: 941: 926: 922: 918: 914: 910: 906: 902: 898: 891: 884: 868: 864: 860: 857:Ned, Rozell. 853: 846: 841: 839: 837: 835: 828:, p. 414 827: 822: 820: 813:, p. 121 812: 807: 805: 803: 795: 794:Ferrians 1989 790: 788: 786: 778: 773: 765: 761: 754: 735: 731: 724: 717: 710: 709:Ferrians 1989 705: 703: 701: 681: 674: 667: 661:, p. 422 660: 655: 653: 651: 649: 647: 640:, p. 418 639: 634: 632: 630: 628: 626: 609: 605: 601: 598:Rozell, Ned. 594: 592: 587: 577: 574: 573: 567: 565: 561: 557: 553: 549: 545: 540: 536: 532: 528: 521: 517: 516:Glenn Highway 512: 503: 500: 499:Mentasta Pass 495: 493: 489: 485: 477: 471: 469: 465: 461: 457: 453: 449: 445: 436: 427: 424: 419: 417: 413: 408: 406: 401: 396: 394: 389: 385: 381: 380:Miocene Epoch 372: 367: 358: 354: 352: 348: 344: 340: 330: 328: 324: 319: 318:to the west. 317: 313: 309: 305: 301: 297: 293: 289: 285: 281: 277: 271: 247: 238: 234: 230: 226: 222: 218: 214: 207: 203: 199: 198:Susitna River 195: 191: 189: 185: 184: 182: 180: 174: 170: 166: 163: 160: 158: 154: 149: 121: 115: 112: 109: 105: 98: 93: 67: 37: 27: 22: 19: 2174:Lake Minchin 2128: 2106:Lake Palomas 2096:Lake Alamosa 2068:Lake Russell 1969:Lake Passaic 1749:Lake Allison 1710:Lake Stanley 1705:Lake Saginaw 1639:Lake Chicago 1595:Lake Ojibway 1566:Lake Bassano 1561:Lake Agassiz 1552:Nelson River 1469:Ancylus Lake 1436:Lake Tengger 1431:Lake Bandung 1399:Lake Ptolemy 1334:, retrieved 1321: 1309:, retrieved 1293: 1281:, retrieved 1261: 1257: 1239:, retrieved 1227: 1223: 1205:, retrieved 1169: 1165: 1135:. Retrieved 1130: 1120: 1108: 1101:Bennett 2002 1096: 1084:. Retrieved 1070: 1063: 1051: 1023: 1011:. Retrieved 1002: 975:. Retrieved 963: 951: 940: 928:. Retrieved 900: 896: 883: 871:. Retrieved 862: 852: 847:, p. 81 845:Winkler 2000 811:Winkler 2000 796:, p. 87 777:Bennett 2002 772: 763: 759: 753: 741:. Retrieved 729: 716: 711:, p. 85 687:. Retrieved 666: 612:. Retrieved 603: 552:Tonsina Lake 548:Klutina Lake 544:Tazlina Lake 525: 496: 472: 456:Knik Glacier 441: 420: 409: 405:Lake Ontario 400:strand lines 397: 377: 355: 336: 320: 304:Alaska Range 300:Lake Ontario 275: 245: 244: 228:Water volume 220:Surface area 206:Copper River 168:Part of 18: 2159:Lake Escara 2073:Lake Tecopa 2058:Lake Mojave 2038:Lake Harper 1978:New England 1964:Lake Albany 1945:Teays River 1897:Mississippi 1856:Lake Circle 1798:Puget Sound 1774:Great Basin 1720:Lake Warren 1689:Lake Minong 1684:Lake Maumee 1654:Lake Duluth 1634:Lake Arkona 1610:Great Lakes 1600:Tyrrell Sea 1571:Lake Souris 1376:Pleistocene 452:Lake George 378:During the 351:Pleistocene 143: / 131:145°45′00″W 118:Coordinates 2312:Megafloods 2286:Categories 2194:Lake Tauca 2164:Inca Huasi 2053:Lake Modoc 2048:Lake Manly 2043:Lake Manix 2020:California 2010:Lake Stowe 1940:Lake Tight 1759:Lake Lewis 1725:Lake Wayne 1679:Lake Lundy 1489:Yoldia Sea 1462:Baltic Sea 1408:Antarctica 1336:2 November 1311:19 January 1283:19 January 1241:19 January 1207:19 January 1137:19 January 1086:19 January 1013:19 January 977:19 January 945:Smith 2019 930:19 January 903:(1): 303. 