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There are 100 volcanoes in the Philippines listed by the Smithsonian Institution's Global Volcanism Program (GVP) at present, [6] of which 20 are categorized as "historical" and 59 as "Holocene". [6] The GVP lists volcanoes with historical, Holocene eruptions, or possibly older if strong signs of volcanism are still evident through thermal ...
This is a list of potentially active volcanoes in the Philippines, as classified by the Philippine Institute of Volcanology and Seismology. Map all coordinates using OpenStreetMap Download coordinates as:
Similarly, Isarog Volcano, also dormant and part of the Bicol Volcanic Arc, last erupted in 2,374 BCE ± 87 years or 3,500 BCE ± 125 years (5,500 ya ± 125 years) and is now a favored camping destination. Together, these volcanoes contribute to the geological diversity and natural attractions of the Philippines.
Smith Volcano in the Babuyan Islands. The Luzon Volcanic Arc is a chain of volcanoes in a north–south line across the Luzon Strait from Taiwan to Luzon.The name "Luzon Volcanic Arc" was first proposed by Carl Bowin et al. [1] [2] to describe a series of Miocene to recent volcanoes due to eastward subduction along the Manila Trench for approximately 1,200 km from the Coastal Range in Taiwan ...
Mount Makaturing, also known locally as Palaw a Magatoring, is a stratovolcano on Mindanao island in the Philippines. It is located in the province of Lanao del Sur (particularly in the town of Butig) in the Bangsamoro Autonomous Region in Muslim Mindanao. Makaturing has an elevation of 1,940 metres (6,365 ft) and a base diameter of 29 km (18 mi).
A volcanic arc (also known as a magmatic arc [1]: 6.2 ) is a belt of volcanoes formed above a subducting oceanic tectonic plate, [2] with the belt arranged in an arc shape as seen from above. Volcanic arcs typically parallel an oceanic trench , with the arc located further from the subducting plate than the trench.
Andesite and basaltic andesite are the most abundant volcanic rock in island arc which is indicative of the calc-alkaline magmas. Some Island arcs have distributed volcanic series as can be seen in the Japanese island arc system where the volcanic rocks change from tholeiite—calc-alkaline—alkaline with increasing distance from the trench. [15]
The volcanic island is dotted with cinder cones, tuff cones, pyroclastic cones, maars and crater lakes. The highest point in the island is Mount Tumatangas [2] with an elevation of 811 metres (2,661 ft) asl. Bud Dajo has an elevation of 620 metres (2,030 ft) asl. Guimba, Matanding, and Sungal, are some other volcanic cones near Bud Dajo.