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It is situated 5,800 feet (1,767.8 m) above sea level, 12 miles (19 km) south of Utah Route 12, and 20 miles (32 km) southeast of Bryce Canyon National Park. It is accessible from the north from Cannonville by a paved road and from the south by Road 400, a dirt road from the Page, Arizona area to Cannonville, passable for most vehicles in dry ...
Observation Point is situated at the north end of Zion Canyon, towering 2,100 feet (640 meters) above the canyon floor and the North Fork of the Virgin River which drains precipitation runoff from this viewpoint. A popular 8-mile round-trip trail climbs from the Weeping Rock trailhead along Zion Canyon Road to reach the top. [3]
The rocks of the eroded canyon contain iron and manganese in various combinations, providing brilliant colors that led Indians to call it the Circle of Painted Cliffs. Iron oxides provide the reds, oranges and yellows, while manganese oxides provide shades of purple. The color of the rock is soft and subtle compared to the hoodoos at Bryce Canyon.
West end of the Pine Creek Bridge and the east portal of the Zion-Mt. Carmel Tunnel, c. 2006 A horseback party at the western entrance to the Zion-Mt. Carmel Tunnel, September 1929. The tunnel shortened the distance from Zion National Park to Bryce Canyon National Park by 70 miles (110 km).
Goblin Valley State Park and Bryce Canyon National Park, also in Utah about 190 miles (310 km) to the southwest, contain some of the largest occurrences of hoodoos in the world. The park lies within the San Rafael Desert on the southeastern edge of the San Rafael Swell , north of the Henry Mountains .
Spring and fall are the most favorable seasons to visit Checkerboard Mesa. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer.
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