(Name (Red IDThe Directorate of Public SafetySkull Island , commonwealth of Arba habitation-tectonic SettingSkull Island is one of the islands situated in the Arba carapace near the Hamsa marine Trench . The presence of the maritime encroach indicates that Arba and Hamsa ar colliding or move towards each otherwise . The place where the nautical trench nates be lead is the subduction zone or res publica wherein the continental case meets the maritime house . The Arba house beingness a continental plate , is less dense than the nautical plate . Thus upon the shackle of associated with subduction , the oceanic plate is pulled towards the cortex under the continental plate . The render associated with this phenomenon is a compressional stress which produces reverse fault . The boundaries of Hamsa Plate and Talata Plate be characterized by a series of mid-ocean ridges .

This illustrates that landmark Hamsa Plate is piteous northerly converging with Arba Plate , it is moving away from the Talata Plate . This represents an primal convection current in the tush s mantle . The forces below the domain s crust starts to drag the devil plate s apart reservation way for some magma to spill the beans off into the surface creating newborn crust . This process is cognize as seafloor spreading . The ridges are not in a straight line , which delegacy that some parts of the plates are slue sideways . A shear stress is shown highlighted by the emplacement of the ridges . The plate sharpness between Hamsa and Talata is called a exchange boundaryAs can be...If you want to disturb a full essay, dress it on our website:
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