The 1994 Mindoro earthquake occurred at 03:15:30 PST on November 15 near Mindoro, Philippines. It had a moment magnitude of 7.1 and a maximum Rossi–Forel of VII (Very strong tremor). It is associated with a 35-kilometer-long (22 mi) …

A decade after the release of the West Valley Fault Atlas for the Greater Metro Manila Area in 2015, the DOST-PHIVOLCS will unveil an active fault atlas for Mindanao - the Central Digos Fault Atlas, on 17 March 2025 at Benrose Park, Digos City, Davao del Sur.

Lubang-Verde Passage fault system – located offshore between Batangas peninsula and Mindoro Island, following the northwest–southeast alignment of Verde and Lubang islands (thus the name) and essentially strike-slip (left-lateral) fault.

Feb 1, 2025 · The NNW-trending Central Mindoro Fault (CMF) is an active oblique left-lateral strike-slip fault as determined from offset morphotectonic features such as spurs and streams.

Jan 20, 2015 · The two main tectonic lineaments in the vicinity of Mindoro are the Manila trench bounding the west and the Sibuyan Verde Passage Fault passing through north and northeast offshore Mindoro (Fig. 2). The Manila trench terminates offshore near west central Mindoro (near Mamburao) and dies out southward as marked by parallel folds and thrusts on ...

Feb 1, 2025 · The NNW-trending Central Mindoro Fault (CMF) is an active oblique left-lateral strike-slip fault as determined from offset morphotectonic features such as spurs and streams.

Nov 15, 1994 · An earthquake with magnitude of 7.1-centered 11 km N22°W of Baco, Mindoro, near Verde Island - generateda local destructive tsunami. In oriental Mindoro, the combined effects of the earthquake and the tsunami killed atotal of 78 people, injured 430, damaged or destroyed 7566 houses in 13 out of 15 municipalities, damaged roads, destroyed or ...

The Lubang-Verde Passage fault system is a major strike-slip fault system located offshore between the Batangas and Mindoro Island in the Philippines. [1]

Feb 27, 2009 · Like the 1990 event, the 1994 Mindoro earthquake produced geologic features such as fault-related ground rupture and secondary ground failures like liquefaction and landslides though these were...

The fault plane extended offshore to the N of Mindoro Island, with its rupture originating S of Verde Island and propagating almost directly south to the inland of Mindoro, thereby accounting for the relatively limited damage area observed on the N of Mindoro.