|
THE
FORMATION OF THE ROCKY MOUNTAINS
|
|
|
→ The Rocky Mountains of North America
extend 5,000 kilometers from New Mexico all the way
|
|
|
up through Canada. Elevations along the
range are about 1,500 meters along the lower plains to
|
|
|
4,399 meters at the
highest peak, and widths range from 120 to 650 kilometers. The natural
beauty,
|
|
|
abundant wildlife, and fresh water of the
ranges have attracted human inhabitants for the last
|
|
5
|
10,000 to 12,000 years.
|
|
|
|
|
|
The history of the
Rocky Mountains begins in the pre-Cambrian era, a half-billion years ago.
|
|
|
While this is long before the Rocky
Mountains themselves began forming, their hard core rocks—
|
|
|
consisting of granites,
schists, gneisses, quartzites, and slates—were produced in ancient ranges.
|
|
10
|
Erosion eventually leveled these mountain
ranges, and during the Paleozoic and Mesozoic Eras,
|
|
|
about 75 to 540 million
years ago, the ocean invaded the land and deposited sediments some
|
|
|
20,000 feet deep. They included layers of sandstones,
shales, and limestones.
|
|
|
|
|
|
At the close of the Mesozoic Era, during
the Cretaceous period about 75 million years ago, the
|
|
15
|
growth of the Rockies
began. There was a tremendous squeezing that uplifted the region in a great
|
|
|
series of folds, like wrinkles in a
carpet. After the arching, erosion carved away at the mountains.
|
|
|
■ Some 10,000 feet of sedimentary rock were
washed off the top of the arch, exposing the hard
|
|
|
rock core. The erosional resistance of
these hard, crystalline rocks led to the formation of the high
|
|
|
peaks that still exist
today. On the flanks of the core the sedimentary beds sloped outward. ■ Great
|
|
20
|
quantities of sand and clay were spread
out on the bordering plains and plateaus. This was only one
|
|
|
of the cycles of upheaval
and erosion that occurred in the region. ■
|
|
|
|
|
|
Near the end of the
Eocene period, about 40 million years ago, the Rockies again rose several
|
|
|
thousand feet. Volcanoes erupted, most
extensively in the Yellowstone Plateau and the Absaroka
|
|
25
|
Range. As the mountains
were formed, streams eroded their sides, and thousands of feet of
|
|
|
sediment spread out on plains and
plateaus. Just before the Pleistocene period, about one million
|
|
|
years ago, the region
again uplifted. ■ Streams flowed faster and began to cut
canyons, and rivers
|
|
|
ate deep gorges through
the ranges. The most recent geological event of note
was the "Ice Age"
|
|
|
during the Pleistocene
Epoch, 1 million to 10,000 years ago. The high peaks of the Sangre de
|
|
30
|
Cristo Mountains supported numerous small
glaciers and snows accumulated on the sides of the
|
|
|
mountains. These
glaciers carved a typical collection of alpine landforms, such as cirques,
horns,
|
|
|
aretes, and cols. Lower down in the
glaciated valleys, various kinds of till and stratified sediments
|
|
|
accumulated to form
Moraines. Most of the glacial deposits and landforms present today date
from
|
|
|
the last glacial phase, known in the
Rocky Mountains as the Pinedale Glaciation or Pinedale Stage.
|
|
35
|
During this stage, over
90% of the Yellowstone National Park was covered in ice. The glaciated
|
|
|
terrains formed in this era are among the
most picturesque in the high alpine Rockies today, as
|
|
|
glaciers formed and
moved down the valleys, thereby further eroding the mountains into bold and
|
|
|
dramatic forms.
|
|
|
|
|
40
|
There was even a "little ice
age" from about 1550 to 1860—a few centuries of glacial advance—that
|
|
|
made its mark on the
mountains recently. For example, the Agassiz and Jackson glaciers in
Glacier
|
|
|
National Park reached their most forward
positions by around 1860. The incessant sculpturing of
|
|
|
the Rockies by rain,
wind, and ice continues even today.
|
No comments:
Post a Comment
thank you for visiting my blog and for your nice comments