The shape and location of the Sumatran fault as well as the active volcanic arc are remarkably correlated with the shape and character in the fundamental subducting oceanic lithosphere. Even so, Energetic volcanic facilities from the Sumatran volcanic arc haven't affected noticeably the geometry with the Lively Sumatran fault. On The idea of its geologic heritage and sample of deformation, we divide the Sumatran plate margin into northern, central and southern domains. We support preceding proposals which the geometry and character with the subducting Investigator fracture zone are influencing The form and evolution in the Sumatran fault process inside the central area. The southern domain is easily the most typical. The Sumatran fault there comprises six battle-stepping segments. This sample indicates that the general pattern of the fault deviates 4 ø clockwise within the slip vector between The 2 blocks it separates. The regularity of the area and its association with the percentage of the subduction zone that generated the large (Mw 9) earthquake of 1833 counsel that a geometrically easy subducting slab brings about the two easy strike-slip faulting and unusually huge subduction earthquakes.
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