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The National Park Service calls this Wyoming site an aquarium in stone, and they’re not wrong

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The Fossil Butte National Monument’s sign, featuring the distinctive National Park Service style, proudly marks the entrance to this renowned National Monument in Wyoming.

It’s an ancient aquarium frozen in stone

Southwest Wyoming doesn’t look like much from the highway. Flat sagebrush, big sky, the occasional pronghorn.

But about 15 miles west of the small town of Kemmerer, the ground holds something that took 52 million years to make.

Fossil Butte National Monument covers 8,198 acres of flat-topped ridges where an ancient lake once sat.

The National Park Service calls it “An Aquarium in Stone,” and once you walk into the visitor center, you’ll understand why. Admission is free, the crowds are thin, and the fossils are real.

Cliffs rise straight up from a steeply sloping hillside covered in trees and bushes. Cliffs along the ridge known as Fossil Butte.

A subtropical lake that vanished 52 million years ago

Long before Wyoming was Wyoming, this corner of the continent looked nothing like it does today.

During the Eocene Epoch, the climate here was warm and humid, closer to what you’d find in the southeastern United States now.

A freshwater body called Fossil Lake spread across the land, the smallest of three great prehistoric lakes that together covered parts of what are now Wyoming, Utah, and Colorado.

Over about two million years, fine sediment drifted to the lake bottom in thin layers, sealing whatever died there in remarkable detail.

Dynamic Lake, a stunning landscape feature in Fossil Butte National Monument, Wyoming, showcases the geological splendor and natural beauty of the National Park Service offerings.

Calm, oxygen-poor water that locked creatures in time

What made this lake different was what happened at the bottom. The deep water held almost no oxygen, which kept scavengers away from anything that sank.

When a fish died, it didn’t get picked apart. It settled into the soft sediment and stayed.

That process repeated itself for two million years, building up the fossil-rich layers that scientists now call the Green River Formation, one of the most significant fossil deposits anywhere on Earth.

The preservation isn’t just good. In many cases, it’s close to perfect.

Fossil Butte National Monument Fossil Butte National Monument is a United States National Monument managed by the National Park Service, located 15 miles (24 km) west of Kemmerer, Wyoming, United States. It centers on an extraordinary assemblage of Eocene Epoch (56 to 34 million years ago) animal and plant fossils associated with Fossil Lake—the smallest lake of the three great lakes which were then present in what are now Wyoming, Utah, and Colorado. The other two lakes were Lake Gosiute and Lake Uinta. Fossil Butte National Monument was established as a national monument on October 23, 1972. Fossil Butte National Monument preserves the best paleontological record of Cenozoic aquatic communities in North America and possibly the world, within the 50-million-year-old Green River Formation — the ancient lake bed. Fossils preserved — including fish, alligators, bats, turtles, dog-sized horses, insects, and many other species of plants and animals — suggest that the region was a low, subtropical, freshwater basin when the sediments accumulated, over about a 2 million-year period. During the Eocene this portion of Wyoming was a sub-tropical lake ecosystem. The Green River Lake System contained three ancient lakes, Fossil Lake, Lake Gosiute, and Lake Uinta. These lakes covered parts of southwest Wyoming, northeast Utah and northwestern Colorado. Fossil Butte is a remnant of the deposits from Fossil Lake. Fossil Lake was 40 to 50 miles (64 to 80 km) long from north to south and 20 miles (32 km) wide. Over the two million years that it existed, the lake varied in length and width. Fossil Buttes National Monument contains only 13 square miles (8,198 acres (33,180,000 m2)) of the 900-square-mile (595,200 acres (2.409×109 m2)) ancient lake. The ancient lake sediments that form the primary fossil digs is referred to as the Green River Formation. In addition to this fossil-bearing strata, a large portion of the Wasatch Formation, river and stream sediments, is within the national monument. The Wasatch Formation represents the shoreline ecosystem around the lake and contains fossil teeth and bone fragments of Eocene mammals. Among these are early primates and horses.

Fish, bats, crocs, and early horses the size of dogs

Researchers have pulled fish, crocodilians, turtles, bats, birds, insects, and plants out of this formation.

They’ve identified 27 fish species from Fossil Lake alone, along with more than 100 varieties of insects and hundreds of plant species. Some fossils show soft tissue and skin impressions.

A few preserve delicate wing structures down to the veins. Paleontologists use a German term, Lagerstaette, for sites where preservation reaches this level.

It means a deposit of outstanding quality. Fossil Butte qualifies.

