Gooseberry Falls is the gateway to the North Shore. It is known for its spectacular waterfalls, river gorge, Lake Superior shoreline, Civilian Conservation Corps log and stone structures, and north woods wildlife. Listen to the thunderous roar of the Upper, Middle and Lower Falls of the Gooseberry River as it plummets through a rocky gorge. Watch for waves, ships, or the moon rise on Lake Superior from an ancient lava flow known as the Picnic Flow.
Hike or ski to see the Fifth Falls through a forest of evergreens, aspen, and birch, and enjoy camping in modern campsites, picnicking, and relaxing along the Lake Superior shoreline or the Gooseberry River.

To get the most out of your visit, stop by the Joseph N. Alexander Visitor Center where you can find park information, interpretive displays, a park video, Nature Store, and more. Don't miss the Gateway Plaza for outdoor interpretive signs on area resources and history.

Wildlife
The park has recorded over 225 species of birds that nest or visit the park, 46 species of mammals, and ten species of reptiles and amphibians. Of special interest to visitors are white-tailed deer, black bears, gray wolves, pine martens, migratory Lake Superior salmon and trout, a variety of conifer-dependent birds, ravens, and the herring gulls that establish nesting colonies along the lakeshore. During fall and spring, many migratory birds can be seen because the park is along the North Shore flyway.

History
The park is named after the magnificent set of falls along the Gooseberry River. A French map from 1670 names the river Riviere des Groseilliers after Medard Chouart sieur des Groseilliers who visited the area a decade earlier. The name Groseilliers translates to Gooseberries in English. With the rise of North Shore tourism in the 1920s, there was a concern that the highly scenic North Shore would be accessible only to the rich. As a result the Legislature authorized preservation of the area around Gooseberry Falls in 1933, and the Civilian Conservation Corps (CCC) began to develop the park the following year. CCC crews built the park's stone and log buildings and the 300-foot long 'Castle in the Park' stone retaining wall. They also laid out the original campground, picnic grounds and trails. The area officially became Gooseberry Falls State Park in 1937. The CCC camps closed in 1941, but the park's CCC legacy lives on in the form of the CCC-style visitor center/wayside rest and the Highway 61 bridge that opened in 1996.

Geology
Geologists have determined that about 1.1 billion years ago, the Earth's crust began to split apart along a great rift zone now covered by Lake Superior. Huge volumes of lava flowed out onto the surface and cooled to form volcanic bedrock, mainly the dark type known as basalt. Several lava flows can be seen at the Upper, Middle, and Lower Falls and south of the Gooseberry River along the Lake Superior shore. The rifting also caused the flows to tilt gently toward the lake. These basalt lava flows, all along the North Shore, are also the birthplaces of Lake Superior agates.

About two million years ago, the Great Ice Age began as periodic glaciers (up to a mile thick) advanced into the region from the north. As they ground across the area, they changed the landscape dramatically, especially by excavating the whole basin now occupied by Lake Superior. About 10,000 years ago the last glacier melted back, allowing the basin to fill with water and starting the erosional process that creates the river gorges and waterfalls. Today, water, wind, and weather continue to shape the North Shore.

Landscape
Rocky Lake Superior shoreline, five waterfalls, Gooseberry River and gorge, Agate Beach and the Picnic Flow highlight the park. Trails lead through a fairly diverse vegetative cover of mixed evergreen, aspen and birch forests that provide habitat for a variety of birds, plants and other animals. Because the local climate is moderated by Lake Superior, some disjunct populations of arctic-alpine plants can be found in the park.