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Filipina · Medan gunung api

Gunung Makiling

San Pablo Volcanic Field

Tipe
Medan gunung api
Ketinggian
1090 m
Letusan terakhir
1350
Gunung Makiling
Public domain · Wikimedia Commons
Tipe
Medan gunung api
Negara
Filipina
Wilayah
Pasifik Barat / Luzon Volcanic Arc
Ketinggian
1090 m
Koordinat
14.120, 121.300
Letusan terakhir
1350
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Trakiandesit / Trakiandesit basaltik
Ringkasan geologi

The San Pablo Volcanic Field, (also known as the Laguna Volcanic Field) lies at the southern end of Laguna de Bay, the largest lake on Luzon Island. The field contains dozens of scoria cones and maars. Three generations of maars are present, with the oldest being sediment-filled and the youngest containing deep lakes. Many of the maars are aligned along a NE-SW trend. Local legends suggest that the youngest maar, 1.2-km-wide Sampaloc Lake, was formed about 500-700 years ago. The high point of the field is the eroded Maquiling (Makiling) andesitic-to-rhyolitic stratovolcano, which has a deep crater whose floor is 480 m below its north rim. Maquiling has several cones, maars, and numerous thermal areas at its northern base; a geothermal project is located on the S flank.

Ringkasan Wikipedia

Ringkasan Inggris

Mount Makiling is an inactive stratovolcano located in the provinces of Laguna and Batangas on the island of Luzon in the Philippines. The mountain rises to an elevation of 1,090 meters (3,580 ft) above mean sea level and is the highest feature of the Laguna Volcanic Field. It is listed as a Stratovolcano of both the Laguna Volcanic Field and the separate Taal caldera by the Global Volcanism Program. The volcano has no recorded historic eruption but volcanism is still evident through geothermal features like mud spring and hot springs. South of the mountain is the Makiling–Banahaw Geothermal Plant. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) classifies the volcano as "Inactive".

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Riwayat letusan

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Ringkasan (VEI dari waktu ke waktu)
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1350~1350 · 1 letusan · VEI maks. ?13501350135113511351

Garis waktu rinci

  1. 1350 (±100 tahun)VEI ?Perkiraan geologi
    1350 – akhir tidak diketahui
    Sampaloc Lake

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