Knowledge (XXG)

Vulcanian eruption

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46: 147: 109:(> 50%). During active periods of volcanic activity, intervals between explosions vary from less than 1 minute (e.g. Anak Krakatoa) to about a day. Pyroclastic flows are also common features of this type of eruption. The gas streaming phase of Vulcanian eruptions are characterised by discrete cannon-like explosions. These expulsions of gas can reach supersonic velocities resulting in shock waves. 65:
which can be extremely noisy due to the rising magma heating water in the ground. This is usually followed by the explosive clearing of the vent and the eruption column is dirty grey to black as old weathered rocks are blasted out of the vent. As the vent clears, further ash clouds become grey-white
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It is believed that water entered due to a partial collapse of the conduit. The water flashed into steam and took the easiest "escape route" via the open conduit. Expansion by contact with the molten magma generated the two very large explosions.
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There were six deaths. Four fishermen died at sea when the avalanches of hot scoria caused the sea to become very disturbed. One person was killed in Stromboli village by falling blocks, and the sixth was killed by the tsunami.
85:. His description of the eruption style is now used all over the world. Mercalli described Vulcanian eruptions as "...Explosions like cannon fire at irregular intervals..." Their explosive nature is due to increased 175:
2 to 2.5 m high was generated. By 10:40 the explosive phase of the eruption was over. Expulsion of lava followed, this flowed down the Sciara del Fuoco, lasting into the night. At the same time incandescent
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Vulcanian eruption: 1 ash plume, 2 lapilli, 3 lava fountain, 4 volcanic ash fall, 5 volcanic bomb, 6 lava flow, 7 layers of lava and ash, 8 stratum, 9 sill, 10 magma conduit, 11 magma chamber, 12 dike
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was a Vulcanian eruption. It started at 08:10 hours (local), when ash was vented for about 10 minutes. Then at 09:52 two incredibly powerful explosions occurred which shook the whole
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Vulcanian eruptions display several common characteristics. The mass of rock ejected during the eruption is usually between 10 and 10 tonnes and contains a high proportion of
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are common products of this type of eruption. These are initially molten blobs of lava, which rapidly cool into blocks often 2 to 3 m across. At
143:, a Vulcanian eruption ejected bombs which struck several volcanologists who were in the crater, some of whom died or suffered severe injuries. 389: 61:
characterized by a dense cloud of ash-laden gas exploding from the crater and rising high above the peak. They usually commence with
356: 343: 330: 317: 556: 132:. Vulcanian eruptions may throw large metre-size blocks several hundred metres, occasionally up to several kilometres. 412: 97:) is most common. Increasing silica levels increase the viscosity of the magma which means increased explosiveness. 58: 458: 62: 369: 39: 338:, Haraldur Sigurdsson, Bruce Houghton, Stephen R McNutt, Hazel Rymer and John Stix (eds) Academic Press, 351:, T. H. Druitt and B. P. Kokelaar (eds), Geological Society Memoir No. 21. Geological Society (London), 181: 443: 117: 466: 171:. Blocks were hurled about 2 km. These fell out of the sky smashing through buildings etc. A 535: 515: 476: 471: 35: 433: 510: 494: 428: 352: 339: 326: 313: 201: 94: 78: 67: 525: 438: 121: 45: 530: 376: 128:, while the ash covers a large surrounding area. The eruption ends with a flow of viscous 325:, John Guest, Paul Cole, Angus Duncan and David Chester, The Geological Society (London) 135:
Vulcanian eruptions are dangerous to persons within several hundred metres of the vent.
520: 154:. A sense of scale is provided by the tourist visible near the centre of the crater. 550: 136: 125: 146: 381: 164: 486: 17: 172: 151: 140: 82: 66:
and creamy in colour, with convolutions of the ash similar to those of
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The eruption of Soufrière Hills Volcano, Montserrat, from 1995 to 1999
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can be involved, but magma with about 55% or more silica (e.g.
