About: Koko Guyot

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Koko Guyot (also sometimes known as Kinmei and Koko Seamount) is a 48.1-million-year-old guyot, a type of underwater volcano with a flat top, which lies near the southern end of the Emperor seamounts, about 200 km (124 mi) north of the "bend" in the volcanic Hawaiian-Emperor seamount chain. Pillow lava has been sampled on the north west flank of Koko Seamount, and the oldest dated lava is 40 million years old. Seismic studies indicate that it is built on a 9 km (6 mi) thick portion of the Pacific Plate. The oldest rock from the north side of Koko Seamount is dated at 52.6 and the south side of Koko at 50.4 million years ago. To the southeast of the bend is Kimmei Seamount at 47.9 million years ago and southeast of it, Daikakuji at 46.7.

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  • Koko Guyot (also sometimes known as Kinmei and Koko Seamount) is a 48.1-million-year-old guyot, a type of underwater volcano with a flat top, which lies near the southern end of the Emperor seamounts, about 200 km (124 mi) north of the "bend" in the volcanic Hawaiian-Emperor seamount chain. Pillow lava has been sampled on the north west flank of Koko Seamount, and the oldest dated lava is 40 million years old. Seismic studies indicate that it is built on a 9 km (6 mi) thick portion of the Pacific Plate. The oldest rock from the north side of Koko Seamount is dated at 52.6 and the south side of Koko at 50.4 million years ago. To the southeast of the bend is Kimmei Seamount at 47.9 million years ago and southeast of it, Daikakuji at 46.7. (en)
  • 光孝海山(こうこうかいざん)とは、北太平洋の天皇海山群に位置する海山。約4,800万年前に形成されたとされ、その頂上は海面下約301メートルである。 (ja)
  • 光孝海底山(英語:Koko Seamount),又稱光孝海底平頂山,是一座位於太平洋夏威夷-皇帝海山鏈的海底平頂山。 (zh)
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  • 48100000 (xsd:integer)
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  • 1973 (xsd:integer)
dbp:group
  • Isolated (en)
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  • 1.262304E15
dbp:location
  • Central Pacific (en)
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  • Bathymetric of the seamount. Note its wide shape. (en)
dbp:name
  • Koko Guyot (en)
dbp:photo
  • EmperorSeamounts.jpg (en)
dbp:photoCaption
  • Elevation of the Pacific seafloor, showing the Hawaiian-Emperor seamount chain, including Koko Guyot above the prominent bend. The sharp "V" separates the Hawaiian Ridge from the older Emperor Seamount portion of the chain. Koko is the largest of the seamounts directly north of the v-bend. (en)
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  • 35.25 171.58333333333334
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  • Koko Guyot (also sometimes known as Kinmei and Koko Seamount) is a 48.1-million-year-old guyot, a type of underwater volcano with a flat top, which lies near the southern end of the Emperor seamounts, about 200 km (124 mi) north of the "bend" in the volcanic Hawaiian-Emperor seamount chain. Pillow lava has been sampled on the north west flank of Koko Seamount, and the oldest dated lava is 40 million years old. Seismic studies indicate that it is built on a 9 km (6 mi) thick portion of the Pacific Plate. The oldest rock from the north side of Koko Seamount is dated at 52.6 and the south side of Koko at 50.4 million years ago. To the southeast of the bend is Kimmei Seamount at 47.9 million years ago and southeast of it, Daikakuji at 46.7. (en)
  • 光孝海山(こうこうかいざん)とは、北太平洋の天皇海山群に位置する海山。約4,800万年前に形成されたとされ、その頂上は海面下約301メートルである。 (ja)
  • 光孝海底山(英語:Koko Seamount),又稱光孝海底平頂山,是一座位於太平洋夏威夷-皇帝海山鏈的海底平頂山。 (zh)
rdfs:label
  • Koko Guyot (en)
  • 光孝海山 (ja)
  • 光孝海底山 (zh)
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