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Mima Mounds

The mysterious mounds of Mima Prairie
The mysterious mounds of Mima Prairie
Photo by Dan Coe, WGS/DNR

What is it and why visit?

Purple camas blossoming at Mima Prairie
Purple camas blossoming at Mima Prairie
Photo by Dan Coe, WGS/DNR

In Thurston County, Washington, mysterious mounded landforms create a wavy surface at the 637-acre Mima Mounds Natural Area Preserve (NAP). This fascinating geological phenomenon will likely leave you wondering, “How did these mounds form?” Don’t worry, you’re not the only person asking this question. Researchers are also puzzled. For many, the appeal is more than the mystery—it’s the views and picturesque hikes. As you wander the trails of this secluded natural area, the raw beauty of the landscape will consume your senses. Enjoy views of Mount Rainier and Mount St. Helens to the east, and the green hills of Capitol State Forest to the west. In the spring, purple camas flowers speckle the lush green grass that blankets these puzzling landforms. Come visit the Mima mounds and see what theory you come up with while enjoying this beautiful Washington natural area.

Morning fog over Mima Mounds Natural Area Preserve
Morning fog over Mima Mounds Natural Area Preserve
Photo by WGS UAV Team

Play the video below for more views of the Mima mounds at Mima Prairie!

Geologic story

More than 30 theories have been published about the origins of the mysterious dome-shaped mounds that speckle Mima Prairie. Some scientists think the mounds were built by pocket gophers. These animals dig tunnels, piling the scooped out earth into mounds. Others think geology played a role. According to the sun cup theory, streams dropped sediment into evaporation pits found on thin layers of ice. When the ice melted, it left behind mounds of sediment. The frost-polygon theory is based on the idea that water-soaked soil expands as it freezes, creating mounds. Perhaps earthquake shaking created these perplexing piles. Despite an abundance of popular theories, nobody knows for sure how the mounds formed.

Trail through the Mima mounds
Trail through the Mima mounds
Photo by Dan Coe, WGS/DNR

So if scientists can’t agree on one of these theories, what do we know? The Mima mounds are 3 to 8 feet tall and 8 to 60 feet wide. They typically sit close together, with as many as 10 mounds per acre. Cobbles of multiple rock types sit in the low spots between the mounds. Another piece of the puzzle is the fact that we seem to find Mima mounds where the edges of the great ice age glaciers used to be.

These are all things that can be observed above ground, but what secrets lie beneath the surface? Scientists have discovered that the mounds rest on 15,000-year-old glacial outwash. Outwash is a collection of sediments dropped at the edges of glaciers by meltwater streams. However, the mounds themselves do not have the layers characteristic of outwash—they are made of dark sand mixed with gravel. This tells scientists that the mounds began forming sometime after the outwash was deposited.

Geologist Tim Walsh examines a cross section of a Mima mound
Geologist Tim Walsh examines a cross section of a Mima mound
Photo by Dan Coe, WGS/DNR

Much of the evidence seems to suggest a glacial origin for the Mima mounds, but does that mean pocket gophers or earthquakes didn’t play a role? We may never know for sure, but in the meantime scientists can still enjoy the debate!


We recently published an educational comic booklet about the Mima mounds. Check it out by clicking here or on the link below.

This site is a National Natural Landmark. The National Natural Landmarks Program recognizes and encourages the conservation of sites that contain outstanding biological and geological resources.

Fun Fact

There are similar mounds in other parts of the country and the world that are sometimes referred to as Mima-like mounds or even “pimple mounds”. “Mima mound” is a term used only to describe the mounds of the southern Puget Lowland within Washington State.

What to see and do

Getting There

From Interstate 5, take exit 95 and take Maytown Road SW for 3 miles to the town of Littlerock. Drive straight through Littlerock (don’t follow the road left at the gas station!). A little less than 1 mile west of Littlerock is a T-intersection. Turn right, then look for a sign and turn-off on your left, about 0.8 miles down the road. It is easy to miss this turn because the sign is hidden by the trees. Turn left into the NAP and follow a one-lane road to the second parking area where there is a trailhead.

Nearby Amenities

Photo gallery

Bibliography

Bretz, J. H., 1913, Glaciation of the Puget Sound region: Washington Geological Survey Bulletin 8, 244 p., 3 plates. [https://www.dnr.wa.gov/publications/ger_b8_glaciation_pugetsound.pdf]

Gabet, E. J.; Perron, J. T.; Johnson, D. L., 2014, Biotic origin for Mima mounds supported by numerical modeling: Geomorphology, v. 206, p. 58–66. [https://doi.org/10.1016/j.geomorph.2013.09.018]

Logan, R. L.; Walsh, T. J., 2009, Mima mounds formation and their implications for climate change [abstract]: Northwest Scientific Association Annual Meeting. [https://www.dnr.wa.gov/publications/ger_presentations_nwsa_2009_logan.pdf?91nbbk]

Miller, M. B.; Cowan, D. S., 2017, Roadside geology of Washington, second edition: Mountain Press Publishing Company, 378 p.

Washburn, A. L., 1988, Mima mounds—An evaluation of proposed origins with special reference to the Puget Lowlands: Washington Division of Geology and Earth Resources Report of Investigations 29, 53 p.

Tucker, Dave, 2015, Geology underfoot in western Washington: Mountain Press Publishing Company, 374 p.