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Myōjin-shō

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336: 308:(Mita, 1949). As a result of the survey, however, the authors found that both Myōjin-shō and the Bayonnaise Rocks are cones on the somma of a double volcano. The foot of this double volcano lies 1,400 to 1,500 meters in depth and the size is about 30 by 25 kilometers east-west, north-south. The somma is almost a circle in the diameter of 7 by 9 kilometers and the height is 1,000 – 1,400meters. 348: 209: 29: 318:
Myōjin-shō is a post caldera cone formed in the northeastern part of the somma of the double volcano. It is a single conical cone and its height is 550 meters with the shallowest depth 50 meters. A record that suggests a gushing of bubbles near the summit was obtained and micro-earthquakes
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The volcanic eruption from 1952 to 1953 was one of its biggest eruptions on record, with the repetitious appearance and disappearance of an island, which at one point reached over ten metres above sea level, before sinking after a major volcanic eruption in September 1953. On September 24, 1952, a
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Department of the Maritime Safety Agency, was destroyed by the volcano, with the loss of its crew of 31 (including the nine scientists studying the eruption). Consequently, the Department developed
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conducted the survey of the sea area within a radius of about 10 nautical miles (about 18.5 kilometers) but farther than the area of the radius of 3 nautical miles (5.6 km).
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In 1998 and 1999, the Hydrography Department conducted comprehensive sea bottom surveys around Myōjin-shō, using the state-of-the-art survey vessel
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The diameter of the caldera floor is 5.6 kilometers and about 1,100 meters in depth. The central cone is a high formerly known as
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Steam pours from the blocky summit of a lava dome formed at Myōjin-shō during a submarine eruption at the Bayonnaise Rocks volcano in 1952.
231:(Sunfish), an unmanned radio operating survey boat, and has used it for the research of dangerous sea areas such as submarine volcanoes. 494: 464: 499: 66: 288:
conducted a comprehensive survey including the geological and geophysical surveys of sea bottom. Bathymetric survey of
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was carried out by using a "Seabeam 2112" echo sounder at intervals of 0.5 nautical miles (about 930 meters).
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works by the order of preprogrammed instructions and measures depth and water temperature. Bathymetric survey of
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was carried out by using the "PRD-601" echo sounder at intervals of 0.2 nautical miles (about 370 meters).
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A mysterious reef raised a volcanic plume and "Chihuri-class patrol vessel" sailors looked at it (1952)
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were observed near Myōjin-shō, showing that the volcano is still active, although at a low level
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Previously, Myōjin-shō was considered to be the central cone of a double volcano with the
177:. Volcanic activity has been detected there since 1869. Since then it has undergone more 419: 473: 305: 269: 235: 181:, the most powerful of which resulted in the appearance and disappearance of a small 224: 174: 59: 372: 435: 304:(rocks of 9.9 meters in height above the sea level) as a portion of the 88: 75: 125: 234:
This was the first time that volcanic activity had been detected using the
451:"Transpacific detection of Myojin volcanic explosions by underwater sound" 404:"Transpacific Detection of Myojin Volcanic Explosions by Underwater Sound" 200:, the crew of which first witnessed the major volcanic eruption of 1952. 208: 132: 28: 182: 207: 193: 170: 108: 16:
Submarine volcano south of Tokyo on the Izu-Ogasawara Ridge
