Escalante Petrified Forest State Park

Escalante Petrified Forest State Park
Escalante Petrified Forest State Park
IUCN category V (protected landscape/seascape)
	Large piece of petrified wood in Escalante Petrified Forest State Park
	Location of Escalante Petrified Forest State Park in Utah Escalante Petrified Forest State Park (the United States)
Location	Garfield, Utah, United States
Coordinates	37°47′16″N 111°37′46″W / 37.78778°N 111.62944°W
Area	1,350 acres (5.5 km2)
Elevation	5,900 ft (1,800 m)
Established	1963
Visitors	73,969 (in 2022)
Governing body	Utah State Parks

Escalante Petrified Forest State Park (also known as Escalante State Park) is a

Jurassic Period). The Petrified Forest Trail is a one-mile (1.6 km) loop, winding up the side of a mesa to the top where most of the fossil wood occurs. Logs two feet or more in diameter are seen at several places along the trail where it is eroding from the conglomerate capping the mesa. This conglomerate lies near the top of the Brushy Basin Member of the Morrison Formation.^[4] The wood is multicolored (mostly red, yellow, white, and black) and was prized by hobbyists before the Park was established. The logs are believed to be of conifers that were transported by a river before being buried and later fossilized as agate

. A 50 foot (15m) log is displayed near the trail head and is one of the most complete fossil logs known from the Morrison Formation.

The Sleeping Rainbows trail is an optional .75-mile (1.21 km) loop off the Petrified Forest Trail. This section is much steeper and requires scrambling and climbing over rocks.[5]

In 1954 Wide Hollow Reservoir was constructed to provide irrigation for the town of Escalante. The reservoir is stocked with large mouth bass, crappie, tiger trout, rainbow trout and bluegill, and is popular for water sports including swimming, boating and fishing.

Petrified wood
Petrified wood
Large piece of petrified wood
Balanced rock
Morrison Formation
Petrified wood is made through a fossilization process called permineralization, when minerals transported by water fill in all the open spaces of an organism or organic tissue
Petrified logs in place
Fossil log displayed at Escalante Petrified Forest State Park, Utah. This 50 foot (15 m) log is one of the longest known from the Morrison Formation

References

This article incorporates public domain material from the website of the Utah Division of State Parks.

^ ^a ^b "Escalante Petrified Forest State Park Resource Management Plan" (PDF). State of Utah Natural Resources: Division of Parks and Recreation. September 2005. Retrieved February 5, 2011.
^ "Escalante Petrified Forest State Park: About the Park". Utah State Parks. Archived from the original on March 16, 2011. Retrieved February 5, 2011.
^ "Park Visitation Data". Utah State Parks. July 6, 2023.
^ Morgan, S., B.W. Lindsay and A.P. Williams 2010. Geology of Escalante State Park, Utah. Pp. 429-436 in The Geology of Utah Parks and Monuments. Utah Geological Association Publication 28
^ "Escalante Petrified Forest State Park". Utah State Parks.

External links