The
Laptev Sea Rift is a divergent
tectonic plate boundary between the
North American Plate and the
Eurasian Plate located on the
Arctic Ocean coast of northeastern
Siberia in
Russia. The Laptev Sea Rift is the continuation of the
Gakkel Ridge (Mid-Arctic Ridge) into the
continental crust of Siberia. It starts offshore in the
continental shelf and continues onshore to a point located in the
Chersky Range where the boundary motion changes from extension to compression.
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