Cave River Valley Park
— where the river goes underground for a while.
Not only on a wall.
Cave River Valley Park, on ceramic.
Each tile is finished by hand in our Knoxville studio. Artwork is slowly infused into the ceramic surface under high heat and pressure, and rests beneath a thin glossy finish. The colour lives in the surface, not on top of it.
Pick any four 4-inch tiles — National Parks you've been to, a Smokies set, the four seasons of one place. $ for a set of , cork-backed, ready to live on the table.
Each tile ships in a kraft box, tied with cream ribbon, with a handwritten note from the studio if you'd like to add one.
Three or five different vistas, hung together — a chapter of places you've been, or want to go.
“A small park in Washington County where the Lost River does what it has always done in this country: ducks into the limestone and surfaces somewhere else. There are caves along the bluff, an old grist-mill foundation in the grass, and oak-hickory woods that hold the sound of water you can't quite see. The kind of place locals know and nobody else does. from the studio
The place, in three passes.
Cave River Valley Park sits in northern Washington County, Indiana, on land the county acquired in 2010 to protect a stretch of karst topography along the Blue River drainage. The park covers roughly 80 acres of wooded hollow with several known cave entrances cut into Mississippian limestone. The Lost River system, characteristic of southern Indiana karst, runs partly underground here before resurfacing downstream. The park lies near Campbellsburg, about an hour north of Louisville, and is part of the broader Hoosier National Forest region known for sinkholes and disappearing streams.
The water here writes the landscape. Southern Indiana sits on a band of soluble limestone, and rainwater carries away the rock in slow geological time, leaving sinkholes, springs, and dry streambeds that fill only in flood. The Lost River drainage, named for the way it disappears underground for miles before re-emerging, is one of the most studied karst systems in the Midwest. Within the park, small springs feed clear pools the colour of weak tea where leaves settle. The hollow stays cool in summer; you hear the water before you find it.
The park is open dawn to dusk and free to enter. There are unpaved trails to two of the cave entrances and a primitive shelter near the parking area. The caves themselves are gated and accessible only on guided trips, both for visitor safety and to protect the bat populations that overwinter inside. Spring and fall are the best seasons: wildflowers along the hollow in April, and oak-hickory colour in mid-October. The road in is narrow and gravel; sturdy shoes matter more than directions.
