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Major physiographic elements of the Philippine Mobile Belt Puerto Princesa Subterranean River National Park marker describing the geologic history of the Philippines. In the geology of the Philippines, the Philippine Mobile Belt is a complex portion of the tectonic boundary between the Eurasian plate and the Philippine Sea plate, comprising most of the country of the Philippines.
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The Philippine archipelago is bounded by subduction zones which makes the region volcanically active. The most active volcano in the Philippines is the Mayon Volcano located in southeastern Luzon. [36] It is related to the subduction of Philippine Sea plate beneath the Philippine Mobile Belt. [4] Earthquakes (mag >6.0) in the Philippines (2019)
The Philippine fault system is a major inter-related system of geological faults throughout the whole of the Philippine Archipelago, [1] primarily caused by tectonic forces compressing the Philippines into what geophysicists call the Philippine Mobile Belt. [2] Some notable Philippine faults include the Guinayangan, Masbate and Leyte faults.
The National Committee on Geological Sciences was created via Executive order no. 625 on October 8, 1980. This committee is under the Office of the President of the Philippines, which consists of 21 government agencies headed by the Mines and Geosciences Bureau (MGB) of the Department of Environment and Natural Resources (DENR). [1]
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:
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Philippines map of Köppen climate classification zones The Philippines has a tropical maritime climate that is usually hot and humid. There are three seasons: tag-init or tag-araw , the hot dry season or summer from March to May; tag-ulan , the rainy season from June to November; and tag-lamig , the cool dry season from December to February.