Grand Canyon Geology Lessons on View
The Colorado River has done all the erosional work of carving away cubic
kilometers of rock in a geologically short period of time. Visible as a darker
line snaking along the bottom of the canyon, the river lies at an altitude of
715 meters (2,345 feet), thousands of meters below the North and South Rims.
Temperatures are furnace-like on the river banks in the summer. But Grand Canyon
Village, the classic outlook point for visitors, enjoys a milder climate at an
altitude of 2,100 meters (6,890 feet).
The Grand Canyon has become a geologic icon—a place where you can almost
sense the invisible tectonic forces within the Earth. The North and South Rims
are part of the Kaibab Plateau, a gentle tectonic swell in the landscape. The
uplift of the plateau had two pronounced effects on the landscape that show up
in this image. First, in drier parts of the world, forests usually indicate
higher places; higher altitudes are cooler and wetter, conditions that allow
trees to grow. The other geologic lesson on view is the canyon itself.
Geologists now know that a river can cut a canyon only if the Earth surface
rises vertically. If such uplift is not rapid, a river can maintain its course
by eroding huge quantities of rock and forming a canyon.
This astronaut photograph (ISS039-E-5258) was taken on March 25, 2014 by the
Expedition 39 crew, with a Nikon D3S digital camera using a 180 millimeter lens,
and is provided by the ISS Crew Earth Observations Facility and the Earth
Science and Remote Sensing Unit, Johnson Space Center. It has been cropped and
enhanced to improve contrast, and lens artifacts have been removed.
Image Credit: NASA
Caption: M. Justin Wilkinson, Jacobs at NASA-JSC
Caption: M. Justin Wilkinson, Jacobs at NASA-JSC
Guillermo Gonzalo Sánchez Achutegui
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