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Monument Rocks - Butte
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Monument Rocks

description Monument Rocks Overview

Monument Rocks, also called the Chalk Pyramids, is a group of tall chalk formations in Gove County, Kansas. The towers, arches, and isolated blocks consist of Niobrara Chalk deposited in the Western Interior Seaway during the Late Cretaceous, and fossils of marine organisms occur in the surrounding rock. The site is designated a National Natural Landmark and is reached across privately owned ranchland open to respectful public visitation.

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What are the Monument Rocks in Kansas?

Monument Rocks, also called the Chalk Pyramids, is a group of tall chalk formations located in Gove County, Kansas. The area consists of isolated towers, arches, and large blocks.

How were the Monument Rocks formed?

The formations consist of Niobrara Chalk deposited in the Western Interior Seaway during the Late Cretaceous period. The soft chalk was carved into towering shapes by millions of years of wind and water erosion.

What type of fossils are found at Monument Rocks?

Because the chalk was formed from marine sediments, fossils of Late Cretaceous marine organisms occur frequently in the area. Visitors and paleontologists have found remains of sharks, bony fish, and large marine reptiles like mosasaurs.

Are the Monument Rocks a protected National Park?

While they are a recognized National Natural Landmark, the Monument Rocks are located on private land rather than within a national park. The owners graciously allow public access to visitors as long as they respect the fragile formations.

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