Where is the earthquake epicenter in Visayas?
Eastern Samar
2019 Visayas earthquake
San Julian, Eastern Samar Show map of Visayas Show map of Philippines Show all | |
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UTC time | 2019-04-23 05:37:51 |
Depth | 54 km (34 mi) |
Epicenter | 11.79°N 125.38°ECoordinates:11.79°N 125.38°E |
Areas affected | Eastern Visayas, Central Visayas, Western Visayas, Bicol Region, Caraga Region |
Where was the epicenter of the Bohol earthquake?
The epicenter of the 1990 Bohol earthquake was located 17 km east of Tagbilaran City with intensities reaching VIII on the Rossi–Forel scale in the town of Jagna, Duero and Guindulman in Bohol (Umbal et al., 1990). The temblor exacted six fatalities with more than 200 injured.
Why is Bohol prone to earthquakes?
But according to the Philippine Institute of Volcanology and Seismology (PHIVOLCS), the 7.2 earthquake may have been caused by a previously undiscovered fault transecting Bohol running ENE-WSW parallel to the island’s northwest coast. This was apparent in the pattern of epicenters of the subsequent aftershocks.
Where are the fault lines in Visayas?
The North Bohol fault is located in Inabanga and near Clarin, the South Offshore fault affects the southern towns, while the East Bohol fault starts at the SW part of Bohol from Loay and goes east towards Pilar….
Bohol Fault System | |
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Region | Central Visayas |
State | Bohol |
Which region in the Philippines are high risk in earthquakes?
The ten provinces most at risk of earthquakes – due to the presence of or their nearness to active faults and trenches – include Surigao del Sur, La Union, Benguet, Pangasinan, Tarlac, Pampanga, Ifugao, Davao Oriental, Nueva Vizcaya and Nueva Ecija (Manila Observatory, 2005).
Which sphere caused the earthquake in Bohol?
East Bohol Fault
An estimated 43,000 people experienced severe shaking, according to the U.S. Geological Survey. The likely culprit is the East Bohol Fault, Solidum said. The East Bohol Fault, which crosses southern Bohol Island, helps relieve some of the tectonic pressure on the Philippines.