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
187:
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.
191:
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
49:
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
167:
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
403:
105:
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
372:
396:
139:
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
349:
The eruption of Soufrière Hills
Volcano, Montserrat, from 1995 to 1999
177:
168:
113:
106:
86:
420:
145:
90:
44:
129:
385:
93:
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:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.