Atoko Point facts for kids

Quick facts for kids Atoko Point
Kwagunt Canyon, Atoko Point (right)
Highest point
Elevation	8,382 ft (2,555 m)
Prominence	50 ft (15 m)
Isolation	0.5 mi (0.80 km)
Parent peak	prominence 8442 ft
Geography
Atoko Point Location in Arizona Show map of Arizona Atoko Point Location in the United States Show map of the United States
Location	Grand Canyon National Park, (Walhalla Plateau) Coconino County, Arizona, US
Parent range	Kaibab Plateau (Walhalla Plateau) Colorado Plateau
Topo map	USGS Walhalla Plateau
Geology
Age of rock	Permian
Mountain type	sedimentary rock: limestone-(prominence-cliff)
Type of rock	Kaibab Limestone

Atoko Point is a tall cliff located in the eastern part of the Grand Canyon in Arizona, United States. It stands at an elevation of 8,382 feet (about 2,555 meters). This amazing natural landmark is found within the Grand Canyon National Park.

Atoko Point is part of a special area called the Walhalla Plateau. It offers incredible views of the vast canyon landscape.

Where is Atoko Point?

Atoko Point is in Coconino County, Arizona. It is about 6.5 miles (10.5 km) south-southeast of Point Imperial. Point Imperial is the northernmost spot on the east side of the North Rim of the Grand Canyon.

Nearby Landmarks

Atoko Point is close to other famous spots. It is 1.3 miles (2.1 km) southeast of Roosevelt Point. It is also 2.6 miles (4.2 km) southeast of the Vista Encantada viewpoint.

Water Features

Two small canyons, which are the beginnings of Upper Kwagunt Creek, surround Atoko Point. These creeks flow east towards the Colorado River. The Colorado River is about 6.5 miles (10.5 km) east, in the southern part of Marble Canyon.

Access to Atoko Point

You can find Atoko Point about one mile east of the Cape Royal Road. This road helps visitors get to different viewpoints in the Grand Canyon.

What is Atoko Point Made Of?

The cliff of Atoko Point is made up of several layers of rock. These layers show the long history of the Earth.

Rock Layers

• Kaibab Limestone: This is the very top layer of the cliff. It is a type of rock often seen at the rim of the Grand Canyon.
• Toroweap Formation: Below the Kaibab Limestone, you will find this layer.
• Coconino Sandstone: This layer forms white cliffs. It is known for its bright, sandy appearance.
• Hermit Shale: Underneath the Coconino Sandstone is a softer, reddish-brown rock. This layer is easy to erode, meaning it wears away over time.
• Supai Group: At the very bottom are four layers of bright red-orange rocks. These layers make up the Supai Group.

An aerial view showing Atoko Point.