#Fold mountains
Hi, Jon–
In Old Red Sandstone, I am pleased to have a name for proto-N.America +
proto-Europe (Laurentia+Baltica), since I gather they were together for a long
time before joining up with Pangaea.
The Jan. 1995 Scientific American has a cover story proposing that Laurentia
rifted away from proto-S.America ~550 million years ago; the coast that would
eventually become the Appalachians separated from what is now Chile, more or
less (modern Scotland would have been in the Arica embayment between Peru and
Chile, more or less). It is suggested that Laurentia might have bumped S.
America twice more while making and end run around it before being collected
into Pangaea. In the mid-Ordovician, the eastern U.S. presumably hit Peru; in
the late Devonian, they have the southeastern U.S. hit again near Peru or
Ecuador (by this time it is really O.R.S., not just Laurentia).
That last collision, in the late Devonian, would have corresponded to the
Acadian orogeny, they figure. Is this the first orogeny you spoke of? Thus S.
America would replace the "small exotic terranes" you spoke of, or perhaps they
were island arcs caught in the squeeze.
–Doug