Lake Lenore Caves
Lake Lenore Caves Rd
Soap Lake, WA
A short desert climb to a row of caves the great Ice Age floods tore out of solid basalt, where people sheltered for thousands of years.
Lake Lenore Caves are a set of shallow caves worn into the basalt walls of the Lower Grand Coulee, reached by a short but rocky trail that climbs from the highway above Lake Lenore. They are not deep caverns but wide, low shelters, most only ten to twenty feet into the rock, scooped from the cliff face and looking out over the desert coulee below.
What makes them remarkable is how they were made. These caves were not carved slowly by a stream but torn out in days by the Ice Age Missoula floods, some of the most violent floods the planet has known. Water released from a vast glacial lake roared down the Grand Coulee and plucked the basalt apart column by column, leaving the alcoves you can walk into today.
What Guests Love
- Scrambling up a short trail to caves the Ice Age floods carved straight out of the cliff
- Standing inside a shelter that people used for thousands of years, with the coulee spread out below
- The stark, wide-open high-desert quiet of the Lower Grand Coulee
- How much geology and history is packed into a quick half-mile stop
Worth Knowing
- It is an exposed desert climb with little shade, so bring water and go early on hot days
- The caves are shallow shelters, ten to twenty feet deep, not deep caverns, so set your expectations
- Watch your footing on the rocky talus and the cliff edges, and keep an eye out for rattlesnakes in warm months
- A Washington Discover Pass is required to park at the trailhead
Details
Soap Lake, WA
Learn about Lake Lenore Caves
How the floods built the caves
At the end of the last Ice Age, a lobe of glacial ice dammed a river in what is now western Montana and backed up an enormous lake, Glacial Lake Missoula. Again and again the ice dam failed and released the entire lake at once, sending walls of water racing across eastern Washington in the events geologists call the Missoula floods.
One of those flood paths was the Grand Coulee. The churning water plucked fastest at the columns of basalt, prying them loose and eroding pockets into the cliff walls. The Lake Lenore Caves were scoured from those basalt colonnades, which is why they line up along the rock in a row rather than sitting deep in the ground. It is a landscape written entirely by moving water, and it is now part of the congressionally designated Ice Age Floods National Geologic Trail.
Shelter for thousands of years
When the floods finally stopped and the coulee dried, the caves became useful. Talus slopes built up below them and made easy paths up to the openings, and Plateau peoples used the shelters for overnight camps and storage for at least five thousand years. Hunters and gatherers from villages along the Columbia and its tributaries came through this desert corridor, and the caves gave them a dry place out of the wind.
This is living heritage, not just an archaeological curiosity. The caves are still used today for certain Native American religious ceremonies, so visit with the same respect you would bring to any place of ongoing cultural importance, and leave everything as you found it.
The Lower Grand Coulee around you
The caves are one stop in a much larger flood landscape. Just up the coulee is Dry Falls, the scarred headwall of what was once a waterfall far larger than any on earth today, and the string of alkali lakes below, Lake Lenore, Soap Lake, and the others, fills the coulee floor where the floods left basins. The whole drive is a lesson in what happens when a continent-sized flood passes through.
The desert here is high and dry, sagebrush and bunchgrass over black rock, and the light at either end of the day turns the basalt walls gold and violet. It feels remote and a little severe, which is much of its appeal.
Wildlife and the desert seasons
The coulee is a raptor corridor. Watch the cliffs and the sky for hawks, falcons, and golden eagles riding the updrafts, and listen for the pikas and marmots among the talus. Yellow-bellied marmots sun themselves on the rocks, and in the alkali lakes below the water is too mineral for most fish but rich in the tiny life that draws migrating birds.
Spring is the sweet spot, when the desert briefly greens and wildflowers dot the slopes before the summer heat sets in. Summer days can be scorching and shadeless, so early morning is best. Fall brings cool, clear air and long light, and winter turns the coulee stark and often snow-dusted, beautiful but cold and windy.
Closest Boutels
The closest Boutel™ stays, so you can turn this stop into an overnight. Each is an independently owned, editorially selected place to stay.
Things to Do Near Soap Lake
Dry Falls
About 8 miles north
The scarred, three-mile headwall of a waterfall that dwarfed Niagara during the Ice Age floods, with an overlook and interpretive center at the top of the coulee.
Soap Lake
About 6 miles south
A mineral-rich alkali lake and small resort town at the mouth of the coulee, long valued for the reputed healing qualities of its water and black mud.
Lake Lenore
Right below the trailhead
A long, narrow alkali lake on the coulee floor, stocked for a unique fishery and framed by the same basalt walls that hold the caves.