The land in
northeastern Alabama is composed of terranes, discrete
fragments of crust accreted on to a craton. Terrane
accretion is one mechanism by which continents grow.
Three major tectonic
events molded the Cheaha State Park area into what it is
today.
- The Taconic
Orogeny took place in the Ordivician Period
(about 420 million years ago). The North American
and European tectonic plates collided, producing
an equivalent mountain building event in Europe
at the same time. The Piedmont Terrane was added
to the continent during this event.
- The Acadian
Orogeny occurred in the Devonian and Silurian
Periods (about 350 MA). This event did not
produce the faulting and thrusting seen with the
other two orogenies. Instead, it left behind
granites of that age, similar to the Andes and
Cascade mountain ranges.
- The last mountain
building event was the Alleghanian Orogeny,
which happened in the Permian and Carboniferous
Periods (about 250 MA). The Carolina Slate Belt
was pasted onto the continent during the
Alleghanian Orogeny.
There is a
compositional change between the Carolina and Piedmont
Terranes, which are separated by a boundary called a
suture.
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