The Arabian Peninsula constitute as the largest part of this plate, hence, its name. The plate is bounded from the southeast by a right-lateral transform fault boundary that extends from the eastern end of the Gulf of Aden to the eastern end of the Makran Mountains, called the Owen Fault. The African-Arabian region is composed of the following tectonic plates: Arabia, Madagascar, Nubia, Seychelles, and Somali (Figure 1). Arrows show the relative direction of plate motion. This plate is sandwiched between the North American and African Plate on the north and west sides. Tyrrhenian. Transform boundaries occur when two plates slide past each other. This spreading center produces many earthquakes along its boundaries with the surrounding plates, such as those along its eastern and northeastern margins that form the Zagros Mountains in Iran or along its northern margins in Turkey, which was hit by a devastating earthquake on August 17, 1999 that claimed the lives of nearly 20,000 people, injured more than 40,000, and displaced over a quarter of a million people, in addition to huge material losses, which was estimated to be in the billions of dollars. The Arabian Plate is important and unique in many ways. Most of these earthquakes occur along the Gulf of Aqaba, the Dead Sea, the middle of the Red Sea, the Gulf of Aden, and along the boundaries between the Arabian and Iranian Plates. There are large volcanic fields called the Older Harrats, such as Harrat Khaybar and Harrat Rahat, cover large parts of the western Arabian Plate. The Nazca Plate has been completed on the map as an example. It moves northeastward as a result of the eruption of magmas along the Red Sea rift, which spreads annually at a rate of approximately 15 mm. [2], The Arabian Plate is the most common designation of the region, although it is also sometimes referred to as the Arab Plate.[3]. It consists of most of Europe, Russia, and parts of Asia. The photos you provided may be used to improve Bing image processing services. "Sizes of Tectonic or Lithospheric Plates", "Plate Boundaries of the Arabian Plate – GEOS 309: Tectonics", "Arabian Plate - African/Arabian Tectonic Plates", "Birth of two volcanic islands in the southern Red Sea", https://en.wikipedia.org/w/index.php?title=Arabian_Plate&oldid=994289561, Short description is different from Wikidata, Articles with disputed statements from May 2017, Creative Commons Attribution-ShareAlike License, This page was last edited on 14 December 2020, at 23:34. Convergent boundaries are … That's where the Eurasian and Arabian Tectonic plates meet and where the Zagros mountain range developed – the location of the latest quake. The tectonic boundary to the Arabian plate and the Zagros range is formed by the Main Zagros Reverse Fault, to the north of which lie once-fragmented microcontinents of Gondwanaland origin. Saudi Arabia is part of the so-called Arabian Plate. It is a rift that is causing sea floor spreading and the expansion of the Red Sea. the plate boundaries. Regions include parts of Awdal (Somalia/Somaliland), the Khuzestan Province (Iran), the Southeastern Anatolia Region (Turkey), and the Southern Denkalya Subregion (Eritrea). The Zagros and Makran Mountains in Iran and the Taurus Mountains in southern Turkey are, respectively, the eastern and northern boundaries of the Arabian Plate, which are classified as convergent plate boundaries that represent the zone of collision between the Arabian Plate and the Eurasian Plate. For some cases, simplified schemes are suggested to explain dynamics of interaction between the in-traplate and plate boundary processes. The western Indo-Arabian boundary is lateral relative to each other giving rise to a transform boundary. Guess the location of the Mid-Atlantic Ridge then check your answer with the teacher. The Arabian Peninsula constitute as the largest part of this plate, hence, its name. It is one of three continental plates (along with the African and Indian plates) that have been moving northward in recent geological history and colliding with the Eurasian Plate. Figure 1: Overview of the African and Arabian tectonic plate region. These dangers include earthquakes, tsunamis, and volcanoes. GulfofAqaba. Asthenosphere: a portion of the mantle where intense pressure and heat cause the material to flow … Answer: 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. The northern portion of the plate is being pulled under the Eurasian plate at the subduction boundary. The rifting of Africa and Arabia opened the Red Sea as well as the Gulf of Aden, bordering the plate on the southwest and southern sides respectively (see figure 1). The Arabian Plate moves northeasterly between the abovementioned transform fault boundaries, causing, on the one hand, the expansion of the Red Sea and the Gulf of Aden, and on the other hand, the plate collisions at the Makran, Zagros and Taurus Mountains. 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. 2. If correct, label the location of the Mid-Atlantic Ridge on your map. The distribution of earthquakes is concentrated at these boundaries of the Arabian Plate. Some activity still continues especially around Medina,[6] and there are regular eruptions within the Red Sea.[7]. The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward at the Sinai Peninsula and the Red Sea and northward to the Levant. It is a unique fit of the earth's surface jig saw puzzle, different than all other lithospheric plates. Unal, Bunyamin, Mucahit Eren, and M. Gurhan Yalcin. 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. "Investigation of leakage at Ataturk dam and hydroelectric power plant by means of hydrometric measurements." [5] It has the three known main tectonic plate boundaries, divergent, convergent and conservative ones. Second-order plate boundary: Distributed strain across the Hellenic/Adriatic plate boundary zone; Lithospheric subduction along trenches (Cyprus Arc. [5] The opening of the Red Sea rift led to extensive volcanic activity. The volcanic flows occupy large areas of western Saudi Arabia, including the holy cities of Mecca and Madina. At a divergent boundary, two plates move away from each other. A minor tectonic plate consisting mostly of the Arabian Peninsula, extending northward to Mesopotamia and the Levant. The collision between the Arabian Plate and Eurasia is pushing up the Zagros Mountains of Iran. The plate borders are: The Arabian Plate was part of the African Plate during much of the Phanerozoic Eon (Paleozoic–Cenozoic), until the Oligocene Epoch of the Cenozoic Era. Earthquakes are very common in Iran and Iraq. Calabrian Arc) (in part also belonging to (1)): Crustal extension in back-arc basins (Pannonian. Saudi Arabia is part of the so-called Arabian Plate. It is located in the Middle East Region of Asia; it covers approximately 6 million sq. boundary between the Arabian Plate and the African Plate. Red Sea Rift - Arabian Plate The Red Sea Rift is a divergent boundary between the Arabian and African Plates. The plate borders are: This type of boundary is more likely to have earthquakes as a result because of the moving Earth. 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