The rain in the forecast I mentioned in my last post came, but it came much later than originally predicted. It was cloudy all day Tuesday but the rain held off until sundown. It rained off and on during the night and continued to rain Wednesday with a few breaks. Thursday we had showers but the sun broke through occasionally. The nice thing about the rain, it cleared the air of whatever pollen was getting to me.
Thursday afternoon during a period of sunshine, we drove to the store. On the way into town, Donna suggested making the 18-mile drive up to Panguitch Lake to have a look around. It turned out to be not such a good day for it. As we climbed to the lake west of town, we drove right back into rain. We didn’t even get out of the truck – we just drove by the lake and took a look. There isn’t much up there and it was too dreary to snap a photo.
Friday morning we had clear skies and the sun was shining. We had a late breakfast, then drove up to Red Canyon in the Dixie National Forest. Red Canyon has a visitor center with a large parking lot providing access to many hiking trails – it’s the gateway to Bryce Canyon National Park with a 17-mile paved biking trail to the park.
After a stop in the visitor center for information and maps, we decided to hike from there. We followed a trail from the visitor center parallel to the highway and started up the Hoodoo Trail. Geologically speaking, a hoodoo is a column of rock, usually softer rock like limestone topped by a harder layer – typically basalt. Hoodoos differ from spires due to their shape – they are irregular, forming a totem pole-like shape or are topped with an area with a larger diameter often looking like a rock balanced on top of a spire. A spire is a column of rock that tapers from a larger diameter base to a thin tip.
Hoodoo Trail is aptly named as it offers views of two distintive hoodoos.
Like arches, hoodoos form from erosion over millions of years.
The Hoodoo Trail fishooks as it climbs and has nine posts, each one numbered with a guide pamphlet giving information about vegetation and geology of the area around the posts. After the ninth post, we reached the junction with the Pink Ledges Trail. This trail climbs and had four more numbered posts (10 through 13) described in the guide. A few of the posts also have benches where you can take a break and look at the scenery.
In the photo above, the high cliff in the background clearly shows the sedimentary layers of rock – softer limestone and sandstone topped with darker basalt.
It was amazing to see trees rooted in the rock formations.
The orange and yellows in picture above are from clay and iron mixed in the limestone. It’s hard to see in the photo, but the darker areas appeared to be a type of lichen adhering to the rock.
The Pink Ledges Trail eventually brought us back to the far end of the visitor center parking lot. The trail wasn’t too strenuous, although it did have significant elevation changes and few steep areas with loose stones. Wear sturdy shoes and tread carefully!
Late in the afternoon on Wednesday, Donna took advantage of a break in the rain to grill chicken breasts. She grilled the chicken seasoned with salt and pepper, then served it topped with a Mediterranean vinaigrette. She roasted patty pan squash (picked up from the local produce stand) with tomatoes and black olives, topped with fresh basil.
This morning, Donna loaded her bike in the truck and returned to Red Canyon. She rode up the trail toward Bryce Canyon to the summit and beyond, gaining nearly 1,000 feet of elevation before turning back after seven-and-a-half miles to make a quick descent back to the truck.
With the rainy day Wednesday, we had a high of only 64 degrees. Thursday was warmer and Friday hit the upper 70s with a high of 78 called for today. We should see highs in the low to mid 80s in the next few days. I paid for three more nights here to get us through the Labor Day weekend. We’ll head out on Tuesday and intend to be back in Mesa, Arizona on Thursday September 9th.
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