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Geological Formation

Chiricahua Hoodoos

Volcanic Formations

The Chiricahua hoodoos are a dense field of standing rock spires, columns and balanced rocks within Chiricahua National Monument in southeastern Arizona, carved from a thick sheet of rhyolitic volcanic tuff deposited by the eruption of the Turkey Creek Caldera roughly 27 million years ago, one of the more voluminous known eruptions in the region. As the welded tuff cooled it fractured into a dense network of vertical joints, and subsequent weathering, including water erosion and freeze-thaw cycles, widened those joints and sculpted the rock between them into thousands of narrow standing pillars and precariously balanced boulders. The formation's maze-like landscape of spires has given the monument its popular nickname, the "Wonderland of Rocks."

Facts
Classification
Protected Status
National Monument or Landmark 1
Connections

Associated With

Tuff, Materials
Source Chiricahua National Monument (Wikipedia)

Caused By

Erosion, Processes
Source Chiricahua National Monument (Wikipedia)
Volcanism, Processes
Source Chiricahua National Monument (Wikipedia)

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Sources
1. Chiricahua National Monument (Wikipedia)
  • Lead section
    The monument was established on April 18, 1924, to protect its extensive hoodoos and balancing rocks.
  • Associated With: Tuff, Article text, rock Tuff
    The thick, white-hot ash spewed forth from the nearby Turkey Creek Caldera, cooled and hardened into rhyolitic tuff, laying down almost 2,000 ft (610 m) of highly siliceous, dark volcanic ash and pumice.
  • Caused By: Volcanism, Article text, process Volcanism
    Located approximately 36 miles (58 km) southeast of Willcox, Arizona, the monument preserves the remains of an immense volcanic eruption that shook the region about 27 million years ago.
  • Caused By: Erosion, Article text, process Erosion
    The volcanic material eventually eroded into the natural rock formations of the present monument.
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