Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Moro Rock

Inselbergs and Crystalline Monoliths

Moro Rock is a granite dome rock formation in Sequoia National Park, California, at the head of Moro Creek between Giant Forest and Crescent Meadow, reaching an elevation of 6,725 feet with a topographic prominence of 245 feet. The dome dates to the Cretaceous period and formed through exfoliation, a process in which the erosion of overlying rock reduces compression on the granite beneath, causing it to expand outward; the fractures produced by this process tend to cut corners rather than edges, which over time rounds the rock into a dome shape. A 797 foot stairway of about 400 steps, built by the Civilian Conservation Corps in 1931, allows visitors to climb to the summit, from which much of the park, including the Great Western Divide, is visible.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Moro Rock

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Moro Rock
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Moro Rock
Sources
1. Moro Rock (Wikipedia)
Wikipedia article lead, protection designation
Quote, Wikipedia article lead, protection designation
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 hea
View the Source
Wikidata: Moro Rock
Wikidata Q2156029, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.