Creation of the Teton Landscape: The Geologic Story of Grand Teton National ParkReed, John C. (John Calvin)
Science
Creation of the Teton Landscape: The Geologic Story of Grand Teton National Park
Reed, John C. (John Calvin)
Geology -- Wyoming -- Grand Teton National Park
During early Eocene time, coal swamps formed in eastern Jackson Hole and
persisted for thousands of years, as is shown by 60 feet of coal in a
single bed at one locality. Continuing on into middle Eocene time, the
climate was subtropical and humid, and the terrain was near sea level.
Tropical breadfruits, figs, and magnolias flourished along with a more
temperate flora of redwood, hickory, maple, and oak. Horses the size of
a dog and many other small mammals were abundant. Primates, thriving in
an ideal forest habitat, were numerous. Streams contained gar fish and
crocodiles (fig. 50).
[Illustration: Figure 51. _A typical Oligocene landscape showing
some of the more abundant types of mammals. Mural painting by Jay H.
Matterness; photo courtesy of Smithsonian Institution._]
_Trigonias_ early rhinoceros
_Perchoerus_ early peccary
_Mesohippus_ 3-toed horse
_Aepinacodon_ remote relative of hippopotamus
_Archaeotherium_ giant piglike mammal
_Protoceras_ bizarre horned ruminant
_Hesperocyon_ ancestral dog
_Hyracodon_ small fleet-footed rhinoceros
_Poëbrotherium_ ancestral camel
_Hypisodus_ very small chevrotainlike ruminant
_Ictops_ small insect-eating mammal
_Brontotherium_ titanothere
_Protapirus_ ancestral tapir
_Glyptosaurus_ extinct lizard
_Hoplophoneus_ saber-toothed cat
_Subhyracodon_ early rhinoceros
_Merycoidodon_ sheeplike grazing mammal
_Hyaenodon_ archaic hyenalike mammal
_Hypertragulus_ chevrotainlike ruminant
Early in the Oligocene Epoch, between 30 and 35 million years ago, the
climate in Jackson Hole became cooler and drier, and the subtropical
plants gave way to the warm temperate flora of oak, beech, maple, alder,
and ash. The general land surface rose higher above sea level, perhaps
by accumulation of several thousand feet of Oligocene volcanic rocks
(fig. 52) rather than by continental uplift. _Titanotheres_ (large
four-legged mammals with the general size and shape of a rhinoceros)
flourished in great numbers for a few million years and then abruptly
vanished. Horses by now were about the size of a very small modern colt.
Rabbits, rodents, carnivores, tiny camels, and other mammals were
abundant in Jackson Hole, and the fauna, surprisingly, was essentially
the same as that 500 miles to the east, at a much lower elevation, on
the plains of Nebraska and South Dakota (fig. 51).
Public-domain text, read in full here on John Shaqi.
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