Search results
Results From The WOW.Com Content Network
Ancestral Pinatubo is a somma volcano with modern Pinatubo as the new cone. Mount Dorst, to the east, is part of the dip slope of the ancestral Pinatubo. Several mountains near modern Pinatubo are old satellite vents of ancestral Pinatubo, forming volcanic plugs and lava domes. These satellite vents were probably active around the same time as ...
A map of Mount Pinatubo showing nearby peaks and the evacuation zones. In early June, tiltmeter measurements had shown that the volcano was gradually inflating, evidently due to fast-growing amounts of magma filling the reservoir beneath the summit. At the same time, seismic activity, previously concentrated at a depth of a few kilometers below ...
The active volcano Mount Pinatubo is located 26 km (16 mi) west, while Manila is located 75 km (47 mi) to the south. Mount Arayat was officially declared a national park in 1933 and a tourist spot in 1997.
Although the mountains are volcanic in origin, [2] Mount Pinatubo is the only active volcano in the mountain range. Its eruption on June 15, 1991 was the second most powerful volcanic eruption of the 20th century after the 1912 eruption of Novarupta in Alaska.
Lake Pinatubo (Filipino: Lawa ng Pinatubo) is the summit crater lake of Mount Pinatubo formed after its climactic eruption on June 15, 1991. The lake is located in the Zambales Mountains, in Botolan, Zambales, near the boundaries of Pampanga and Tarlac provinces in the Philippines. It is about 90 km (56 mi) northwest of the capital city of Manila.
The following other wikis use this file: Usage on ar.wikipedia.org جبل بيناتوبو; Usage on cs.wikipedia.org Pinatubo; Usage on ja.wikipedia.org
Major events that took place in Pampanga after the People Power revolution include the Mount Pinatubo eruption and the end of the Philippines' Bases Treaty with the United States, which resulted in the closure of Clark Air Base and the later creation of the Clark Freeport and Special Economic Zone.
Several of these (most especially volcanoes) were provided by the PHIVOLCS website). Others were derived mostly from the OpenStreetMap (OSM) database (released under the Open Database License), and a few from GeoNames (released under the Creative Commons attribution license). Notes: if a volcano, may contain the type, as classified by the PHIVOLC