(Science: geology) Designating, or pertaining to, the series of rocks forming the Taconic mountains in western new England. They were once supposed to be older than the Cambrian, but later proved to belong to the Lower silurian and Cambrian.

Please contribute to this project, if you have more information about this term feel free to edit this page

This page was last modified on 3 October 2005, at 21:16. This page has been accessed 1,309 times. 
What links here | Related changes | Permanent link