Stations on the ocean plate moved about 8 centimetres per year toward the continental side. But a station on the continental plate where the two plates meet also moved about 8 centimeters in the same direction. Researchers said this indicates that parts of the plates are firmly joined together, and strain may be accumulating. Assuming that the plates have been joined similarly since the 17th-century quake, the team says the built-up strain would be equivalent to the energy released by a mega-quake.