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  2. Pacific plate - Wikipedia

    en.wikipedia.org/wiki/Pacific_Plate

    The plate formed because the triple junction had converted to an unstable form surrounded on all sides by transform faults, due to the development of a kink in one of the plate boundaries. The "Pacific Triangle", the oldest part of the Pacific plate, created during the initial stages of plate formation, is located just east of the Mariana ...

  3. Pacific–Farallon Ridge - Wikipedia

    en.wikipedia.org/wiki/Pacific–Farallon_Ridge

    The East Pacific Rise did not begin its subduction under the North American Plate until 20 million years ago, and the presently surviving portion of the East Pacific Rise is the Pacific-Nazca segment. The present-day spreading from the East Pacific Rise dominates the spreading regime in the Central and South Pacific. [10]

  4. Farallon plate - Wikipedia

    en.wikipedia.org/wiki/Farallon_Plate

    The Farallon plate began subducting under the west coast of the North American plate—then located in modern Utah—as Pangaea broke apart and after the formation of the Pacific plate at the center of the triple junction during the Early Jurassic. It is named for the Farallon Islands, which are located just west of San Francisco, California.

  5. Geology of the Pacific Ocean - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Pacific_Ocean

    The Pacific Ocean evolved in the Mesozoic from the Panthalassic Ocean, which had formed when Rodinia rifted apart around 750 Ma. The first ocean floor which is part of the current Pacific plate began 160 Ma to the west of the central Pacific and subsequently developed into the largest oceanic plate on Earth. [1]

  6. Panthalassa - Wikipedia

    en.wikipedia.org/wiki/Panthalassa

    The Pacific Plate began forming when the triple junction at the center of Panthalassa destabilized about 190 million years ago. Panthalassa , also known as the Panthalassic Ocean or Panthalassan Ocean (from Greek πᾶν "all" and θάλασσα "sea"), [ 1 ] was the vast superocean that encompassed planet Earth and surrounded the ...

  7. Kermadec–Tonga subduction zone - Wikipedia

    en.wikipedia.org/wiki/Kermadec–Tonga_subduction...

    The Tonga plate begins 2,500 km (1,600 mi) NNE of New Zealand and stretches northward, [4] until the plate ends bounded by the Niuafo'ou plate to the northwest and the Pacific plate to the northeast. The Hikurangi Margin is the extension of the Kermadec–Tonga subduction zone further south down the east coast of the North Island.

  8. Geologic timeline of Western North America - Wikipedia

    en.wikipedia.org/wiki/Geologic_timeline_of...

    Northward propagation of the East Pacific Rise into the North American Plate initiates rifting off of the Baja California peninsula. 4 Ma Pliocene Sierra Nevada begins to rise. 3.5 Ma Pliocene The Pacific Plate changes its direction of motion about 11 degrees east of its previous heading, from northwest to the present northwest by north.

  9. Baja California peninsula - Wikipedia

    en.wikipedia.org/wiki/Baja_California_peninsula

    The Baja California peninsula is now part of the Pacific Plate and is moving with it away from the East Pacific Rise in a north northwestward direction. Along the coast north of Santa Rosalia, Baja California Sur is a prominent volcanic activity area. Volcanoes of the peninsula and adjacent islands include: [15] Volcanoes of east-central Baja ...