81:, witnessing the 1888–1890 eruptions on the island of 312:, Chris Kilburn and Bill McGuire, Terra Publishing, 503: 485: 457: 419: 30:"Vulcanian" redirects here. For the species in 290:Journal of Volcanology and Geothermal Research 116:is dispersed over a wider area than that from 397: 8: 222:Earthquake Research Institute Tokyo Bulletin 404: 390: 382: 89:content of the magma. Almost all types of 124:and the base surge deposits form an ash 213: 27:Volcanic eruption with dense ash clouds 7: 288:Nairn, I.A. & Self, S.J., 1978, 237:Melson, W.G. & Saenz, R., 1973, 220:Murai, I. & Hosoya, Y., 1964, 184:and entered the sea near Piscità. 163:The 11 September 1930 eruption of 25: 1: 256:Geophysical Research Letters 413:Types of volcanic eruptions 370:Kinds of volcanic eruptions 323:Volcanoes of Southern Italy 573: 254:Stith, J.L. et al., 1977, 159:1930 eruption of Stromboli 29: 336:Encyclopedia of Volcanoes 63:phreatomagmatic eruptions 59:type of volcanic eruption 273:Bulletin of Volcanology 239:Bulletin of Volcanology 40:Vulcan (disambiguation) 155: 50: 38:. For other uses, see 504:Other classifications 149: 118:Strombolian eruptions 107:non-juvenile material 48: 271:Minakami, T., 1950, 557:Vulcanian eruptions 375:2017-12-27 at the 156: 150:The Gran Cratere, 77:was first used by 55:Vulcanian eruption 51: 36:Vulcan (Star Trek) 544: 543: 310:Italian Volcanoes 202:Volcanic eruption 182:Vallonazzo Valley 95:basaltic andesite 79:Giuseppe Mercalli 68:Plinian eruptions 16:(Redirected from 564: 406: 399: 392: 383: 297: 286: 280: 269: 263: 252: 246: 235: 229: 218: 180:flowed down the 122:pyroclastic rock 21: 572: 571: 567: 566: 565: 563: 562: 561: 547: 546: 545: 540: 499: 481: 459:Phreatomagmatic 453: 415: 410: 377:Wayback Machine 366: 306: 304:Further reading 301: 300: 287: 283: 270: 266: 253: 249: 236: 232: 219: 215: 210: 198: 161: 103: 101:Characteristics 43: 28: 23: 22: 15: 12: 11: 5: 570: 568: 560: 559: 549: 548: 542: 541: 539: 538: 533: 528: 523: 518: 513: 507: 505: 501: 500: 498: 497: 491: 489: 483: 482: 480: 479: 474: 469: 463: 461: 455: 454: 452: 451: 446: 441: 436: 431: 425: 423: 417: 416: 411: 409: 408: 401: 394: 386: 380: 379: 365: 364:External links 362: 361: 360: 346: 333: 320: 305: 302: 299: 298: 281: 264: 247: 230: 212: 211: 209: 206: 205: 204: 197: 194: 160: 157: 137:Volcanic bombs 102: 99: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 569: 558: 555: 554: 552: 537: 534: 532: 529: 527: 524: 522: 519: 517: 514: 512: 509: 508: 506: 502: 496: 493: 492: 490: 488: 484: 478: 475: 473: 470: 468: 465: 464: 462: 460: 456: 450: 447: 445: 442: 440: 437: 435: 432: 430: 427: 426: 424: 422: 418: 414: 407: 402: 400: 395: 393: 388: 387: 384: 378: 374: 371: 368: 367: 363: 358: 357:1-86239-098-3 354: 350: 347: 345: 344:0-12-643140-X 341: 337: 334: 332: 331:1-86239-138-6 328: 324: 321: 319: 318:1-903544-04-1 315: 311: 308: 307: 303: 295: 291: 285: 282: 278: 274: 268: 265: 261: 257: 251: 248: 244: 240: 234: 231: 227: 223: 217: 214: 207: 203: 200: 199: 195: 193: 189: 185: 183: 179: 174: 170: 166: 158: 153: 148: 144: 142: 138: 133: 131: 127: 126:volcanic cone 123: 119: 115: 110: 108: 100: 98: 96: 92: 88: 84: 80: 76: 71: 69: 64: 60: 56: 47: 41: 37: 33: 19: 448: 348: 335: 322: 309: 293: 289: 284: 276: 272: 267: 259: 255: 250: 242: 238: 233: 225: 221: 216: 190: 186: 162: 134: 111: 104: 74: 72: 54: 52: 31: 444:Strombolian 467:Subglacial 208:References 536:Subaerial 516:Explosive 477:Surtseyan 472:Submarine 449:Vulcanian 165:Stromboli 75:Vulcanian 73:The term 32:Star Trek 18:Vulcanian 551:Category 511:Effusive 495:Phreatic 487:Phreatic 429:Hawaiian 421:Magmatic 373:Archived 262:, 259–62 245:, 416–37 228:, 203–36 196:See also 526:Lateral 439:Plinian 296:, 39–60 279:, 59–87 173:tsunami 152:Vulcano 141:Galeras 83:Vulcano 531:Limnic 434:Peléan 355:  342:  329:  316:  178:scoria 169:island 120:. The 114:tephra 87:silica 34:, see 521:Flank 91:magma 57:is a 353:ISBN 340:ISBN 327:ISBN 314:ISBN 130:lava 112:The 553:: 292:, 277:10 275:, 243:37 241:, 226:42 224:, 70:. 53:A 405:e 398:t 391:v 359:, 294:3 260:4 258:, 42:. 20:)

Index

Vulcanian
Vulcan (Star Trek)
Vulcan (disambiguation)

type of volcanic eruption
phreatomagmatic eruptions
Plinian eruptions
Giuseppe Mercalli
Vulcano
silica
magma
basaltic andesite
non-juvenile material
tephra
Strombolian eruptions
pyroclastic rock
volcanic cone
lava
Volcanic bombs
Galeras

Vulcano
Stromboli
island
tsunami
scoria
Vallonazzo Valley
Volcanic eruption
ISBN
1-903544-04-1

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