The Black Hills, Mid-Continent ResortWilliams, Albert N. (Albert Nathaniel)
History
The Black Hills, Mid-Continent Resort
Williams, Albert N. (Albert Nathaniel)
Black Hills (S.D. and Wyo.) -- Description and travel
PALEOZOIC ERA
510
Cambrian Period—First fossils deposited.
Marine life.
430>
Ordovician Period—Invertebrates increase
greatly.
350>
Silurian Period—Coral reefs formed. First
evidence of land life.
310>
Devonian Period—First forests. First
amphibians.
250>
Mississippian, Pennsylvanian, and Permian
Periods.—Reptiles and insects appear.
Continental uplift at end of this period.
180
MESOZOIC ERA
Triassic Period—Small Dinosaurs. First
mammals.
150>
Jurassic Period—Dinosaurs and marine
reptiles dominant.
125>
Cretaceous Period—Dinosaurs reach zenith of
development then disappear. Small mammals.
Flowering plants and development of hardwood
forests.
60
CENOZOIC ERA & PERIOD
Paleocene Epoch—Archaic mammals.
50>
Eocene Epoch—Modern mammals appear.
35>
Oligocene Epoch—Great apes appear.
25>
Miocene Epoch—Grazing types of mammals
appear.
10>
Pliocene Epoch—Man appears.
0
The next period of the earth’s age—the Ordovician period, which extended
from 430,000,000 to 350,000,000 years ago—has left its mark just as
visibly upon the Black Hills. It was during this period that the many
species of invertebrate marine life reached a zenith of development, and
that a bed of sediment was laid down and later compressed to a pinkish
limestone. The fact that this Ordovician bed is less than forty feet
thick indicates that the land mass from which the muds and sands were
drawn was very low, and that the Cambrian sea was relatively shallow,
entertaining only minor erosive currents along its shores.
Public-domain text, read in full here on John Shaqi.
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