Filipina · Medan gunung api
Gunung Makiling
San Pablo Volcanic Field
- Tipe
- Medan gunung api
- Ketinggian
- 1090 m
- Letusan terakhir
- 1350

- 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 InggrisMount 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
1 tercatatGlosariumGaris waktu rinci
- 1350 (±100 tahun)VEI ?Perkiraan geologi1350 – akhir tidak diketahuiSampaloc Lake
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Tautan eksternal
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