873:19 January 743:19 January 689:19 January 614:19 January 582:References 556:permafrost 539:lacustrine 371:Quaternary 276:Lake Ahtna 128:62°17′04″N 2129:Lake Atna 1649:Lake Dana 1586:James Bay 1505:Lake Komi 1194:129855432 925:128892602 527:Diamicton 468:megaflood 412:endorheic 337:In 1898, 333:Discovery 246:Lake Atna 202:Tok River 188:endorheic 79:Lake Atna 49:Lake Atna 24:Lake Atna 1928:drainage 1899:drainage 1588:drainage 1554:drainage 1441:Mundafan 1330:archived 1302:archived 1232:archived 1198:archived 1131:UW Today 1080:Archived 1007:Archived 1003:UW Today 968:Archived 867:Archived 734:Archived 680:Archived 608:Archived 570:See also 520:Mt. Drum 518:towards 107:Location 2208:Summary 2189:Salinas 1266:Bibcode 1174:Bibcode 1150:Sources 905:Bibcode 863:SitNews 560:stratum 531:glacial 488:Wasilla 464:fluvial 192:Later: 186:Early: 2169:Mataro 2154:Cabana 2121:Alaska 1957:valley 1955:Hudson 1895:Upper 1841:Upper 1800:system 1776:system 1742:system 1498:Russia 1455:Europe 1387:Africa 1192:  923:  550:, and 537:, and 480:  388:spruce 204:, and 2184:Sajsi 1326:(PDF) 1305:(PDF) 1298:(PDF) 1254:(PDF) 1235:(PDF) 1220:(PDF) 1201:(PDF) 1190:S2CID 1162:(PDF) 971:(PDF) 960:(PDF) 921:S2CID 893:(PDF) 737:(PDF) 726:(PDF) 683:(PDF) 676:(PDF) 492:dunes 374:Atna. 2179:Ouki 1926:Ohio 1424:Asia 1338:2019 1313:2017 1285:2017 1243:2017 1228:1026 1209:2017 1139:2017 1088:2017 1015:2017 979:2017 932:2017 875:2017 745:2017 691:2017 616:2017 157:Type 1274:doi 1182:doi 913:doi 2288:: 1272:, 1262:21 1260:, 1256:, 1226:, 1222:, 1196:, 1188:, 1180:, 1170:73 1168:, 1164:, 1129:. 1078:. 1074:. 1034:^ 1001:. 987:^ 962:. 919:. 911:. 901:75 899:. 895:. 865:. 861:. 833:^ 818:^ 801:^ 784:^ 764:68 762:. 728:. 699:^ 645:^ 624:^ 602:. 590:^ 546:, 533:, 529:, 384:ka 329:. 284:ka 258:ɑː 200:, 196:, 1368:e 1361:t 1354:v 1276:: 1268:: 1184:: 1176:: 1141:. 1090:. 1017:. 981:. 934:. 915:: 907:: 877:. 747:. 693:. 618:. 270:/ 267:ə 264:n 261:t 255:ˈ 252:/ 248:(

Index

Historic location of Lake Atna in Alaska, US
Historic location of Lake Atna in Alaska, US
Map showing one of the possible extents (pale green) of ancient Lake Atna
Southcentral Alaska
62°17′04″N 145°45′00″W / 62.28444°N 145.75000°W / 62.28444; -145.75000
Type
Proglacial lake
Primary outflows
endorheic
Matanuska River
Susitna River
Tok River
Copper River
/ˈɑːtnə/
proglacial lake
ka
Copper River Basin
Anchorage, Alaska
Wisconsin glaciation
Lake Ontario
Alaska Range
Wrangell Mountains
Chugach Mountains
Talkeetna Mountains
glacial lake outburst floods
1964 Alaska earthquake
Frank Charles Schrader
United States Geological Survey
Walter Curran Mendenhall
Pleistocene

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