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Lake Mashū

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The Mashu-dake Hiking Course is a trail that goes along the crater rim and to the top of Mount Mashū. The trail leads through forest and grassland for about seven kilometers and takes about 2.5 to 3 hours to hike one way. There are no settlements along the shores of the lake. Access to the lakeshore
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Lake Mashū is surrounded by steep crater walls 200 metres (660 ft) high. It has no significant inlets and no outlet. The lake is one of the clearest in the world and one of the deepest in Japan. On August 1, 1931, the transparency of the water was measured at 41.6 metres (136 ft). Around
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In summer, the surface of Lake Mashū is often obscured by fog. There is usually fog covering around the lake for about 100 days of the year. This has given the lake a reputation for mysteriousness. A local legend says that if you can see the surface of the lake, you will have bad luck.
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was measured 40.5 metres (133 ft). This is the basis for the lake's claim to be the clearest in the world. Since the 1950s the transparency has tended to range between 20 and 30 metres (66 and 98 ft). The loss in transparency is probably due to the introduction of
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by the Japanese. Over time, however, the Japanese began to refer to the lake by the Japanese reading for the neighboring peak, Mount Mashū
1490: 1412: 1135: 1049: 1258: 30: 1645: 890: 1207: 828: 538: 387: 1033: 939: 272: 431:. Ainu language researcher Nagata Housei proposed that that the Japanese name originated from the Ainu Mas-un-to or 1615: 515:
caldera. The eruption that created the current caldera occurred around 7,000 years ago. The last eruption was a
1630: 1620: 1610: 1251: 1197: 841: 1115: 491: 1655: 1640: 1625: 527: 340: 1650: 1635: 1169: 545:, which forms the highest point on the eastern shore. A third volcano neighbors Kamuinupuri. It is 344: 1164: 1244: 1174: 955: 865: 1218: 382: 1143: 931: 923: 165: 135: 81: 1057: 332: 140: 8: 800: 572:. Some rock around the Mashū crater and Mount Nishibetsu is older still, dating from the 363: 77: 847: 1555: 1417: 996: 573: 151: 475:. The Ainu name for this peak, by which it is commonly known today, is Kamuinupuri or 1478: 1029: 966: 935: 293: 1532: 1424: 860: 851:
is based on this lake as the Sinnoh region is a fictionalized version of Hokkaido.
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Explosive eruption of the central vent with pyroclastic flow and caldera collapse
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On the slopes around and above the lake grow a mixture of evergreen forest with
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The following table lists the eruptions of the Mashū volcano and Kamuinupuri.
1604: 1514: 1486: 1467: 1331: 1306: 1301: 1281: 1003:. Akan Tourism Association & Community Development Promotion Organization 970: 786: 512: 504: 496: 404: 321: 118: 105: 1463: 1374: 1591: 1581: 1429: 1379: 1311: 1291: 1336: 831:. Visitors may only view the lake from the designated observation towers. 1545: 1473: 1455: 1389: 1384: 1364: 1341: 1326: 1321: 965:(in Japanese). Center for Global Environmental Research. September 2004. 503:
Mashū formed less than 32,000 years ago. The caldera is the remains of a
479:. The lake also retains its Ainu name in a shortened form, as Kamuyto or 424: 395: 1563: 1296: 930:(Second ed.). Chico, California: Moon Publications, Inc. pp.  408: 152: 533:
Two volcanoes have grown out of the Mashū caldera. Kamuishu Island, a
411:. At the same time, the clarity of Lake Baikal has not been measured. 166: 1522: 1504: 1286: 751: 542: 534: 371: 329: 1087:, Journey of Hokkaidō Place Names—Notes on Ainu Language Place Names 1459: 759: 569: 553: 348: 85: 1024:
Hunt, Paul (1988). "32. Climbing an Active Volcano: Meakan-dake".
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The origin of Lake Mashū's name is unclear. The lake's original
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Crater lake in Akan Mashu National Park, Hokkaido island, Japan
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which rises from the middle of the lake, is one. The other is
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Hiking in Japan: An Adventurer's Guide to the Mountain Trails
818: 468: 352: 89: 1230: 1208:"Mashu: National catalogue of the active volcanoes in Japan" 897:. International Lake Environment Committee. Archived from 594: 1142:. Geological Survey of Japan, AIST. 2007. Archived from 977: 747:
The lake is inhabited by phytoplankton and zooplankton.
