Gooseberry Falls State Park
A stair-step river drops over dark lava flows before reaching a cobble shore, with CCC structures, forest trails, and the Superior Hiking Trail crossing the park.
Artwork inspired by Birney Quick
The famous Upper, Middle, and Lower falls expose layers of ancient volcanic rock while spring snowmelt and rain radically change their force. Trails and bridges make several viewpoints easy to connect, but wet basalt and crowded overlooks demand attention.
Do not stop at the highway-side waterfall loop. The river mouth, Lake Superior shoreline, Gitchi-Gami State Trail, and CCC-built structures show water moving through a larger landscape. Arrive early on summer weekends and never treat low flow as permission to climb closed rock.
- Geology
- North Shore basalt
- Trail link
- Superior Hiking Trail
- Historic fabric
- CCC construction
Quick guide
- Classic loop
- Link all three falls before choosing an extension
- Add depth
- Follow the river to its Lake Superior mouth
Follow the Gooseberry from lava ledges to open lake
- Start with
- Compare Upper and Lower Falls to see how bedrock steps, channels, and current alter the river’s force.
- Look closely at
- Notice CCC stonework as designed park infrastructure, not natural rock accidentally beside the trail.
- Connect the story
- Follow the river to Lake Superior to connect inland flow with shoreline weather and water level.
- Plan around
- Arrive off-peak and treat wet rock as hazardous even when the falls appear easy to approach.
Good to know
A large highway rest-area lot provides free access to the visitor center and main falls; other state-park uses may still require a vehicle permit.
Notice these
- Upper and Lower falls
- CCC stone structures
- Lake Superior river mouth