Kaldera Masaya
Masaya
Kaldera · Nicaragua · 594 m

- Tipe
- Kaldera
- Negara
- Nicaragua
- Wilayah
- Amerika Tengah & Karibia / Central America Volcanic Arc
- Ketinggian
- 594 m
- Koordinat
- 11.984, -86.169
- Letusan terakhir
- 2026
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
Masaya volcano in Nicaragua has erupted frequently since the time of the Spanish Conquistadors, when an active lava lake prompted attempts to extract the volcano's molten "gold" until it was found to be basalt rock upon cooling. It lies within the massive Pleistocene Las Sierras caldera and is itself a broad, 6 x 11 km basaltic caldera with steep-sided walls up to 300 m high. The caldera is filled on its NW end by more than a dozen vents that erupted along a circular, 4-km-diameter fracture system. The Nindirí and Masaya cones, the source of observed eruptions, were constructed at the southern end of the fracture system and contain multiple summit craters, including the currently active Santiago crater. A major basaltic Plinian tephra erupted from Masaya about 6,500 years ago. Recent lava flows cover much of the caldera floor and there is a lake at the far eastern end. A lava flow from the 1670 eruption overtopped the north caldera rim. Periods of long-term vigorous gas emission at roughly quarter-century intervals have caused health hazards and crop damage.
Ringkasan Wikipedia
Ringkasan InggrisMasaya, also known historically by its aboriginal name Popogatepe in Nawat, is a caldera located in Masaya, Nicaragua, 20 km (12 mi) south of the capital Managua. It is Nicaragua's first and largest national park, and one of 78 protected areas of Nicaragua. The complex volcano is composed of a nested set of calderas and craters, the largest of which is Las Sierras shield volcano and caldera. Within this caldera lies a sub-vent, which is Masaya Volcano sensu stricto. The vent is a shield type composed of basaltic lavas and tephras and includes a summit crater. This hosts Masaya caldera, formed 2,500 years ago by an 8 km3 (1.9 cu mi) basaltic ignimbrite eruption. Inside this caldera a new basaltic complex has grown from eruptions mainly on a semi-circular set of vents that include the Masaya and Nindiri cones. The latter host the pit craters of Masaya, Santiago, Nindiri and San Pedro. Observations in the walls of the pit craters indicate that there have been several episodes of cone and pit crater formation.
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Riwayat letusan
Garis waktu rinci
- 2015VEI 1Teramati2015-10-03 – 2026-03-31Santiago crater
- 2013VEI 0Teramati2013-04-11 – 2013-04-26
- 2012VEI 1Teramati2012-04-30 – 2012-06-08Santiago Crater
- 2008VEI 1Teramati2008-04-29 – 2008-12-17Santiago
- 2006VEI 1Teramati2006-08-04 – 2006-10-25Santiago
- 2005VEI 1Teramati2005-03-04 – 2005-03-30Santiago
- 2004VEI 1Perkiraan geologi2004-07-04 – 2004-07-04Santiago
- 2003VEI 1Teramati2003-09-22 – 2003-12-12Santiago
- 2001VEI 1Teramati2001-04-23 – 2001-04-25Santiago
- 1999VEI 1Teramati1999-11-22 – 2000-03-02Santiago
- 1998VEI 1Teramati1998-09-14 – 1998-09-14Santiago
- 1997VEI 1Teramati1997-06-03 – 1997-11-17Santiago
- 1996VEI 1Teramati1996-12-05 – 1996-12-05Santiago
- 1993VEI 1Teramati1993-06-16 – 1994-11-16Santiago
- 1989VEI 1Teramati1989-02-20 – 1989-11-16Santiago
- 1987VEI 1Teramati1987-02-15 – 1987-02-22Santiago
- 1965VEI 1Teramati1965-10-10 – 1985-04-16Santiago
- 1948VEI 1Teramati1948-09-16 – 1948-09-16Santiago
- 1946VEI 1Teramati1946-06-16 – 1947-12-16Santiago
- 1925VEI 2Teramati1925-04-16 – BerlangsungSantiago
- 1919VEI 2Teramati1919-07-02 – 1924-07-02Santiago
- 1918VEI 1Teramati1918-01-16 – BerlangsungSantiago
- 1913VEI 1Teramati1913-07-12 – BerlangsungSantiago
- 1906VEI 2Teramati1906-01-02 – 1906-01-09Santiago and upper NE flank near El Pelón
- 1904VEI 2Teramati1904-05-16 – 1904-06-16Santiago
- 1902VEI 2Teramati1902-07-15 – 1903-11-16Santiago
- 1858VEI ?Perkiraan geologi1858-04-16 – Berlangsung
- 1858VEI 2Teramati1858-11-10 – 1859-03-27Santiago, San Pedro
- 1856VEI 2Teramati1856-12-16 – 1857-01-16Santiago or San Pedro
- 1853VEI 1Teramati1853-04-09 – 1853-09-15Santiago
- 1852VEI 2Teramati1852-06-16 – 1852-07-16Between Masaya and Nindirí Craters
- 1772VEI 2Teramati1772-03-16 – 1772-03-25North side of Old Masaya Crater
- 1670VEI 3Teramati1670 – BerlangsungNindirí
- 1613VEI 0Perkiraan geologi1613 – BerlangsungNindirí
- 1570VEI 0Teramati1570 – 1586Nindirí
- 1551VEI 0Teramati1551 – BerlangsungNindirí
- 1524VEI 0Teramati1524 – 1544Nindirí
- 150VEI 5Perkiraan geologi150 – Berlangsung
- 170 SM (±100 tahun)VEI 5Perkiraan geologiBCE 170 – Berlangsung
- 4050 SMVEI 6Perkiraan geologiBCE 4050 – BerlangsungNW of caldera
Tautan eksternal
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