This is an old revision of this page, as edited by Hike395 (talk | contribs) at 06:51, 4 October 2015 (remove overused {{geological history}} template per discussion at WT:WikiProject Geology using AWB). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
 | This article does not cite any sources. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources: "Charcot Plate" – news · newspapers · books · scholar · JSTOR (November 2006) (Learn how and when to remove this message) |
The Charcot Plate was a fragment of the Phoenix Plate. The Charcot Plate is subducting under West Antarctica. The subduction of the Charcot Plate stopped before 83 Ma, and became fused onto the Antarctic Peninsula. There are remnants of the western part of the Charcot Plate in the Bellingshausen Sea.
 | This palaeogeography article is a stub. You can help Wikipedia by expanding it. |