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Explosive eruption of a flank vent and caldera collapse
355:. It has been called the clearest lake in the world. 991: 989: 386:Map of Hokkaido showing location of Lake Mashū and 733:1,000,000,000 cubic metres (0.24 cu mi) 639:11,000,000,000 cubic metres (2.6 cu mi) 549:. Mount Nishibetsu probably predates the caldera. 986: 1602: 619:440,000,000 cubic metres (0.11 cu mi) 96: 1096: 530:of 6, the third highest among large volcanoes. 460: 444: 313: 1090: 1080: 454: 438: 307: 1252: 367:View from Viewing Platform No. 1 (July 2008) 1157: 1098:Hokkaidō Chimei no Tabi — Ainugo Chimei Kai 917: 915: 1259: 1245: 921: 1140:Seamless Digital Geological Map of Japan 1128: 912: 817: 490: 381: 370: 362: 552:The main rock type of the volcanoes is 1603: 1019: 1017: 885: 883: 881: 53: 1240: 1071: 963:Cger's Supercomputer Monograph Report 834: 435:This was then rendered as Lake Mashin 418: 1023: 1014: 948: 878: 829:Ministry of the Environment (Japan) 678:Explosive eruption of a flank vent 660:Explosive eruption of a flank vent 519:about 2,000 years ago that dropped 486: 471:for this peak translate roughly as 239:2.86 km (0.69 cu mi) 184:32.4 km (12.5 sq mi) 13: 1266: 922:Bisignani, J. D. (December 1993). 789:have been introduced to the lake. 742: 499:(left) & Mashu Caldera (right) 14: 1667: 1191: 1116:"Large Volcano Explocivity Index" 1585: 1575: 52: 45: 35:Lake Mashū, Japan, during winter 29: 1225:Mashu: Global Volcanism Program 564:or mafic rock, dating from the 1200:- Japan Meteorological Agency 1108: 1042: 526:Mashū volcano is rated with a 1: 1215:- Japan Meteorological Agency 871: 1646:Potentially active volcanoes 1221:- Geological Survey of Japan 1056:. 2024-05-31. Archived from 1001:Highlights: Eastern Hokkaido 956:"GEMS/Water 摩周湖モニタリングデータブック" 827:itself is prohibited by the 427:name was Kintan-kamuy-to or 358: 7: 1097: 1050:"Lake Mashu DATA (摩周湖DATA)" 854: 461: 445: 314: 247:19.8 km (12.3 mi) 10: 1672: 1105:, page 128, (in Japanese). 813: 528:Volcanic Explosivity Index 341:potentially active volcano 294:not a well-defined measure 255:351 m (1,152 ft) 231:211.5 m (694 ft) 223:137.5 m (451 ft) 1572: 1554: 1531: 1513: 1438: 1398: 1350: 1272: 1227:- Smithsonian Institution 1165:"Mashu: Eruptive History" 1091: 1081: 842:Pokémon Diamond and Pearl 560:. The rock is non-alkali 455: 439: 308: 291: 281: 271: 263: 259: 251: 243: 235: 227: 219: 211: 203: 199: 188: 178: 164: 150: 134: 95: 73: 40: 28: 21: 1170:Global Volcanism Program 926:. In Taran March (ed.). 