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Ice volcano

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meter to ten meters, with the largest ones located far from the shore. Eruptions over ten meters high have been observed, but it is believed that the height of the eruptions are proportional to the size of the mounds. A single eruption may increase the height of the volcano by several centimeters. When an eruption occurs above 0 Â°C (32 Â°F), however, the water erodes the uplift instead of expanding it. Spacing is determined by the amplitude and direction of the waves. In general, the appearance and number of ice volcanoes change considerably between winters.
131:. Instead, ice volcanoes are created by waves colliding with irregularities at the edge of an ice sheet. The abnormalities concentrate the wave energy in a small area, where the ice is eroded to form a V-shaped channel. Spray, ice, and slush splashing out of the feature create a volcanic cone at the channel's shoreward end. This process takes only a few hours. The lakeward end of the channel may then be sealed by ice, but the volcano may continue to erupt. A wave 38: 1060: 1082: 1071: 162:
is required, so the volcanoes normally form near land. They are found in successive rows, and within one row, the features usually have equal height and spacing. However, when comparing two rows, the height and spacing may be drastically different. Ice volcanoes range in height from less than one
143:, which absorb the wave energy needed for the phenomenon. Nonetheless, they may produce larger cones further out at sea, where the greater depth makes this possible. Formation is more thoroughly suppressed by powerful storms, which erode the ice too fast for mound creation. 146:
One type of ice volcano, known as a "cold spot", does not require waves to break against the edge of an ice shelf. Instead, water and slush erupt through a region of weak ice near the coast and form a mound. This is analogous to a
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The uplifts may attract a number of visitors, but they are dangerous, and experts warn that people may fall through the ice or slip into the cold lake. Ice volcanoes are used by
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of at least one metre (3 ft 3 in) is needed to induce eruptions, so ice volcanoes are rarely active without storm-force winds. Formation near land is suppressed by
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there. The formations are temporary: they are frequently destroyed by storms and warm weather, and once the lake wholly freezes over, eruptions are no longer possible.
69:. The process is wave-driven, with wind providing the energy for the waves to cut through the ice and create formations that loosely mimic the shape and activity of 272: 85:, when the temperature is below freezing and the wind blows onshore with a velocity of at least 25 mph (40 km/h). They are known to reduce 357: 435: 73:. After being ejected into the atmosphere, the liquid water and slush freeze and fall back to the surface, growing the formation. 174:. They are noted for their symmetry. Cold spot volcanoes are particularly symmetrical, but their eruption has not been observed. 1144: 196: 280: 467: 92:
There is no consensus name for this phenomenon. Due to its visual similarity to volcanism and particularly
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may also be erupted. The phenomenon is most often observed along the southern coast of
460: 127:, which are uplifts formed by the compression of ice against a shoreline or another 1139: 839: 314: 251: 96:, the term "ice volcano" is frequently used, but it remains controversial. Unlike 489: 86: 342:
Jeffries, Martin O. (December 29, 2006). "Sea ice". In Rafferty, John P. (ed.).
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Fahnestock, R. K.; Crowley, D. J.; Wilson, M.; Schneider, H. (1973).
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For the extraterrestrial volcanoes in the outer Solar System, see
