The Golden Throne (7,042') is comprised of interlayered red sandstone and gypsum from the Carmel Formation, a layer in the San Rafael Group formed during the Jurassic Period. It's among the tallest features in the Waterpocket Fold, and visible from many points in the Park. The Golden Throne Trail climbs 1.95 mles and 727' above Capitol Gorge along cliffs and rims to a slickrock terrace with good views of the Throne and adjacent domes. 

Though relatively short, the Golden Throne Trail's steep profile and various aspects expose visitors to a range of geologic layers and ecological diversity

The trail ends on a wavy slickrock bench under the Golden Throne, with access to open rims that overlook the entrance to Capitol Gorge

Portions of the trail cross areas of loose scattered rock, which may obfuscate the location and continuity of cairns

The Carmel Formation is the oldest layer in the San Rafael group formed during the Jurassic Age

The trail wraps along open rims of side canyons which reveal multi-layer rock profiles in Capitol Gorge

Pinyon Pine Nuts contain approximately 3000 calories per pound, and are a great source of protein, fat and oleic acid

Biological soil crusts, which cover much of the bluff on which the trail ends, stabilize soil, fix nitrogen and increase soil's ability to absorb and retain water

The final approach to Golden Throne runs across a colorful pallet of white, pink and red sandstones

Juniper root systems are extensive: they can reach 25' down and spread dozens of feet laterally to access water

Juniper berries are actually not berries at all - they're actually a type of cone with collapsed scales which protect the seed inside

Roundleaf Buffaloberry bushes have leathery leaves covered in short, light-colored hairs that help minimize water loss; its berries were used by settlers to make a rudimentary sauce for bison steaks

View of the Golden Throne from a marked viewpoint along Pleasant Creek Road