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Arabian Plate

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Type
  
Minor

Movement
  
north

Approx. Area
  
5,000,000 km

Speed
  
25–20 mm/year

Arabian Plate Arabian Plate AfricanArabian Tectonic Plates

Features
  
Arabian peninsula, Red Sea, Gulf of Aden, Persian Gulf, Indian Ocean

Arabian plate


The Arabian Plate is a minor tectonic plate in the northern and eastern hemispheres.

Contents

It is one of three continental plates (the African, Arabian, and Indian Plates) that have been moving northward in recent geological history and colliding with the Eurasian Plate. This is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and Zagros Mountains, to the Himalayas and ranges of southeast Asia.

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Shadwell arabian plate 2013


Borders

Arabian Plate FileArabian Plate showing general tectonic and structural features

The Arabian Plate consists mostly of the Arabian peninsula; it extends eastward at the Sinai and the Red Sea and northward to the Levant. The plate borders are:

Arabian Plate Tectonic amp Structure

  • East, with the Indian Plate, at the Owen Fracture Zone
  • South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east
  • West, a left lateral fault boundary with the African Plate called the Dead Sea Transform (DST), and a divergent boundary with the African Plate called the Red Sea Rift which runs the length of the Red Sea;
  • North, complex convergent boundary with the Anatolian Plate and Eurasian Plate.
  • History

    Arabian Plate The influence of Late Cretaceous tectonic processes on sedimentation

    The Arabian Plate was part of the African plate during much of the Phanerozoic Eon (PaleozoicCenozoic), until the Oligocene Epoch of the Cenozoic Era. Red Sea rifting began in the Eocene, but the separation of Africa and Arabia occurred approximately 25 million years ago in the Oligocene, and since then the Arabian Plate has been slowly moving toward the Eurasian Plate. The opening of the Red Sea rift led to extensive volcanic activity. There are large volcanic fields called the Older Harrats, such as Harrat Khaybar and Harrat Rahat, cover large parts of the western Arabian Plate. Some activity still continues especially around Medina, and there are regular eruptions within the Red Sea.

    Arabian Plate Arabian Basin Tectonics SEPM Strata

    The collision between the Arabian Plate and Eurasia is pushing up the Zagros Mountains of Iran. Because the Arabian Plate and Eurasian Plate collide, many cities are in danger such as those in southeastern Turkey (which is on the Arabian Plate). These dangers include earthquakes, tsunamis, and volcanoes.

    Countries

    Arabian Plate httpsworldvolcanoeswikispacescomfileviewKK

    Countries within the plate include Lebanon, Syria, Djibouti, Yemen, Oman, Qatar, Bahrain, Kuwait, Iraq, Saudi Arabia, Jordan, and the United Arab Emirates. Regions include parts of the Southern Denkalya Subregion, the Southeastern Anatolia Region, Awdal and the Khuzestan Province.

    Arabian Plate Arabian Plate Wikipedia

    References

    Arabian Plate Wikipedia