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Grand Canyon

The Grand Canyon leaves all who experience it with a sense of wonder, magic and awe. From its dramatic 1500 m (5000 ft) deep, 446 km (277 mi) long, and up to 29 km (18 mi) wide gorge, to its diverse plateaus, towers and hills, the Grand Canyon is one of the world's most stunning destinations. Rich with exceptional beauty, ancient geological history and modern universal amazement, the Grand Canyon attracts more than 5 million tourists each year.
See the Grand Canyon as the eagle does and soar above the plateau on a helicopter or airplane tour. Fly around towering buttes, mesas, and valleys within the Grand Canyon's main gorge. Soar over dense evergreen forests of juniper and piñon, or arid plateaus speckled with desert plants like agave and Spanish bayonet. The Grand Canyon plateau region's forests are segmented by old lava flows, hills of volcanic debris and intrusions of igneous rock. Seeing the Grand Canyon by air is an unforgettable adventure with a unique perspective.
You will also find restaurants, shopping, art galleries, and other services in the communities of the Grand Canyon area. Find yourself wandering through quaint boutiques, art and shopping areas. Discover one-of-a-kind hand-made treasures and enjoy the thrill of selecting a special souvenir.
What climate should you expect on the Coconino and Kaibab plateaus, the North and South Rim? At 1500 and 2700 km (5000 and 9000 feet) above sea level, the climate of the plateau region above the Grand Canyon can swing between extremes of heat and cold. The canyon floor can also exceed 100 degrees Fahrenheit in the summer, but seldom experiences frost in the winter. Regardless of the weather, the Grand Canyon is one of the world's favorite sites year-round. Visit the Grand Canyon and see why it has been the stuff of wonder for centuries of adventurers, vacationers, artists and explorers.

For information on the Grand Canyon click on the following links

Links

http://memory.loc.gov/ammem/gmdhtml/nphtml/

http://sunsite.nus.edu.sg/mw/iss06/canyon.html

http://www.kaibab.org/geology/gc_geol.htm