Laptev Sea Rift

This article has multiple issues. Please help improve it or discuss these issues on the talk page. (Learn how and when to remove these messages) This article relies largely or entirely on a single source. Relevant discussion may be found on the talk page. Please help improve this article by introducing citations to additional sources. Find sources: "Laptev Sea Rift" – news · newspapers · books · scholar · JSTOR (January 2022) This article includes a list of references, related reading, or external links, but its sources remain unclear because it lacks inline citations. Please help improve this article by introducing more precise citations. (January 2022) (Learn how and when to remove this message) (Learn how and when to remove this message)

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.

• Joint US-Russia Workshop on the Plate Tectonic Evolution of Northeast Russia, Dec. 2004

This tectonics article is a stub. You can help Wikipedia by expanding it.

• v
• t
• e