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conducted the survey of the sea area within a radius of 3
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10.1130/0016-7606(1954)65[941:TDOMVE]2.0.CO;2
131: 119: 114: 104: 65: 55: 50: 42: 21: 188:The name Myōjin-shō derives from a fishing boat, 262:around Myōjin-shō was made for the first time. 158: 8: 510:Former islands from the last glacial maximum 272:(about 5.4 kilometers) of Myōjin-shō. 169:located about 450 kilometers south of 18: 364: 331: 408:Geological Society of America Bulletin 7: 402:Dietz, R. S.; Sheehy, M. J. (1954). 315:, 328 metres below sea level. 173:on the Izu-Ogasawara Ridge in the 14: 346: 334: 27: 485:Seamounts of the Pacific Ocean 1: 139:; 54 years ago 526: 495:Natural disasters in Japan 159: 38: 26: 378:Global Volcanism Program 254:, the second generation 383:Smithsonian Institution 500:1952 natural disasters 213: 46:11 metres (36 ft) 211: 204:Eruption of 1952-1953 465:Survey of Myojin-sho 89:31.9183°N 140.0217°E 420:1954GSAB...65..941D 242:Survey of 1998-1999 198:Shizuoka Prefecture 85: /  214: 490:Ephemeral islands 260:seabed topography 190:No.11 Myōjin-Maru 167:submarine volcano 151: 150: 94:31.9183; 140.0217 517: 452: 450: 448: 447: 438:. Archived from 399: 393: 392: 390: 389: 369: 353:Myōjin-shō, 1952 350: 341:Myōjin-shō, 1952 338: 302:Bayonnaise Rocks 220:Kaiyo Maru No. 5 164: 162: 161: 147: 145: 140: 100: 99: 97: 96: 95: 90: 86: 83: 82: 81: 78: 31: 19: 525: 524: 520: 519: 518: 516: 515: 514: 470: 469: 461: 456: 455: 445: 443: 401: 400: 396: 387: 385: 371: 370: 366: 361: 354: 351: 342: 339: 330: 325: 298: 244: 217:survey vessel, 206: 156: 143: 141: 138: 93: 91: 87: 84: 79: 76: 74: 72: 71: 34: 17: 12: 11: 5: 523: 521: 513: 512: 507: 502: 497: 492: 487: 482: 472: 471: 468: 467: 460: 459:External links 457: 454: 453: 394: 363: 362: 360: 357: 356: 355: 352: 345: 343: 340: 333: 329: 326: 324: 321: 297: 294: 270:nautical miles 243: 240: 205: 202: 149: 148: 135: 129: 128: 123: 117: 116: 112: 111: 106: 102: 101: 69: 63: 62: 57: 53: 52: 48: 47: 44: 40: 39: 36: 35: 32: 24: 23: 15: 13: 10: 9: 6: 4: 3: 2: 522: 511: 508: 506: 505:Postwar Japan 503: 501: 498: 496: 493: 491: 488: 486: 483: 481: 478: 477: 475: 466: 463: 462: 458: 442:on 2012-02-29 441: 437: 433: 429: 425: 421: 417: 413: 409: 405: 398: 395: 384: 380: 379: 374: 368: 365: 358: 349: 344: 337: 332: 328:1952 eruption 327: 322: 320: 316: 314: 309: 307: 303: 295: 293: 291: 287: 283: 279: 275: 271: 267: 263: 261: 257: 253: 249: 241: 239: 237: 236:SOFAR channel 232: 230: 226: 222: 221: 210: 203: 201: 199: 195: 191: 186: 184: 180: 176: 172: 168: 155: 136: 134: 133:Last eruption 130: 127: 124: 122: 118: 113: 110: 107: 103: 98: 70: 68: 64: 61: 58: 54: 49: 45: 41: 37: 30: 25: 20: 444:. Retrieved 440:the original 411: 407: 397: 386:. Retrieved 376: 367: 317: 310: 299: 289: 285: 281: 277: 273: 265: 264: 255: 251: 247: 245: 233: 228: 225:Hydrographic 219: 215: 189: 187: 153: 152: 43:Summit depth 480:Izu Islands 414:(10): 941. 373:"Myojinsho" 175:Izu Islands 92: / 67:Coordinates 60:Izu Islands 474:Categories 446:2009-06-30 388:2018-01-05 359:References 313:Takane-shō 194:Yaizu City 154:Myōjin-shō 22:Myōjin-shō 436:0016-7606 296:Structure 282:Manbou II 278:Manbou II 266:Manbou II 252:Manbou II 179:eruptions 126:lava dome 80:140°1.3′E 77:31°55.1′N 51:Location 416:Bibcode 323:Gallery 223:of the 142: ( 115:Geology 105:Country 434:  256:Manbou 229:Manbou 183:island 306:somma 290:Shoyo 286:Shoyo 274:Shoyo 248:Shoyo 171:Tokyo 165:is a 109:Japan 56:Group 432:ISSN 250:and 144:1970 137:1970 121:Type 424:doi 192:of 160:明神礁 476:: 430:. 422:. 412:65 410:. 406:. 381:. 375:. 238:. 196:, 185:. 449:. 426:: 418:: 391:. 163:) 157:( 146:)

Index


Izu Islands
Coordinates
31°55.1′N 140°1.3′E / 31.9183°N 140.0217°E / 31.9183; 140.0217
Japan
Type
lava dome
Last eruption
submarine volcano
Tokyo
Izu Islands
eruptions
island
Yaizu City
Shizuoka Prefecture

Kaiyo Maru No. 5
Hydrographic
SOFAR channel
seabed topography
nautical miles
Bayonnaise Rocks
somma
Takane-shō
Myōjin-shō, 1952
Myōjin-shō, 1952
"Myojinsho"
Global Volcanism Program
Smithsonian Institution
"Transpacific Detection of Myojin Volcanic Explosions by Underwater Sound"

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