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
The Cenozoic (table 1), last and shortest of the geologic eras,
comprises the Tertiary and Quaternary Periods. It began about 65 million
years ago and is represented by only the final one-half inch of our
imaginary yardstick of time (fig. 19). Nevertheless, it is the era
during which the Tetons rose in their present form and the landscape was
sculptured into the panorama of beauty that we now see. In order to show
the many Tertiary and Quaternary events in the Teton region, it is
necessary to enlarge greatly the last part of the yardstick (fig. 44).
There are two reasons for the extraordinarily clear and complete record.
First, the Teton region was a relatively active part of the earth’s
crust, characterized by many downdropped blocks. The number of events is
great and their records are preserved in sediments trapped in the
subsiding basins. Second, the geologically recent past is much easier to
see than the far dimmer, distant past; the rocks that record later
events are fresher, less altered, more complete, and more easily
interpreted than are those that tell us of older events.
[Illustration: Table 5.—Cenozoic sedimentary rocks and
unconsolidated deposits in the Teton region.]
Age Formation Thickness Description Where exposed
(feet)
QUATERNARY
Recent
Modern 0-200± Sand, gravel, and Floor of Jackson
stream, silt along present Hole and in canyons
landslide, streams; jumbled and on
glacial and broken rock in mountainsides
talus deposits landslides and on throughout the
talus slopes; region.
debris around
existing glaciers.
Pleistocene
Glacial 0-200± Gravel, sand, silt, Floor of Jackson
deposits and and glacial debris. Hole.
loess
Unnamed upper 0-500 Shale, brown-gray, Gros Ventre River
lake sequence sandstone, and Valley.
conglomerate.
Unnamed lower 0-200 Shale, siltstone, National Elk Refuge.
lake sequence and sandstone,
gray, green, and
red.
? Pleistocene or Pliocene
Bivouac 0-1,000 Conglomerate, with Signal Mountain and
Formation purplish-gray West Gros Ventre
welded tuff in Butte.
upper part.
TERTIARY
Pliocene
Teewinot 0-6,000 Limestone, tuff, National Elk
Formation and claystone, Refuge, Blacktail
white, soft. Butte, and eastern
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