Godzilla Megamullion

The Godzilla Megamullion (Japanese: ゴジラ・メガムリオン, romanized: Gojira megamurion) is an undersea Japanese megamullion, or oceanic core complex, 600 kilometres (370 mi) south-east of the island of Okinotorishima in the Philippine Sea. It is about 125 km (78 mi) long by 55 km (34 mi) wide, and is the largest known oceanic core complex in the world. Due to its size it is named after the fictional monster Godzilla, and 14 individual topographic features have been named after Godzilla's body parts.

False-colour elevation map of the western Pacific Ocean
Godzilla Megamullion marked on an elevation map
map showing Izu–Bonin–Mariana Arc ridges running parallel south from Japan, with an extinct spreading ridge parallel between them and the Godzilla Megamullion towards the southern end of that ridge
Map of the Izu–Bonin–Mariana Arc system, with the Godzilla Megamullion in the Parece Vela Basin

Description

The Godzilla Megamullion is 600 kilometres (370 mi) to the south-east of Okinotorishima, the southernmost island of Japan. It is part of the Parece Vela Rift in the Philippine Sea, between Japan and the Philippines in the western Pacific Ocean.[1] The megamullion is dome-shaped, and is named after Godzilla as it is the largest known oceanic core complex, measuring approximately 125 by 55 km (78 by 34 mi),[2] more than ten times the size of the next largest known oceanic core complex. It is also the first known megamullion in a back-arc basin,[3] which is unique as most megamullions form on slow-spreading mid-ocean ridges.[4]

Sampling of the megamullion lithology yielded mostly peridotite, gabbroic rocks, leucocratic rocks, and basalt. The gabbroic rocks and peridotite are present throughout the entire length of the megamullion's flow line, indicating that the megamullion is a detachment fault that exposes the uppermost mantle and lower oceanic crust. The megamullion has abundant plagioclase bearing peridotite.[3]

Discovery and exploration

The Godzilla Megamullion was discovered in 2001 as part of the Continental Shelf Surveys Project of the Hydrographic and Oceanographic Department of Japan, and was first described by Yasuhiko Ohara. It was initially named as the "Giant Megamullion". Since 2001 more than 20 expeditions have explored the megamullion. Due to the large size of the megamullion, when describing features it is often divided into distal, medial, and proximal parts. Names describing Godzilla's body parts have also been given to 14 topographic features (south-west to north-east): West Leg Ridge, South Tail Rise, East Leg Ridge, West Hipbone Rise, North Tail Rise, East Hipbone Rise, West Arm Rise, Backbone Rise, East Arm Rise, West Shoulder Ridge, Neck Peak, East Shoulder Ridge, Head Peak, Hat Ridge.[3]

Naming
Dark night scene with city lights in the background, with a massive dinosaur-like creature stands on hind legs facing tall electrical towers
Godzilla depicted in Godzilla, King of the Monsters! (1956)

The Japan Coast Guard helped to name the megamullion, reaching an agreement with Toho, who own the rights to the character Godzilla. Toho's chief Godzilla officer Keiji Ota stated: "I am truly honored that [the megamullion] bears Godzilla's name, the Earth's most powerful monster."[2]

References
  1. Loocke, M.; Snow, J.E.; Ohara, Y. (2013). "Melt stagnation in peridotites from the Godzilla Megamullion Oceanic Core Complex, Parece Vela Basin, Philippine Sea". Lithos. 182–183: 1–10. Bibcode:2013Litho.182....1L. doi:10.1016/j.lithos.2013.09.005.
  2. "Pacific undersea province given name 'Godzilla Megamullion' | The Asahi Shimbun: Breaking News, Japan News and Analysis". asahi.com. Retrieved 2022-01-15.
  3. Ohara, Yasuhiko (2016). "The Godzilla Megamullion, the largest oceanic core complex on the earth: A historical review". Island Arc. 25 (3): 193–208. doi:10.1111/iar.12116. S2CID 140601539.
  4. Michibayashi, Katsuyoshi; Snow, Jonathan E. (2016). "Virtual special issue: Understanding of the largest oceanic core complex on the Earth, Godzilla Megamullion". Island Arc. 25 (3): 192. doi:10.1111/iar.12157. ISSN 1440-1738. S2CID 132843798.

16°00′N 139°20′E

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