Vast, majestic and ever changing
In October 2016, my partner and I spent several wonderful days hiking in three of Southern Utah’s parks. Each offered a special geological wonderland to explore. Layers of sedimentary rock were formed over millions of years when today’s inland desert region was under water. About 13 million years ago, the sea bed was uplifted to form a series of plateaux broken by fault lines. Over the centuries, water and wind have sculpted exposed rock layers of varying hardness and mineral content into fantastic formations in rich shades of red, purple, yellow and white.
Bryce Canyon features giant rock amphitheatres lined by mazes of pinnacles nicknamed “hoodoos.” True to native Paiute legend, they look like weird creatures which have been turned to stone, standing as sentinels over the passage of time. Along the trails snaking from the rim down to the floor, we saw trees and shrubs adapted to harsh conditions, anchored on exposed sandstone hillsides or thrusting upward toward the light between steep rock walls. We marveled at how some trees become eerily twisted when they die slowly in portions as their roots are exposed. On the Peekaboo Trail, we randomly asked a passing couple to take our photo and discovered they were from Auckland. Facing the maze of spires, I understood why Ebenezer Bryce, the Mormon pioneer for whom the park was named, referred to the landscape as “a hell of a place to lose a cow.” We lingered in a cold wind to watch the sunset from the rim. A nearby chipmunk appeared to do the same, perched at the very tip of a tree root jutting out over the chasm. …
