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Mount Apo is the highest mountain peak in the Philippines, with an elevation of 2,954 meters (9,692 ft) above sea level. A large solfataric , dormant stratovolcano , it is part of the Apo-Talomo Mountain Range of Mindanao island.
The following is an incomplete list of mountains in the Philippines. ... Mount Apo † 2,954 m (9,692 ft), ... Located near the Ilocos Sur-Abra-Mountain Province ...
The Apo–Talomo Range (also known as Mount Talomo) or Talomo Mountain Range in the provinces of Davao del Sur and Cotabato on the island of Mindanao contains the Philippines' highest peak: Mount Apo, at (9,692 ft (2,954 m)). [4] Mount Talomo (8,773 ft (2,674 m)) is one of the top 15 highest mountains in the Philippines. In terms of climbing ...
Mouth of the Davao River in Talomo District Mount Apo is the tallest mountain in the Philippines. Davao City's land, totaling about 2,443.61 square kilometres (943.48 sq mi), is hilly in the west (the Marilog district) and slopes down to the southeastern shore. Mount Apo, the highest peak in the Philippines, is located at the city's ...
Mount Sicapoo: 2,360 m 7,740 ft 9 IV-A-Calabarzon: Mount Banahaw: 2,177 m 7,142 ft 10 VI-Western Visayas: Mount Madja-as: 2,117 m 6,946 ft 11 III-Central Luzon: Mount Tapulao: 2,037 m 6,683 ft 12 XIII-Caraga: Mount Hilong-hilong: 2,012 m 6,601 ft 13 IX-Zamboanga Peninsula: Mount Pinukis: 1,532 m 5,026 ft 14 VIII-Eastern Visayas: Alto Peak ...
The Philippines is part of a western Pacific arc system characterized by active volcanoes. Among the most notable peaks are Mount Mayon near Legazpi City, Taal Volcano south of Manila, and Mount Apo in Mindanao. All of the Philippine islands are prone to earthquakes.
English: Mount Apo, also known locally as Apo Sandawa, is a large solfataric, dormant stratovolcano on the island of Mindanao, Philippines. With an elevation of 2,954 meters above sea level, it is the highest-mountain in the Philippine Archipelago and 24th-highest peak of an island on Earth.
This is a list of inactive volcanoes in the Philippines. Volcanoes with no record of eruptions are considered as extinct or inactive. Their physical form since their last activity has been altered by agents of weathering and erosion with the formation of deep and long gullies. [ 1 ]