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2007-01-09 18:56:06 · 8 answers · asked by lollybolly 2 in Science & Mathematics Earth Sciences & Geology

8 answers

The Grand Canyon is a very deep - in places over a mile (1600 m) deep - 277 mile (446 km) long cut in the Colorado Plateau that exposes uplifted Proterozoic and Paleozoic strata. The canyon appears on many versions of the Seven Natural Wonders of the World list, although none of these lists is by any means authoritative. The exposed strata are gradually revealed by the gentle incline beginning at Lee's Ferry and continuing to Hance Rapid. At the point where the river crosses the Grand Wash Fault (near Lake Mead) the Canyon ends.

Uplift associated with plate tectonics-caused mountain building events later moved these sediments thousands of feet upward and created the Colorado Plateau. The higher elevation has also resulted in greater precipitation in the Colorado River drainage area, but not enough to change the Grand Canyon area from being semi-arid. Landslides and other mass wasting events then caused headward erosion and stream capture - all of which tend to increase the depth and width of canyons in arid environments.

The uplift of the Colorado Plateau is uneven, resulting in the North Rim of the Grand Canyon being over a thousand feet (about 300 meters) higher than the South Rim. The fact that the Colorado River flows closer to the South Rim is also explained by this asymmetrical uplift. Almost all runoff from the plateau behind the North Rim (which also gets more rain and snow) flows toward the Grand Canyon, while much of the runoff on the plateau behind the South Rim flows away from the canyon (following the general tilt). The result is much greater erosion and thus faster widening of the canyon and its tributary canyons north of the Colorado River.

Temperatures on the North Rim are generally lower than the South Rim because of the greater elevation (8000 feet (2400 meters) above sea level). Heavy snowfall is common during the winter months. Views from the North Rim tend to give a better impression of the expanse of the canyon than those from the South Rim.


[edit] Geology
Main article: Geology of the Grand Canyon area
The principal consensus among geologists is that the Colorado River basin (of which the Grand Canyon is a part) has developed in the past 40 million years and that the Grand Canyon itself is probably less than five to six million years old (with most of the downcutting occurring in the last two million years). The result of all this erosion is one of the most complete geologic columns on the planet.

The major geologic exposures in Grand Canyon range in age from the 2 billion year old Vishnu Schist at the bottom of the Inner Gorge to the 230 million year old Kaibab Limestone on the Rim. Many of the formations were deposited in warm shallow seas, near-shore environments (such as beaches), and swamps as the seashore repeatedly advanced and retreated over the edge of a proto-North America. Major exceptions include the Permian Coconino Sandstone which was laid down as sand dunes in a desert and several parts of the Supai Group.

The great depth of the Grand Canyon and especially the height of its strata (most of which formed below sea level) can be attributed to 5,000 to 10,000 feet (1500 to 3000 m) of uplift of the Colorado Plateaus, starting about 65 million years ago (during the Laramide Orogeny). This uplift has steepened the stream gradient of the Colorado River and its tributaries, which in turn has increased their speed and thus their ability to cut through rock (see the elevation summary of the Colorado River for present conditions).

Weather conditions during the ice ages also increased the amount of water in the Colorado River drainage system. The ancestral Colorado River responded by cutting its channel faster and deeper.

The base level and course of the Colorado River (or its ancestral equivalent) changed 5.3 million years ago when the Gulf of California opened and lowered the river's base level (its lowest point). This increased the rate of erosion and cut nearly all of the Grand Canyon's current depth by 1.2 million years ago. The terraced walls of the canyon were created by differential erosion[2].

About one million years ago, volcanic activity (mostly near the western canyon area) deposited ash and lava over the area, which at times completely obstructed the river. These volcanic rocks are the youngest in the canyon.

2007-01-09 19:06:30 · answer #1 · answered by Anonymous · 0 1

At the South Rim, near Grand Canyon Village, it's a vertical mile (about 5,000 feet / 1524 m) from rim to river (7 miles / 11.3 km by trail, if you're walking). At its deepest, it is 6000 vertical feet / 1829 km from rim to river. The width of the canyon at Grand Canyon Village is 10 miles / 16 km (rim to rim), though in places it is as much as 18 miles / 29 km wide.

2007-01-10 19:12:42 · answer #2 · answered by zaleonia1 4 · 0 0

tdystoner - is wrong, it isn't the deepest.
the deepest canyon on earth is in the atlantic ocean off the east coast of the USA can't remember the name, geologist know it's over 3 miles deep in parts but they can't tell how deep it actually is as they haven't the technology to reach the deepest parts.
In fairness, the grand canyon is the deepest on land at 1.26 miles.

2007-01-10 05:09:51 · answer #3 · answered by willygromit 3 · 0 0

About 4,000 down from the rim to the river at the deepest point.

2007-01-09 19:00:21 · answer #4 · answered by Scythian1950 7 · 0 0

Its deepest point is 1.2 miles down
Shallowest 6 ft

2007-01-09 20:26:10 · answer #5 · answered by Red5 5 · 0 0

At its deepest, it is 6000 vertical feet / 1829 km from rim to river

2007-01-09 22:38:47 · answer #6 · answered by Anonymous · 0 0

According to wikipedia, a mile.

2007-01-09 19:04:16 · answer #7 · answered by SJH 3 · 0 0

Oh! Where would we be without Wikipedia.....

2007-01-09 20:13:29 · answer #8 · answered by Anonymous · 0 0

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