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Webster 1913 Edition


Niagara period

Ni-ag′a-ra pe′ri-od

.
(Geol.)
A subdivision or the American Upper Silurian system, embracing the
Medina
,
Clinton
, and
Niagara epoch
. The rocks of the Niagara epoch, mostly limestones, are extensively distributed, and at Niagara Falls consist of about eighty feet of shale supporting a greater thickness of limestone, which is gradually undermined by the removal of the shale. See Chart of
Geology
.