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Why is Denali (6,194 m) so big? Caught inside the tectonic wake of a migrating restraining bend
Topography along strike‐slip fault restraining bends is theoretically self‐limited by erosion,
block translation and the expected abandonment of fault bends. However, Denali (6,194 m) …
block translation and the expected abandonment of fault bends. However, Denali (6,194 m) …