Talk:Transform boundary
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this site doesnt tell you what forms ON THE BOUNDARIES....PUT something on that
some more general info is needed
For what I remember from my studies the general term for conservative plate margins is "strike-slip", while "transform" applies specifically to discontinuities that apparently dislocate two segments of oceanic ridge. In these inner segments the reciprocal motion of the walls (adjacent plates) creates a friction and seismic activity, while in the outer segments the walls belong to the same plate and show no reciprocal movement. Possa (talk) 22:29, 20 February 2008 (UTC)
[edit] help me how can this work
this doesnt make sense tome i neee this for schooli needhelp —Preceding unsigned comment added by 70.119.145.79 (talk) 23:50, 27 February 2008 (UTC)
[edit] Continential Crust
THE LAYER OF THE EARTH THAT UNDER LiES THE CONTiNENTS AND CONTiNENTAL SHELVES;THE THICK PART OF THE EARTHS CRUST THAT FORM LARGE LAND MASSES.CONTiNENTiAL CRUST iS LiGHTER THAN THE OCEANiC CRUST.iT iS FOUND UNDER THE VARiOUS MOUNTAiN RANGES. BY--> ₡AILEY
[edit] Merge Proposal
This article ought to be merged with the Transform fault article. Tmangray (talk) 18:58, 30 April 2008 (UTC)
- Support, with the feeling that the fault article name should survive. Cheers Geologyguy (talk) 19:01, 30 April 2008 (UTC)
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- Here. Cheers Geologyguy (talk) 21:46, 30 April 2008 (UTC)
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- Thanks for that. I see that they allow "boldness". I think I'll try that first and see what happens. Looking at this article here, I don't see much that isn't mostly duplicative. Therefore, I will "boldly" make a redirect to the other article, leaving it up to anyone out there who wants to cut and paste material from this article that they think belongs over at the other article. Tmangray (talk) 21:51, 30 April 2008 (UTC)
