Beware, this post has a lot of hoodoos. Really, awesome hoodoos.
Bryce Canyon National Park is famous for its magnificent collection of hoodoos, which are caused by erosion over a long period of time. These tall chimney-like stacks of rocks form all over the Southwest. I’ve already showed you them from nearby Cedar Breaks in Central Utah and from Chiricahua in southern Arizona. However, Bryce’s collection of hoodoos is even more outstanding.
Bryce is located high up there, averaging over 8,000 ft (2500 m) in elevation. Even during my visit in mid-April, spring had only begun. Snow was still on the ground and the scenic road was only partially open.
Bryce Canyon isn’t even a canyon. Canyons are formed by water, flowing through a stream or river, eroding the rock. Bryce was formed by erosion and is almost open on one side. Nevertheless, the original name stuck.
Let’s start with the most famous of part of the park, the Amphitheater.
I hiked in this area the next day. The Queen’s Garden Trail is the easiest trail that goes into the canyon. (And one of few that was actually open at the time.) It was really cool going down and hiking among the hoodoos.
After seeing the Amphitheater and driving what was open of the scenic drive on my first day at Bryce, I headed to the Mossy Cove Trail. This trail is located outside of the main area of the park, along Highway 12. It is much lower in elevation (so much easier to hike) and somehow the sun came out right on time.
Bryce Canyon National Park is an excellent place to escape to nature. However, it gets busier and busier every year and often gets snowed in the winter, so plan accordingly. Check the weather and park updates and arrive before 9 to get a coveted parking spot inside of the park. Mid-morning to late afternoon, park in town and take the bus. There won’t be much parking at all in the summer. I only snagged one because I have a tiny car (and that was in April).
Check out my next update where I explore some history and pre-history along US-89.