Pacific Plate

The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At 105 million square kilometres, it is the largest tectonic plate.

The north-eastern side is a divergent boundary with the Explorer Plate, the Juan de Fuca Plate and the Gorda Plate forming respectively the Explorer Ridge, the Juan de Fuca Ridge and the Gorda Ridge. In the middle of the eastern side is a transform boundary with the North American Plate along the San Andreas Fault, and a boundary with the Cocos Plate. The south-eastern side is a divergent boundary with the Nazca Plate forming the East Pacific Rise.

The southern side is a divergent boundary with the Antarctic Plate forming the Pacific-Antarctic Ridge.

The western side, the plate is bounded by the Okhotsk Plate at the Kuril-Kamchatka Trench and the Japan Trench, forms a convergent boundary by subducting under the Philippine Sea Plate creating the Mariana Trench, has a transform boundary with the Caroline Plate, and has a collision boundary with the North Bismarck Plate.

In the south-west, the Pacific Plate has a complex but generally convergent boundary with the Indo-Australian Plate, subducting under it north of New Zealand forming the Tonga Trench and the Kermadec Trench. The Alpine Fault marks a transform boundary between the two plates, and further south the Indo-Australian Plate subducts under the Pacific Plate forming the Puysegur Trench. The southern part of Zealandia, which is to the east of this boundary, is the plate's largest block of continental crust.

The northern side is a convergent boundary subducting under the North American Plate forming the Aleutian Trench and the corresponding Aleutian Islands.

The Pacific Plate contains an interior hot spot forming the Hawaiian Islands.

Hillis and Müller are reported to consider the Bird's Head Plate to be moving in unison with the Pacific Plate. Bird considers them to be unconnected.

Read more about Pacific Plate:  Paleo-geology of The Pacific Plate

Other articles related to "pacific, plates, pacific plate, plate":

Geology Of New Zealand - Astride A Plate Boundary
... New Zealand is currently astride the convergent boundary between the Pacific and Australian Plates ... The Pacific Plate is subducted beneath the Australian Plate from around Samoa and Tonga in the north, through the Tonga Trench, Kermadec Trench, and Hikurangi Trough to the east of the North ... Through most of the South Island, the plates slide past each other, with slight obduction of the Pacific Plate over the Australian Plate, forming the Alpine Fault ...
Okhotsk Plate
... The Okhotsk Plate is a tectonic plate covering the Sea of Okhotsk, the Kamchatka Peninsula, Sakhalin Island and Tōhoku and Hokkaidō in Japan ... It was formerly considered a part of the North American Plate, but recent studies indicate that it is an independent plate, bounded on the north by the North American Plate ... On the east, the plate is bounded by the Pacific Plate at the Kuril-Kamchatka Trench and the Japan Trench, on the south by the Philippine Sea Plate at the Nankai Trough, on the west by ...
Paleo-geology of The Pacific Plate
... The Pacific Plate has the distinction of showing one of the largest areal sections of the oldest members of seabed geology being entrenched into eastern Asian oceanic trenches ... A geologic map of the Pacific Ocean seabed shows not only the geologic sequences, and associated Ring of Fire zones on the ocean's perimeters, but the various ages of the seafloor in a ... The oldest member disappearing by way of the Plate Tectonics cycle is early-Cretaceous (145 to 137 million years ago) ...
Geology Of Nauru
... Nauru is positioned in the Nauru Basin of the Pacific Ocean, on a part of the Pacific Plate that formed at a mid oceanic ridge at 132 Ma ... developed simultaneously with a major Pacific Plate reorganisation ... Nauru is moving at 104 mm per year to the north west along with the underlying Pacific Plate ...
Hawaii Hotspot - Theories - Wilson's Stationary Hotspot Theory
... This "mid-plate" volcanism builds peaks that rise from relatively featureless sea floor, initially as seamounts as later as fully-fledged volcanic islands ... Plate tectonics cause the local tectonic plate (in the case of the Hawaii hotspot, the Pacific Plate) to slowly slide over the hotspot, carrying its volcanoes with it ... serves as a record direction and speed of the Pacific Plate's movement ...

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