Fossil Butte National Monument Fossil Butte National Monument is a United States National Monument managed by the National Park Service, located 15 miles (24 km) west of Kemmerer, Wyoming, United States. It centers on an extraordinary assemblage of Eocene Epoch (56 to 34 million years ago) animal and plant fossils associated with Fossil Lake—the smallest lake of the three great lakes which were then present in what are now Wyoming, Utah, and Colorado. The other two lakes were Lake Gosiute and Lake Uinta. Fossil Butte National Monument was established as a national monument on October 23, 1972. Fossil Butte National Monument preserves the best paleontological record of Cenozoic aquatic communities in North America and possibly the world, within the 50-million-year-old Green River Formation — the ancient lake bed. Fossils preserved — including fish, alligators, bats, turtles, dog-sized horses, insects, and many other species of plants and animals — suggest that the region was a low, subtropical, freshwater basin when the sediments accumulated, over about a 2 million-year period. During the Eocene this portion of Wyoming was a sub-tropical lake ecosystem. The Green River Lake System contained three ancient lakes, Fossil Lake, Lake Gosiute, and Lake Uinta. These lakes covered parts of southwest Wyoming, northeast Utah and northwestern Colorado. Fossil Butte is a remnant of the deposits from Fossil Lake. Fossil Lake was 40 to 50 miles (64 to 80 km) long from north to south and 20 miles (32 km) wide. Over the two million years that it existed, the lake varied in length and width. Fossil Buttes National Monument contains only 13 square miles (8,198 acres (33,180,000 m2)) of the 900-square-mile (595,200 acres (2.409×109 m2)) ancient lake. The ancient lake sediments that form the primary fossil digs is referred to as the Green River Formation. In addition to this fossil-bearing strata, a large portion of the Wasatch Formation, river and stream sediments, is within the national monument. The Wasatch Formation represents the shoreline ecosystem around the lake and contains fossil teeth and bone fragments of Eocene mammals. Among these are early primates and horses.

More than 400 fossils packed inside the visitor center

Walk into the visitor center and the first thing that stops you is scale.

A replica of a 13-foot crocodilian stretches across the room, modeled on a fossil from the formation.

Beyond it, you’ll find a slab containing 356 fish that died together in a single event, locked into the rock just as they fell. One display holds some of the oldest complete bat fossils ever found.

The Fish Wall exhibit lines up 49 original fossils representing 16 of the 27 fish species from Fossil Lake. Nothing here is decoration.

Fossil Exhibit at Fossil Butte Nat'l Monument, Wyoming.

A road-length timeline of Earth’s entire 4.54-billion-year history

Before you reach the visitor center building, the sidewalk starts telling a story. Every nine inches of the path represents one million years of Earth’s history, with major events marked along the way.

The timeline wraps around the building and ends at the present day.

When you get to the end and look back at where recorded human history appears on that scale, you’re looking at a sliver just a few inches long.

Standing there with 52-million-year-old fossils inside puts that in sharp relief.

Looking across a valley filled with green bushes and shrubs. A trail cuts across from the bottom right diagonally but gets lost in the greenery. A path of stairs is visible immediately to the left in the foreground and then again further down. Looking down from the top of the loop through the historic quarry down onto the trail and across the valley. If hiking all the way into the historic quarry you will gain almost 700 feet in elevation.

Hike through the rock layers where early fossil hunters dug

The Historic Quarry Trail is a 2.5-mile loop that climbs about 688 feet through exposed layers of the Wasatch and Green River Formations.

Wayside panels along the route explain the geology and the plants and wildlife of the high desert.

A short side loop takes you to the spot where early fossil collectors actually worked, cutting into the same butte that researchers still study today. There’s no shade on this trail, no water, and no restrooms.

Bring more than you think you need, and bring sunscreen.

A low-growing plant with a lot of purple bell-shaped flowers that face outwards. There are seven species of penstemon in the park. It is unknown what species this is. Several species can be seen along the Nature Trail and Historic Quarry Trail.

An aspen grove at 7,000 feet with benches and big views

The Fossil Butte Nature Trail runs 1.5 miles through sagebrush steppe and a spring-fed aspen grove, starting at about 7,000 feet. Benches at the top give you a long look across the butte and the surrounding landscape.

In summer it’s a solid morning walk with interpretive signs explaining what you’re seeing. Come winter, when snow covers the access road, the trail draws snowshoers and cross-country skiers.

The aspen grove is especially worth the stop if you’re birding, with over 50 species documented in that stretch alone.

Pronghorn antelope in the Wyoming desert

A scenic drive up a ridgeline with pronghorn along the road

The scenic drive runs about 5.5 miles one way from the visitor center area to the top of a ridge. The lower portion is paved.

The upper section turns to steep gravel and isn’t a good idea for RVs or trailers.

From the top, the Green River Basin spreads out below you, and on clear days the Uinta Mountains show up on the horizon. The drive is slow going in the best possible way.

Pronghorn, mule deer, and birds of prey tend to show up without warning along the upper stretch.

