Why Separated Coastlines Can Have Matching Shapes

Continental Drift (Plate Tectonics)

When a continent rifts apart, the newly formed conjugate margins—now separated by an ocean basin—retain complementary shapes because they were once joined. Classic examples:

  • South America & Africa – The bulge of Brazil fits the Gulf of Guinea (noted by Ortelius, 1596; confirmed by plate tectonics).
  • North America & Europe/Africa – Matching Appalachian/Caledonian mountain belts and coastal outlines.
  • India & Antarctica/Australia – Gondwanan breakup left matching rifted margins.

Process

Rifting thins the lithosphere, creates a rift valley, then seafloor spreading forms new oceanic crust. The passive margins on either side preserve the "fit" for tens to hundreds of millions of years, modified only by sedimentation, erosion, and later tectonics.

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