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Silvertip Park Services Ltd.
Pinnacles Provincial Park
About This Park
Pinnacles Provincial Park comprises approximately 124 hectares of pine forest overlooking Baker Creek. The park is a popular day-use area and is easily accessible from Quesnel. From the Pinnacles viewpoint, visitors enjoy the unique formation of “Hoodoos,” and a picturesque view of the city of Quesnel and Baker Creek.
The park is open year-round for day-use and sightseeing despite the locked gate at the entrance; camping is not permitted. The park provides an opportunity for a pleasant 1 km hike along a well maintained trail to the viewpoint; allow 15 minutes for access. Horseback riding in the park is not permitted. The hoodoos are fragile, please do not climb on or near them.
Established Date: September 18, 1969
Park Size: 124.39 hectares
Know Before You Go
- The viewpoint is an area with steep cliffs. Please exercise extreme caution and stay in designated viewing areas.
- Bring your own drinking water as potable water is not available in the park.
- Climbing on rock formations accelerates erosion and destroys the scenic value of the area. Please view the hoodoos from the established viewpoint only; remain behind the fence.
Location and Maps
Nature and Culture
- Conservation: Pinnacles Provincial Park protects a very unique formation of hoodoos. These hoodoos began their formation 12 million years ago, when molten lava flowing over the earth’s surface cooled in flat basalt layers over older layers of ash and rock. The Ice Age followed, and when the ice mass receded, melt-water streams eroded the valley below Pinnacles Park. The hoodoos are formed from the effects of this natural erosion and weathering. The basalt is eroded away, revealing the more resistant ash layer, and often producing vivid bands of color as individual basalt layers are removed. The hoodoos at Pinnacles Provincial Park are fragile, since they are still undergoing these forces of erosion and weathering. The Pinnacles viewpoint provides an unobstructed view of these impressive geological formations.