Fossil Butte National Monument Fossil Butte National Monument is a United States National Monument managed by the National Park Service, located 15 miles (24 km) west of Kemmerer, Wyoming, United States. It centers on an extraordinary assemblage of Eocene Epoch (56 to 34 million years ago) animal and plant fossils associated with Fossil Lake—the smallest lake of the three great lakes which were then present in what are now Wyoming, Utah, and Colorado. The other two lakes were Lake Gosiute and Lake Uinta. Fossil Butte National Monument was established as a national monument on October 23, 1972. Fossil Butte National Monument preserves the best paleontological record of Cenozoic aquatic communities in North America and possibly the world, within the 50-million-year-old Green River Formation — the ancient lake bed. Fossils preserved — including fish, alligators, bats, turtles, dog-sized horses, insects, and many other species of plants and animals — suggest that the region was a low, subtropical, freshwater basin when the sediments accumulated, over about a 2 million-year period. During the Eocene this portion of Wyoming was a sub-tropical lake ecosystem. The Green River Lake System contained three ancient lakes, Fossil Lake, Lake Gosiute, and Lake Uinta. These lakes covered parts of southwest Wyoming, northeast Utah and northwestern Colorado. Fossil Butte is a remnant of the deposits from Fossil Lake. Fossil Lake was 40 to 50 miles (64 to 80 km) long from north to south and 20 miles (32 km) wide. Over the two million years that it existed, the lake varied in length and width. Fossil Buttes National Monument contains only 13 square miles (8,198 acres (33,180,000 m2)) of the 900-square-mile (595,200 acres (2.409×109 m2)) ancient lake. The ancient lake sediments that form the primary fossil digs is referred to as the Green River Formation. In addition to this fossil-bearing strata, a large portion of the Wasatch Formation, river and stream sediments, is within the national monument. The Wasatch Formation represents the shoreline ecosystem around the lake and contains fossil teeth and bone fragments of Eocene mammals. Among these are early primates and horses.

Watch rangers dig real fossils out of the rock

On Fridays and Saturdays in summer, rangers lead groups up to an active research quarry about three-quarters of a mile uphill with more than 300 feet of elevation gain.

At the top, you watch how paleontologists actually extract and prepare fossils, which turns out to be slower and more precise than most people expect.

Back at the visitor center, Fossil Preparation Demonstrations let you see rangers working on real specimens up close. Shorter ranger talks run on weekends and some weekdays.

None of these programs cost anything, and none require a reservation.

Greater Sage Grouse performing mating display on a lek

Golden eagles, sage grouse and 93 bird species in the sagebrush

The monument supports more than 100 species of mammals, reptiles, amphibians, and birds. Pronghorn and mule deer move through the sagebrush regularly, and elk show up as well.

Birdwatchers have recorded 93 species here, including golden eagles, red-tailed hawks, sage grouse, and western meadowlarks. The aspen groves concentrate the bird activity, with more than 50 species in those areas alone.

Smaller animals like rabbits, chipmunks, and ground squirrels pick up toward dusk. One thing you won’t find: rattlesnakes are absent from the monument entirely.

GIP Julie Rozen cleaning fossils with a Junior Ranger at Fossil Butte National Monument, Wyoming. (NPS Photo by Julie Rozen, GIP)ulie Rozen, GIP)

Fewer visitors means rangers actually have time for you

Fossil Butte ranks among the least-visited units in the entire National Park system. On most days, that means you get the trails to yourself and the rangers actually have time to stop and talk.

The visitor center stays open year-round, with longer hours from Memorial Day through Labor Day and shorter hours the rest of the year.

The landscape changes hard between seasons, green sagebrush giving way to snow-covered ridgelines by winter.

The monument sits at the edge where the Rockies meet Wyoming’s central desert, and the mix shows in the terrain around every bend.

A road in Fossil Butte National Monument leads into Fossil Butte Valley, winding past Dynamic Lake in Wyoming's unique landscape and geological features.

Visit Fossil Butte National Monument in Wyoming

To see one of the country’s richest fossil sites, head to Fossil Butte National Monument about 15 miles west of Kemmerer, Wyoming, off U.S. Highway 30. Admission is free year-round with no pass required.

In summer, the visitor center opens daily from 8 a.m. to 5:30 p.m. Winter hours run Monday through Saturday, 8 a.m. to 4:30 p.m., closed Sundays and major holidays.

The nearest airports are in Rock Springs, Wyoming, about 130 miles away, and Salt Lake City, Utah, about 150 miles out. Check the official website for current program schedules before you go.

This article was created with AI assistance and human editing.

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John Ghost is a professional writer and SEO director. He graduated from Arizona State University with a BA in English (Writing, Rhetorics, and Literacies). As he prepares for graduate school to become an English professor, he writes weird fiction, plays his guitars, and enjoys spending time with his wife and daughters. He lives in the Valley of the Sun. Learn more about John on Muck Rack.

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