Geologic Formations

Geology of Wupatki
Moenkopi sandstone and Wukoki Pueblo.

NPS photo by Dallas Larsen.

Geology Of Wupatki

Traveling through the four corners states is like jumping into a time machine and going through millions of years of geologic time. Some of the oldest rocks are at the bottom of the Grand Canyon but most of the geology in Wupatki consists of sedimentary rocks from the Permian and Early to Middle Traissic.

The Kaibab (ky-babb) and Moenkopi (moh-en-co-pee) formations are the most prominent sedimentary rock layers in Wupatki. Today these rocks are dry as the sun baked deserts, but a closer look reveals evidence of a much wetter landscape. Ripple marks set in sandstone, ancient mud cracks, and the imprints of shells and other marine life tell the story of dynamic water systems during the Permian and Triassic periods. Wupatki National Monument is on the edge of both the San Francisco Volcanic field and the colorful layers of the Painted Desert.

Paleontologists, scientists who study ancient life by looking at fossils, depend on clues in rocks to understand the history of the local and global events that shape life on earth. The stratigraphy of those rocks is the order in which they were laid down. By looking at the layers in chronological order we can learn about the conditions that created the rocks, the ecology that shaped life at certain times, and the changes of living organisms throughout the fossil record.

Where can these rocks be seen?

You will see many of the layers within the Moenkopi formation throughout the southeastern areas of the monument. Since most of the pueblo walls are built with these naturally straight ‘bricks’ you can easily view them while also absorbing the dynamic human history. Prominent in-situ sandstone and shale outcrops can be seen along the Wupakti and Wukoki pueblo trails.

The Kaibab Limestone is most easily seen by visiting the western half of the monument. There are in-situ outcrops of Kaibab layers at mile 24 along the loop road and along the Lomaki Pueblo Trail. Visiting Doney Mountain or Citadel Pueblo and climbing to the top of either trail will provide a greater geologic context.

Click HERE to view the USGS Geologic map of Wupatki National Monument.

Ranger shows strength of blowhole with hat.

Blowholes and Earth Cracks

Wupatki National Monument is home to a surprising phenomenon where air blows directly out of the ground beneath your feet. At the end of the Wupatki Pueblo trail is one of several ‘blow holes’ where visitors can experience what some have called the ‘breathing earth’.

Between 80 and 40 million years ago, as the Pacific and North American plates were colliding, a near-vertical fault occurred through roughly 300 ft of the Kaibab Limestone and Moenkopi Sandstone layers. This fault allowed ground water to penetrate into and dissolve the limestone creating a huge underground crack system that spans several miles through the monument. The behavior of the blowholes is dependent on several factors related to the weather. When the air is cool and dense the air rushed into the ground. When the air is warm and less dense then the air is blowing out.

The blowhole crack system has not been fully explored or mapped because it is too narrow for human passage but, by measuring the amount of air blowing out of the holes, scientists estimate it to be 7 billion cubic feet of air space. That’s enough air to fill about 84 thousand hot air balloons! Archeologists are unsure what the ancestral Puebloan residents of Wupatki thought of this natural wonder. No structures were built around the hole near Wupatki Pueblo during that time.

Last updated: March 7, 2018

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