The movement between the Sinai Peninsula and the Arabian Plate is primarily a left-lateral strike-slip motion. This means that the two plates are sliding past each other horizontally. This movement is due to the northward movement of the Arabian Plate relative to the Sinai Peninsula. The boundary between these two plates is known as the Dead Sea Transform fault system. This system extends from the Red Sea rift in the south to the East Anatolian Fault in the north. The movement along this fault system has resulted in several significant earthquakes in the region throughout history.

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The movement between the Sinai Peninsula and the Arabian Plate is primarily a left-lateral strike-slip motion. This means that the two plates are sliding past each other horizontally. This movement is due to the northward movement of the Arabian Plate relative to the Sinai Peninsula. The boundary between these two plates is known as the Dead Sea Transform fault system. This system extends from the Red Sea rift in the south to the East Anatolian Fault in the north. The movement along this fault system has resulted in several significant earthquakes in the region throughout history.

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The movement between the Sinai Peninsula and the Arabian Plate is primarily a left-lateral strike-slip motion. This means that the two plates are sliding past each other horizontally. This movement is due to the northward movement of the Arabian Plate relative to the Sinai Peninsula. The boundary between these two plates is known as the Dead Sea Transform fault system. This system extends from the Red Sea rift in the south to the East Anatolian Fault in the north. The movement along this fault system has resulted in several significant earthquakes in the region throughout history.

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What is the plate movement between Sinai Peninsula and Arabian plate?

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