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. (September 2019)

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