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San Salvador (volcano)

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490: 29: 406: 322:. The crater has been nearly filled with a relatively newer edifice, the BoquerĂłn volcano. San Salvador is adjacent to the volcano and the western section of the city actually lies among its slopes. Due to this close proximity, any geological activity of the volcano, whether eruptive or not, has the potential to result in catastrophic destruction and death to the city. Despite this, the volcano is iconic of the city, and several TV and radio antennas are situated on the El Picacho peaks and the crater of Boqueron. El Picacho, the prominent peak is the highest elevation (1,960 meters altitude). 150: 430: 157: 466: 454: 442: 478: 418: 331: 182: 347: 700: 355: 367:
lavas of the older edifice. Around 800 years ago, the present day crater was formed in a violent explosion. The crater, which gives it the present name (BoquerĂłn means "big mouth" in Spanish) is 1.5 km in diameter and 500m deep. Within the crater around the upper walls, crops are cultivated by the locals who live on the volcano.
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The main edifice, known as the BoquerĂłn edifice, formed between 700 and 1,000 years ago, filling up a former caldera. The crescent-shaped ridge on the northeast side of the volcano is a remnant of the caldera rim. The lavas of the BoquerĂłn edifice contain more alkali elements and iron oxide than the
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The magma chamber which the volcano sits upon contains a number of fissures which protrude along the flanks and sides of the volcano. The northwest (N40W) fissure has been the most active recently, with such significant eruptive events, such as the Loma Caldera eruption which buried the ancient
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Sofield. D., Eruptive history and volcanic hazards of Volcan San Salvador, in Rose W.I. et al., Natural Hazards in El Salvador: Bolder, Colorado, Geological Society of America Special Paper 375, pp 147–158.
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Williams, H., and Meyer-Abich, H., 1955 Volcanisim in the southern part of El Salvador: University of California Publication in geological Sciences v. 32 pp1–64
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Fairbrothers G E., Carr M J., and Mayfield F G., Temporal Magmatic Variation at Boqueron Volcano, El Salvador. Contrib. Mineral. Petrol. v 67, pp 1–9 (1978)
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A 1914 postal, with the image of the lagoon in the crater of San Salvador Volcano, El Salvador. The lagoon disappeared when the volcano erupted in 1917
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The San Salvador volcano is instantly recognizable by its distinctive triangular crescent pointed apex, which has a dorsal fin-like shape.
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The massive compound San Salvador (volcano) dominates the landscape west of El Salvador's capital city of San Salvador.
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The massive San Salvador volcano dominates the landscape and skyline west of the city of San Salvador.
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and the eruption of El Playon (1658–71) which buried the town of Nexapa. The citizens relocated to
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caused a flank eruption on the volcano along the N40W fissure. During this eruption, the
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Topographical hazard zonation maps regarding the volcano and the city
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BoquerĂłn crater with Boqueroncito cinder cone visible at the bottom
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San Salvador volcano towering over San Salvador city at night
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Note: volcanoes are ordered from north-west to south-east.
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Caldera. The Pacific Coast is adjacent south of the city
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View of San Salvador Volcano from downtown San Salvador
379:and nowadays the eruption is celebrated annually. 922: 447:San Salvador skyline with the volcano behind it 587: 362:City from San Salvador volcano's highest point 573: 338:is pinned between San Salvador (volcano) and 483:San Salvador Volcano from Cuscatlán Stadium 156: 580: 566: 353: 345: 329: 923: 286:Drive and hike via El BoquerĂłn Highway 561: 394:appeared, christened 'Boqueroncito'. 390:inside the BoquerĂłn evaporated and a 325: 13: 318:situated northwest to the city of 14: 952: 546: 698: 507:List of volcanoes in El Salvador 488: 476: 464: 452: 440: 428: 416: 404: 180: 155: 148: 27: 459:A view of San Salvador volcano. 936:Stratovolcanoes of El Salvador 336:San Salvador Metropolitan Area 16:Complex volcano in El Salvador 1: 512: 59:1,580 m (5,180 ft) 49:1,893 m (6,211 ft) 7: 500: 79:4.08 km (2.54 mi) 10: 957: 589:Central American volcanoes 397: 909: 881: 828: 765: 707: 696: 595: 295:El BoquerĂłn National Park 290: 280: 275: 265: 253: 237: 225: 213: 208: 193: 175: 142: 137: 127: 122: 83: 73: 63: 53: 43: 38: 26: 21: 931:Mountains of El Salvador 525:Global Volcanism Program 655:Santa MarĂ­a/Santiaguito 530:Smithsonian Institution 363: 351: 343: 357: 349: 333: 304:San Salvador Volcano 163:San Salvador Volcano 22:San Salvador Volcano 103: /  863:RincĂłn de la Vieja 364: 352: 344: 39:Highest point 941:Complex volcanoes 918: 917: 913: 630:Cuilapa-Barbarena 300: 299: 107:13.734°N 89.294°W 948: 911: 702: 582: 575: 568: 559: 558: 533: 492: 480: 468: 456: 444: 432: 420: 408: 384:eruption in 1917 382:The most recent 326:BoquerĂłn edifice 186: 184: 183: 159: 158: 152: 118: 117: 115: 114: 113: 108: 104: 101: 100: 99: 96: 69:Cerro El Picacho 31: 19: 18: 956: 955: 951: 950: 949: 947: 946: 945: 921: 920: 919: 914: 905: 877: 824: 761: 703: 694: 591: 586: 549: 518: 515: 503: 496: 493: 484: 481: 472: 469: 460: 457: 448: 445: 436: 433: 424: 421: 412: 409: 400: 328: 306:(also known as 260:Central America 181: 179: 171: 170: 169: 168: 167: 166: 165: 164: 160: 112:13.734; 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Index


Elevation
Prominence
Parent peak
Isolation
Coordinates
13°44′02″N 89°17′38″W / 13.734°N 89.294°W / 13.734; -89.294
Nickname
San Salvador Volcano is located in El Salvador
El Salvador
San Salvador
La Libertad
Age of rock
Pleistocene
Mountain type
Complex
Type of rock
Basalt
Andesite
Volcanic arc
Central America
Last eruption
Normal route
El BoquerĂłn National Park
stratovolcano
San Salvador

San Salvador Metropolitan Area
Lake Ilopango

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