Bohol Fault System

Bohol Fault System, or also known as (BFS), is a reverse fault system in Bohol province, Philippines. This fault system contains two segments: the newly found North Bohol Fault following the 2013 Bohol earthquake,[3] and the East Bohol Fault.

Bohol Fault System
Surface rupture of the North Bohol Fault during the 2013 Bohol earthquake at Inabanga, Bohol
EtymologyBohol
Named byPhilippine Institute of Volcanology and Seismology
Year defined2013
CountryPhilippines
RegionCentral Visayas
StateBohol
CitiesNorth; Loon, Calape, Inabanga, Tubigon, Buenavista, Clarin, Sagbayan, Getafe, Trinidad
East; Loboc, Bilar, Batuan, Carmen
Characteristics
RangeInabanga & Clarin
SegmentsNorth Bohol Fault, East Bohol Fault
Depth30 km (19 mi)
Tectonics
PlatePhilippine Sea Plate and Sunda Plate
StatusActive
Earthquakes1981, 1990, 2013
TypeReverse fault
MovementDextral
AgeGelasian
OrogenyMindanao-Surigao-Davao Orogeny
Volcanic arc/beltBohol Corridor
1981
1990
1990
All known recent magnitude ≥ 6.0 Mw in Bohol. In 1981 (6.0 Mw),[1] a doublet in 1990 (6.8 Mw) near Guindulman.[2] and the well-known 2013 Bohol earthquake (7.2 Mw).

The North Bohol fault is located in Inabanga and near Clarin, while the East Bohol fault passes through the SW part of Bohol at Tagbilaran and goes eastwards.

Bohol fault segments

North Bohol fault

North Bohol fault or Inabanga fault is a reverse fault located at Anonang, Inabanga which was found on 15 October 2013 during the Bohol earthquake. Based on Phivolcs, a new fault occurs only once in a century. The North Bohol fault, shaped as a hanging wall and also known as the "Great Wall of Bohol", became one of the tourist attractions in Bohol province.[4][5]

East Bohol fault

The East Bohol fault is a dominantly strike slip fault located at the southern portion of Bohol province, opposite to the North Bohol fault.[6][7]

Bohol earthquake
Main article: 2013 Bohol earthquake

The 2013 Bohol earthquake was a deadly event which happened on 15 October, striking the provinces of Bohol, Cebu, Negros Oriental, Masbate and Leyte.

The 15 October 2013 magnitude (Mw) 7.2 Bohol earthquake produced an ~50‐km‐long, ~12‐km‐wide northeast trending zone of uplift with an ~8‐km‐long discontinuous ground rupture indicating predominantly reverse‐slip movement on a southeast dipping fault.[8]

Displacement along the northeastern segment of the NBF in Inabanga is significantly larger in the northeast than in the southwest. In the northeast, the displacement is mostly 2 m and reaches a maximum of 5 m, while in the southwest, the displacement is mostly less than 1 m. The maximum and average displacements, which were measured along the nearly continuous approximately 2‐km‐long ground rupture in Sitio Cumayot, Barangay Anonang, Inabanga, are around 5 and 2 m, respectively.[8]

Documentation of the nearly continuous northern terminus of the 2013 Bohol earthquake ground rupture revealed its association to preexisting scarps of the previously unmapped, Quaternary‐active North Bohol Fault. Trenching across the rupture at four sites not only reveals the geometry and kinematics of the fault but also shows at least one or two pre‐2013 surface rupturing events. Onshore geologic mapping and offshore seismic reflection profiles demonstrate the presence of an island‐wide, northeast‐southwest trending fold‐and‐thrust belt through which deformation related to the regional shortening across the Visayan Sea Basin in the central Philippines is likely distributed.[8]

See also

References
  1. "M 6.0 - Bohol, Philippines". United States Geological Survey. Retrieved March 14, 2018.
  2. "M 6.8 - Bohol, Philippines". United States Geological Survey. Retrieved March 14, 2018.,
  3. Camille Diola (October 23, 2013). "Phivolcs discovers new fault system in Bohol quake". philstar.com. STAR Group of Publications. Retrieved 8 August 2016.
  4. "North Bohol fault becomes tourist attraction". news.abs-cbn.com. ABS-CBN Corporation. October 28, 2013. Retrieved 8 August 2016.
  5. "Post-earthquake Bohol: Silver lining after the disaster". Department of Environment and Natural Resources. Archived from the original on 25 January 2017.
  6. Live Science, Becky Oskin (15 October 2013). "What Caused the Deadly Philippines Earthquake?". Archived from the original on 15 October 2013.CS1 maint: ref=harv (link)
  7. Bohol Chronicle, Chito M. Visarra (24 April 2016). "PHIVOLCS warns on quake due to East fault". Archived from the original on 29 April 2016.CS1 maint: ref=harv (link)
  8. Rimando, Jeremy M.; Aurelio, Mario A.; Dianala, John Dale B.; Taguibao, Kristine Joy L.; Agustin, Krissen Marie C.; Berador, Al Emil G.; Vasquez, Adriann A. (2019). "Coseismic Ground Rupture of the 15 October 2013 Magnitude (MW) 7.2 Bohol Earthquake, Bohol Island, Central Philippines". Tectonics. 38 (8): 2558–2580. doi:10.1029/2019TC005503. ISSN 1944-9194.
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