822:Lake Mashū in the winter 727:Uncorrected radiocarbon 429:lake of the mountain god 378:image of the lake (1999) 345:Akan Mashu National Park 215:19 km (4,700 acres) 1616:Endorheic lakes of Asia 1175:Smithsonian Institution 924:"Doto~Eastern Hokkaido" 891:"MASHU-KO (LAKE MASHU)" 541:, a stratovolcano with 207:6 km (3.7 mi) 866:List of lakes in Japan 823: 804:and birch forest with 709:Corrected radiocarbon 671:Corrected radiocarbon 653:Corrected radiocarbon 633:Corrected radiocarbon 613:Corrected radiocarbon 507:, which is actually a 500: 473:scrubbed area mountain 390: 379: 368: 1631:Volcanoes of Hokkaido 1621:Volcanic crater lakes 821: 494: 385: 374: 366: 82:Kushiro Subprefecture 1611:Calderas of Hokkaido 983:NHK World HD Channel 895:World Lakes Database 668:1400 BC ± 100 years 650:2750 BC ± 100 years 610:7400 BC ± 200 years 477:mountain of the gods 801:Abies sachalinensis 724:970 AD ± 100 years 716:Explosive eruption 698:Explosive eruption 686:100 BC ± 500 years 630:6600 BC ± 50 years 622:Explosive eruption 343:. It is located in 115: /  839:Sendoff Spring in 835:In popular culture 824: 769:Daphnia longispina 706:300 AD ± 75 years 574:Middle Pleistocene 501: 433:lake of the gulls. 419:Origin of the name 407:into the lake and 391: 380: 369: 119:43.583°N 144.517°E 1656:Hokkaido Heritage 1641:Holocene calderas 1626:Lakes of Hokkaido 1598: 1597: 1479:Mikata Five Lakes 740: 739: 591:Dating technique 588:Date of eruption 523:over the region. 347:on the island of 300: 299: 267:December to April 252:Surface elevation 1663: 1592:Japan portal 1590: 1589: 1588: 1582:Lakes portal 1580: 1579: 1578: 1421: 1261: 1254: 1247: 1238: 1237: 1233:- Teshikaga Town 1214: 1212: 1203: 1185: 1184: 1182: 1181: 1161: 1155: 1154: 1152: 1151: 1132: 1126: 1125: 1123: 1122: 1112: 1106: 1104: 1103: 1100: 1094: 1093: 1092:北海道 地名の旅—アイヌ語地名解 1086: 1084: 1083: 1075: 1069: 1068: 1066: 1065: 1046: 1040: 1039: 1021: 1012: 1011: 1009: 1008: 993: 984: 981: 975: 974: 960: 952: 946: 945: 919: 910: 909: 907: 906: 887: 861:Tourism in Japan 848:Pokémon Platinum 776:Bosmina coregoni 690:Tephrochronology 582: 581: 566:Late Pleistocene 562:pyroclastic flow 547:Mount Nishibetsu 517:plinian eruption 497:Kussharo Caldera 487:Volcanic caldera 481:lake of the gods 466: 464: 458: 457: 450: 448: 442: 441: 319: 317: 311: 310: 292:Shore length is 168: 167:Primary outflows 154: 130: 129: 127: 126: 125: 120: 116: 113: 112: 111: 108: 98: 56: 55: 49: 33: 19: 18: 1671: 1670: 1666: 1665: 1664: 1662: 1661: 1660: 1651:Parasitic cones 1636:VEI-6 volcanoes 1601: 1600: 1599: 1594: 1586: 1584: 1576: 1574: 1568: 1550: 1527: 1509: 1448:Fuji Five Lakes 1434: 1415: 1394: 1346: 1274:Hokkaido region 1268: 1265: 1210: 1206: 1201: 1194: 1189: 1188: 1179: 1177: 1163: 1162: 1158: 1149: 1147: 1134: 1133: 1129: 1120: 1118: 1114: 1113: 1109: 1101: 1088: 1078: 1076: 1072: 1063: 1061: 1048: 1047: 1043: 1036: 1022: 1015: 1006: 1004: 995: 994: 987: 982: 978: 958: 954: 953: 949: 942: 920: 913: 904: 902: 889: 888: 879: 874: 857: 837: 816: 795:Picea jezoensis 745: 743:Flora and fauna 489: 452: 436: 421: 361: 305: 277:Kamuishu Island 192: countries 153:Primary inflows 124:43.583; 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Retrieved 