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Leonard Bryan, M.; Marcus, Melvin G. (September 1972).
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Different types of ice volcanoes have been compared to
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is a conical mound of ice formed over a terrestrial
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Wave-driven mound of ice formed on terrestrial lakes
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Archived from 1106:"Evidence of Cryovolcanism on Titan" 1070: 111:as hunting platforms to search for 13: 404: 364: 14: 1156: 386:Michigan Technological University 123:These features are distinct from 1080: 1069: 1059: 1058: 1098: 271:Burlingame, Liz (2014-03-01). 1: 1145:Snow or ice weather phenomena 177: 118: 7: 195:Swasko, Mick (2015-02-12). 10: 1161: 18: 1053: 1020: 984: 938: 882: 865:Short-track speed skating 810: 762: 753: 612: 526: 500: 483: 257:10.1017/s0022143000022735 155:Appearance and eruptions 475: 344:Encyclopedia Britannica 438:on September 17, 2018. 46: 34: 236:Journal of Glaciology 40: 29: 57:via the eruption of 30:An ice volcano over 961:Iceman (occupation) 432:National Geographic 320:10.14430/arctic2960 277:The Weather Channel 248:1973JGlac..12...93F 513:Crystalline phases 149:geological hotspot 47: 35: 1094: 1093: 1075:Wikimedia Commons 878: 877: 352:cite encyclopedia 1152: 1120: 1119: 1117: 1116: 1102: 1084: 1073: 1072: 1062: 1061: 760: 759: 470: 463: 456: 447: 446: 439: 434:. 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Retrieved 1110:www.usgs.gov 1109: 1100: 870:Tour skating 670:Frost flower 603: 501:Major phases 442: 436:the original 431: 416:Live Science 415: 401: 390:. Retrieved 385: 343: 337: 310: 306: 296: 285:. Retrieved 281:the original 276: 266: 239: 235: 204:. Retrieved 200: 165: 160:Landfast ice 158: 145: 122: 106: 102:hydrothermal 91: 83:Lake Ontario 50: 48: 1040:Pleistocene 754:Ice-related 665:Frost heave 599:Stalactites 424:Nadia Drake 65:through an 51:ice volcano 21:Cryovolcano 1135:Glaciology 1129:Categories 1115:2021-10-13 1086:Wiktionary 1030:Glaciology 985:Other uses 855:Ice racing 850:Ice hockey 825:Iceboating 756:activities 527:Formations 518:Superionic 392:2018-05-25 346:. Chicago. 287:2018-05-26 206:2018-05-25 178:References 109:snowy owls 797:Sculpture 613:Phenomena 133:amplitude 119:Formation 113:waterfowl 79:Lake Erie 71:volcanoes 67:ice shelf 1064:Category 1022:Ice ages 976:Yakhchāl 956:Icehouse 782:Climbing 777:Blocking 772:Blasting 690:Hair ice 640:Crystals 329:40508045 1140:Sea ice 946:Cutting 920:Pykrete 840:Cycling 835:Curling 830:Cricket 802:Skating 792:Rafting 787:Fishing 767:Bathing 710:Nucleus 695:Jacking 674:sea ice 672: ( 604:Volcano 568:calving 566: ( 564:Iceberg 559:Glacier 244:Bibcode 98:geysers 1079:  1068:  1057:  951:Icebox 910:Palace 895:Bridge 812:Sports 730:Slurry 705:Needle 655:Frazil 574:Icicle 534:Anchor 327:  307:Arctic 141:shoals 1002:Cream 992:Chips 971:Trade 905:Igloo 900:Hotel 820:Bandy 745:Storm 735:Slush 725:Shuga 720:Shove 680:Glaze 660:Frost 635:Clear 625:Black 594:Spike 589:Sheet 554:Field 494:water 490:state 487:solid 325:JSTOR 137:reefs 63:slush 59:water 43:Ystad 1012:Pack 1007:Cube 997:Core 966:Pick 939:Work 930:Road 925:Rink 915:Pier 740:Snow 715:Rime 700:NĂ©vĂ© 685:Hail 645:Firn 549:Dune 544:Cave 485:The 358:link 170:and 139:and 129:floe 81:and 61:and 55:lake 890:Bar 650:Fog 584:Sea 579:Jam 539:Cap 492:of 477:Ice 315:doi 252:doi 75:Ice 49:An 1131:: 1108:. 430:. 414:. 384:. 366:^ 354:}} 350:{{ 323:. 311:25 309:. 305:. 275:. 250:. 240:12 238:. 215:^ 199:. 185:^ 151:. 115:. 104:. 1118:. 676:) 570:) 469:e 462:t 455:v 395:. 360:) 331:. 317:: 290:. 260:. 254:: 246:: 209:. 23:.

Index

Cryovolcano

Lake Michigan

Ystad
lake
water
slush
ice shelf
volcanoes
Ice
Lake Erie
Lake Ontario
coastal erosion
cryovolcanism
geysers
hydrothermal
snowy owls
waterfowl
pressure ridges
floe
amplitude
reefs
shoals
geological hotspot
Landfast ice
shield volcanoes
stratovolcanoes

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