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Cheops Pyramid facts for kids

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Cheops Pyramid
Cheops Pyramid seen from Yavapai Point.jpg
South aspect, from South Rim's Yavapai Point
Highest point
Elevation 5,401 ft (1,646 m)
Prominence 800 ft (240 m)
Isolation 1.72 mi (2.77 km)
Parent peak Isis Temple (7,006 ft)
Geography
Cheops Pyramid is located in Arizona
Cheops Pyramid
Cheops Pyramid
Location in Arizona
Cheops Pyramid is located in the United States
Cheops Pyramid
Cheops Pyramid
Location in the United States
Location Grand Canyon National Park
Coconino County, Arizona, US
Parent range Kaibab Plateau
Colorado Plateau
Topo map USGS Phantom Ranch
Type of rock sandstone, limestone, shale
Climbing
Easiest route class 4 climbing

Cheops Pyramid is a cool mountain peak in the amazing Grand Canyon, Arizona, USA. It stands tall at 5,401 feet (1,646 meters) above sea level. This special type of mountain, called a butte, looks like a flat-topped hill with steep sides.

It's located in Coconino County, about four miles north of Grand Canyon Village. Cheops Pyramid is also near other famous peaks. It's about 2.5 miles southwest of Buddha Temple and 1.7 miles southeast of Isis Temple.

This butte rises dramatically, about 3,000 feet (914 meters) above the Colorado River in just 1.5 miles. That's a huge drop! The area around Cheops Pyramid has a Cold semi-arid climate. This means it's usually dry with hot summers and cold winters.

How Cheops Pyramid Got Its Name

The name "Cheops Pyramid" was given by George Wharton James. He thought the mountain looked a lot like the famous Great Pyramid of Giza in Egypt. That pyramid was built by an ancient Egyptian pharaoh named Khufu, also known as Cheops.

This naming tradition was started by Clarence Dutton. He liked to name Grand Canyon features after gods and goddesses from old myths. The name "Cheops Pyramid" was officially accepted in 1906. This was done by the United States Board on Geographic Names.

What is Cheops Pyramid Made Of?

Cheops Pyramid is a natural leftover from erosion. Imagine water and wind slowly wearing away rock over millions of years. This mountain is what's left behind.

It has a flat top made of a rock called Redwall Limestone. This limestone formed during the Mississippian period, a long time ago. Below the limestone, you'll find green shale slopes. These shales are part of the Tonto Group from the Cambrian period. Even deeper, there are red shales and a tough rock called Shinumo Quartzite. These older rocks belong to the Unkar Group from the Proterozoic era.

When it rains on Cheops Pyramid, the water flows off its sides. This water, called runoff, drains south towards the Colorado River. It travels through two creeks: Phantom Creek on the east side and Ninetyone Mile Creek on the west side.

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