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Miranda, roughly 500 km (311 mi) in diameter, exhibits varied geologic provinces. Ridges and valleys of one province are cut off against the boundary of the next. Probable compressional (pushed-together) folded ridges are seen in curvilinear patterns, as are many extensional (pulled-apart) faults. Some of these show very large cliffs, ranging from 0.5 to 5 km (0.3 to 3.1 mi) in height, higher than the walls of the Grand Canyon on Earth.

CREDIT: NASA/JPL.

Source:
http://photojournal.jpl.nasa.gov/catalog/PIA00043