Moro Rock

For the volcanic plug in Morro Bay, see Morro Rock.

Moro Rock
View of Moro Rock from Potwisha (near Hospital Rock), Sequoia National Park
Highest point
Elevation	6,725 ft (2,050 m)
Prominence	245 ft (75 m)
Coordinates	36°32′39″N 118°45′54″W
Geography
Moro Rock Sequoia National Park, Tulare County, California, United States Moro Rock Moro Rock (the United States)
Parent range	Sierra Nevada
Topo map	USGS Giant Forest
Geology
Rock age	Cretaceous
Mountain type	Granite dome
Climbing
First ascent	1861, by Hale Tharp, John Swanson and George Swanson (first recorded ascent by non-natives)
Easiest route	Hike

Moro Rock is a granite dome rock formation in Sequoia National Park, California, United States. It is located in the center of the park, at the head of Moro Creek, between Giant Forest and Crescent Meadow. A stairway, designed by the National Park Service and built in 1931, is cut into and poured onto the rock, so that visitors can hike to the top. The view from the rock encompasses much of the Park, including the Great Western Divide. Use of this trail is discouraged during thunderstorms and when it is snowing.

The name "Moro Rock" derives from a blue roan mustang of color the Mexicans call moro, owned by one Mr. Swanson of Three Rivers in the 1860s.

Recreation

The road to Moro Rock is closed in winter, so visitors need to hike 2 miles to reach the viewpoint. The road is open in summer so the hike is shortened. The 1996 general plan for the park calls for the road to Moro to be closed, and replaced by a shuttle. As of June 2012, the road is open to general traffic only during weekdays; on weekends, the shuttle is running and the road is closed to general traffic. The west face of Moro Rock offers 1,000 vertical feet of cracks and knobs for rock climbing. However, climbing is prohibited during peregrine falcon nesting season on the South and East faces (up to Full Metal Jacket).

Geology

Moro Rock is a dome-shaped granite monolith. Common in the Sierra Nevada, these domes form by exfoliation, the spalling or casting off in scales, plates, or sheets of rock layers on otherwise unjointed granite. Outward expansion of the granite results in exfoliations. Expansion results from load relief; when the overburden that once capped the granite has eroded away, the source of compression is removed and the granite slowly expands. Fractures that form during exfoliation tend to cut corners. This ultimately results in rounded dome-like forms.

Stairway

Moro Rock Stairway
U.S. National Register of Historic Places
Built	1931
Architect	National Park Service
NRHP reference No.	78000283
Added to NRHP	December 29, 1978

The first stairway leading to the summit of Moro Rock was constructed of wood and installed in 1917. This stairway deteriorated significantly by the late 1920s, and was replaced in 1931 by the present Moro Rock Stairway, built by the Civilian Conservation Corps. Unlike the earlier stairway, the new stairway adopted a design policy of blending with the natural surfaces to the greatest extent possible. The 797-foot-long stairway was designed by National Park Service landscape architect Merel S. Sager and engineer John Diehl, following natural ledges and crevices. It has 400 steps that lead to the summit of Moro Rock. Changes since the original construction have impaired the integrity of the design.

External links

Media related to Moro Rock at Wikimedia Commons

• "Moro Rock". Summitpost.org. Retrieved 2006-12-03.
• "Giant Forest Points of Interest, Summer". Sequoia & Kings Canyon National Parks. National Park Service. Retrieved 2009-01-14.
• "Moro Rock Summit interactive 360˚ panorama". 360Around.com. Retrieved 2010-06-01.