Stationary boundaries are when two plates are too weak to take over each other. 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. The northern portion of the plate is being pulled under the Eurasian plate at the subduction boundary. 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 Late Paleozoic-Mesozoic rifts Most prominent rift-related structures of Arabia are inverted intracontinental rifts … 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 Palmyride belt strikes NE and is sandwiched between two relatively stable crustal blocks of the Arabian platform: the Aleppo plateau in the north and the Rutbah uplift in the south. Divergent boundaries happen when two plates move apart from each other. The photos you provided may be used to improve Bing image processing services. 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. It has the three known main tectonic plate boundaries, divergent, convergent and conservative ones. Tyrrhenian. The Arabian Plate is rifting away from the African plate along an active divergent ridge system, to form the Red Sea and Gulf of Aden. The primary geologic structures of the northern Arabian plate in western Syria include the intracontinental Palmyride mountain belt and the interplate boundary of the Dead Sea transform fault system. "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. The rift, a narrow zone, is a developing divergent tectonic plate boundary where the African Plate is in the process of splitting into two tectonic plates, called the Somali Plate and the Nubian Plate, at a … Saudi Arabia is part of the so-called Arabian Plate. The answer is divergent boundary. What type of plate boundary is the East African Rift Valley? At a divergent boundary, two plates move away from each other. 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. A)seafloor fossils at location W B)earthquakes and volcanic eruptions near location X C)flooding near location Y D)horizontal sedimentary layers at location Z The Red Sea is growing because a divergent boundary exists in the Red Sea between the Arabian Peninsula and Africa. It consists of most of Europe, Russia, and parts of Asia. Plate tectonics is the theory explaining the structure of the Earth's crust (and many associated phenomena) that result from the interaction of rigid lithospheric plates that move slowly over the underlying mantle.. Lithosphere: composed of the crust and uppermost solid portion of the mantle. The Arabian Peninsula constitute as the largest part of this plate, hence, its name. It is located in the Middle East Region of Asia; it covers approximately 6 million sq. Second-order plate boundary: Distributed strain across the Hellenic/Adriatic plate boundary zone; Lithospheric subduction along trenches (Cyprus Arc. Aegean. To the east, the East Anatolian Fault, a left lateral transform fault, forms a boundary with the Arabian Plate. Search for Renewable Energy Sources and Water, Environmental Impacts and Occupational Safety of Mining Activities, Paleontology of Vertebrate and Invertebrate Fossils, Environmental Impacts of Natural Materials, Earthquakes in the Harrat Al-Shaqa (Lunayyir). The Arabian Peninsula constitute as the largest part of this plate, hence, its name. Regions include parts of Awdal (Somalia/Somaliland), the Khuzestan Province (Iran), the Southeastern Anatolia Region (Turkey), and the Southern Denkalya Subregion (Eritrea). Transform boundaries occur when two plates slide past each other. If correct, label the location of the Mid-Atlantic Ridge on your map. For some cases, simplified schemes are suggested to explain dynamics of interaction between the in-traplate and plate boundary processes. km and its net movement is northward. Engineering Geology 93.1 (2007): 45-63. The plate is bounded from the west by the Red Sea floor spreading zone and from the south by the Gulf of Aden floor spreading zone, and in both regions, these parts of the Arabian Plate are larger. Some studies suggest that some internal regional faults may be extensions of some transform faults in the Red Sea. The collision between the Arabian Plate and Eurasia is pushing up the Zagros Mountains of Iran. Arrows show the relative direction of plate motion. [2], The Arabian Plate is the most common designation of the region, although it is also sometimes referred to as the Arab Plate.[3]. The African-Arabian region is composed of the following tectonic plates: Arabia, Madagascar, Nubia, Seychelles, and Somali (Figure 1). 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 the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. The boundaries of the Arabian Plate relative to its neighboring plates (Johnson, 1998). 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. This region is perhaps most well known for the North Anatolian Fault; the east-west striking continental transform fault situated in northern Turkey, which … The Anatolian Plate or the Turkish Plate is a continental tectonic plate comprising most of the Anatolia (Asia Minor) peninsula (and the country of Turkey). That's where the Eurasian and Arabian Tectonic plates meet and where the Zagros mountain range developed – the location of the latest quake. "Investigation of leakage at Ataturk dam and hydroelectric power plant by means of hydrometric measurements." Earthquakes are very common in Iran and Iraq. 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. It is a unique fit of the earth's surface jig saw puzzle, different than all other lithospheric plates. Saudi Arabia is part of the so-called Arabian Plate. Plate Boundaries Type of Boundary Pacific Plate – Nazca Plate Divergent Pacific Plate – Cocos Plate Divergent Hellenic/Adriatic plate boundary: Distributed strain across the Hellenic/Adriatic plate boundary processes the.! Opening of the fact it is a rift that is causing Sea floor spreading and the plate! Dangers include earthquakes, tsunamis, and M. Gurhan Yalcin: Rifting and graben (! 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