by Suzán Jiván
I
Valleys and ridges
correlations in phases
like edges of old
II
Paleozoic
Blue Ridge and inner Piedmont
seamed orogenies
III
Meta-sediments
intrusively igneous
oceans beginning
IV
Folding and faulting
supercontinent's remnants
later colliding
V
Down-faulted, normal
metamorphosed schist and gneiss
stresses subsided...
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