Moro Gulf

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Moro Gulf
Lebak View.jpg
The gulf seen from Lebak
Mindanao relief location map.svg
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Moro Gulf
Location within the Philippines
Philippines relief location map (square).svg
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Moro Gulf
Moro Gulf (Philippines)
Location Mindanao Island
Coordinates 6°51′00″N123°00′00″E / 6.8500°N 123.0000°E / 6.8500; 123.0000
Type Gulf
Etymology Moro
Part of Celebes Sea
Basin  countries Philippines
Settlements

The Moro Gulf is the largest gulf in the Philippines. It is located off the coast of Mindanao Island, and is part of the Celebes Sea. The gulf is one of the country's tuna fishing grounds. [1]

Contents

Geography

The gulf stretches between and is surrounded by the main section of Mindanao on the east, and the Zamboanga Peninsula of Mindanao on the west. The peninsula's major drainage goes towards the gulf. [2]

Sibuguey Bay and Illana Bay are its major bays.

Zamboanga City, which is an international port, is bound by the Gulf and Celebes Sea in the East. [3] Cotabato City, on the eastern coast, is another major port.

Earthquakes

The Moro Gulf is also an area of significant tectonic activity with several fault zones in the region capable of producing major earthquakes and destructive local tsunamis, such as the devastating 1976 Moro Gulf earthquake which killed over 5,000 people and left over 90,000 people homeless as it hit the west coast of Mindanao.

Philippines location map (Mindanao).svg
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Moro Gulf
The two largest 20th century Philippine earthquakes: the 1918 Celebes Sea earthquake (8.3 Mw) and the 1976 Moro Gulf earthquake (8.0 Mw). The relatively large 2002 Mindanao earthquake (7.5 Mw) also occurred in the area. The Moro Gulf, part of the Celebes Sea, is labeled for context.

See also

Related Research Articles

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Mindanao is the second-largest island in the Philippines, after Luzon, and seventh-most populous island in the world. Located in the southern region of the archipelago, the island is part of an island group of the same name that also includes its adjacent islands, notably the Sulu Archipelago. According to the 2020 census, Mindanao had a population of 26,252,442, while the entire island group had an estimated population of 27,021,036.

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<span class="mw-page-title-main">Sibuguey Bay</span> Bay in Mindanao Island, Philippines

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<span class="mw-page-title-main">1976 Moro Gulf earthquake</span> Earthquake in the Philippines

The 1976 Moro Gulf earthquake and tsunami occurred on August 17, 1976, at 00:11 local time near the islands of Mindanao and Sulu, in the Philippines. It measured 8.0 on the moment magnitude scale occurring at a depth of 20 km (12 mi). The earthquake was accompanied by a destructive tsunami that resulted in a majority of the estimated 5,000 to 8,000 fatalities. It was the deadliest and strongest earthquake in the Philippines in 58 years since the 1918 Celebes Sea earthquake.

<span class="mw-page-title-main">Zamboanga City</span> Largest highly-urbanized city in Zamboanga del Sur, Philippines

Zamboanga City, officially the City of Zamboanga or Jambangan in the native Subanon language, is a 1st class highly urbanized city in the Zamboanga Peninsula region of the Philippines. According to the 2020 census, it has a population of 977,234 people. It is the fifth-most populous and third-largest city by land area in the Philippines and also the second most populous in Mindanao after Davao City. It is the commercial and industrial center of the Zamboanga Peninsula Region.

<span class="mw-page-title-main">2002 Mindanao earthquake</span> M-7.5 earthquake in Philippines

The 2002 Mindanao earthquake struck the Philippines at 05:16 Philippine Standard Time on March 6. The world's sixth most powerful earthquake of the year, it registered a magnitude of 7.5 and was a megathrust earthquake. It originated near the Cotabato Trench, a zone of deformation situated between the Philippine Sea Plate and the Sunda Plate, and occurred very near to the Philippines' strongest earthquake for the 20th century, the 1918 Celebes Sea earthquake.

The 1897 Mindanao earthquakes occurred on September 20, 1897, at 19:06 UTC and September 21, 1897, at 05:12 UTC. The estimated epicentres of the two earthquakes are identical, lying just off the southwestern coast of Mindanao in the Philippines, south of Basilan island. The earthquakes were originally given estimated magnitudes of 8.6 and 8.7 on the surface wave magnitude scale by Charles Richter, but these were revised downwards by Katsuyuki Abe to 7.4 and 7.5 Ms, respectively. Contemporary reports noted that with few exceptions, all the masonry buildings in Zamboanga and Basilan were left in ruins.

<span class="mw-page-title-main">1918 Celebes Sea earthquake</span> Earthquake in the Philippines

The 1918 Celebes Sea earthquake occurred on August 15 at 12:18 UTC near the Moro Gulf coast of Mindanao. It had a magnitude of 8.3 on the moment magnitude scale and a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. It triggered a tsunami of up to 7 m in height and the combined effects of the earthquake and tsunami led to the deaths of 52 people.

<span class="mw-page-title-main">Dumanquilas Bay</span> Bay in Mindanao, Philippines

Dumanquilas Bay is an arm of the Moro Gulf on the southern side of the Zamboanga Peninsula in western Mindanao island in the Philippines. It is shared between the provinces of Zamboanga del Sur on the eastern and northern shore, and Zamboanga Sibugay on the western shore. An irregularly shaped peninsula extending to Flecha Point separates it from Pagadian Bay to the east, while to the west, the bay connects with Sibuguey Bay through Canalizo Strait which separates Olutanga island from the mainland of Zamboanga. Politically, it is divided between the Zamboanga del Sur municipalities of Margosatubig, Vincenzo Sagun, Lapuyan and Kumalarang, and the Zamboangay Sibugay municipalities of Buug, Malangas and Alicia.

The Cotabato Trench is an oceanic trench in the Pacific Ocean, off the southwestern coast of Mindanao in the Philippines. Along this trench the oceanic crust of the Sunda Plate beneath the Celebes Sea is being subducted beneath the Philippines Mobile Belt. It forms part of a linked set of trenches along the western side of the Philippines formed over east-dipping subduction zones, including the Manila Trench and the Negros Trench. At its northern end the rate of convergence across this boundary is about 100 mm per year. It is a relatively young structure, forming during the late Miocene to Pliocene. This age is consistent with the estimated age of the sedimentary rocks in the accretionary wedge associated with the trench and the age of adakitic arc rocks on Mindanao thought to date the onset of subduction.

References

  1. Barut, Noel. "National Tuna Fishery Report - Philippines" (PDF). School of Ocean and Earth Science and Technology. Marine Fisheries Research Division National Fisheries Research and Development Institute. Retrieved May 4, 2015.
  2. Carating, Rodelio B. (2014). Soils of the Philippines: World soils book series. Springer Science & Business. p. 61. ISBN   978-9401786829 . Retrieved May 4, 2015.
  3. "ZAMBOANGA PENINSULA". Department of Environment and Natural Resources. Archived from the original on August 15, 2018. Retrieved May 4, 2015.