899:the original 894: 846: 840: 838: 825: 805: 799: 793: 791: 781: 774: 767: 760: 752: 746: 721:Mount Kamui 703:Mount Kamui 683:Mount Kamui 665:Mount Kamui 647:Mount Kamui 578: 551: 532: 525: 502: 480: 476: 472: 432: 428: 422: 413: 392: 325: 302: 301: 285: 244:Shore length 236:Water volume 212:Surface area 172: 158: 1425:Kasumigaura 1416: [ 539:Mount Kamui 396:Lake Baikal 388:Mount Kamui 333:crater lake 282:Settlements 204:Max. length 159:two streams 141:crater lake 122: / 97:Coordinates 60:Lake Mashū 22:Lake Mashū 1605:Categories 1370:Inawashiro 1180:2020-03-23 1150:2010-09-28 1136:"Hokkaido" 1121:2011-03-08 1064:2024-05-31 1007:2008-10-15 905:2008-10-15 872:References 462:Mashū-dake 409:landslides 303:Lake Mashū 228:Max. depth 1452:Kawaguchi 971:1341-4356 543:lava dome 535:lava dome 446:Mashin-ko 359:Hydrology 330:endorheic 145:endorheic 78:Teshikaga 1487:Suigetsu 1468:Yamanaka 1408:Chūzenji 1332:Shikotsu 1307:Kutcharo 1302:Kussharo 1282:Abashiri 855:See also 753:Melosira 585:Volcano 570:Holocene 554:andesite 349:Hokkaido 328:) is an 326:Kamuy-to 315:Mashū-ko 110:144°31′E 86:Hokkaido 74:Location 1541:Nakaumi 1495:Kugushi 1430:Kitaura 1380:Ogawara 1360:Hachirō 1312:Kuttara 1292:Akkeshi 932:805–807 814:Economy 761:Synedra 568:to the 376:Landsat 337:caldera 273:Islands 173:seepage 107:43°35′N 1546:Shinji 1499:Hiruga 1483:Mikata 1474:Hamana 1456:Motosu 1390:Towada 1385:Tazawa 1365:Hibara 1342:Utonai 1327:Saroma 1322:Notoro 1032:  969:  938:  627:Mashū 607:Mashū 558:dacite 521:pumice 467:. The 264:Frozen 1564:Ikeda 1464:Shōji 1420:] 1375:Jūsan 1317:Mashū 1297:Furen 1219:Mashu 1211:(PDF) 1198:Mashu 1082:赤木 三兵 959:(PDF) 798:and 602:Type 469:kanji 353:Japan 339:of a 195:Japan 190:Basin 90:Japan 1523:Biwa 1505:Suwa 1491:Suga 1413:Inba 1337:Tōya 1287:Akan 1030:ISBN 967:ISSN 936:ISBN 845:and 785:and 755:spp. 556:and 425:Ainu 403:and 322:Ainu 286:none 136:Type 1460:Sai 763:sp. 595:VEI 456:摩周岳 440:魔神湖 309:摩周湖 62:摩周湖 24:摩周湖 1607:: 1497:, 1493:, 1489:, 1485:, 1466:, 1462:, 1458:, 1454:, 1418:ja 1173:. 1167:. 1138:. 1095:, 1052:. 1016:^ 999:. 988:^ 961:. 934:. 914:^ 893:. 880:^ 810:. 730:5 636:6 616:4 576:. 483:. 459:, 443:, 351:, 324:: 312:, 143:, 88:, 84:, 80:, 1501:) 1481:( 1470:) 1450:( 1260:e 1253:t 1246:v 1213:. 1183:. 1153:. 1124:. 1102:) 1089:( 1085:) 1079:( 1067:. 1038:. 1010:. 973:. 944:. 908:. 465:) 453:( 449:) 437:( 320:( 318:) 306:( 296:.

Index


Lake Mashū 摩周湖 is located in Japan
Teshikaga
Kushiro Subprefecture
Hokkaido
Japan
43°35′N 144°31′E / 43.583°N 144.517°E / 43.583; 144.517
Type
crater lake
endorheic
Primary inflows
Primary outflows
Catchment area
Basin
Islands
not a well-defined measure
Ainu
endorheic
crater lake
caldera
potentially active volcano
Akan Mashu National Park
Hokkaido
Japan


Landsat

Mount Kamui
Lake Baikal

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