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transform fault
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transform faults Figure 23: Two transform faults offsetting a mid-oceanic ridge. volcanism and plate tectonics The Earth's crust is a jigsaw puzzle of huge rigid plates in constant relative motion. The plates are bounded by three types of features: ridge axes, where new seafloor is created in mid-ocean; transform faults, where plates slide past one another; and subduction zones, where plates overlap, with one plate sliding under the other.
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transform faults
Figure 23: Two transform faults offsetting a mid-oceanic ridge.
volcanism and plate tectonics
The Earth's crust is a jigsaw puzzle of huge rigid plates in constant relative motion. The plates are bounded by three types of features: ridge axes, where new seafloor is created in mid-ocean; transform faults, where plates slide past one another; and subduction zones, where plates overlap, with one plate sliding under the other.
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