I’m fascinated by erosion patterns in rock that make solid rock look like ice cream that has been scooped with a spoon or carved with a giant fork. So, I was transfixed by this “fork action” on the red rock in Sedona.
It’s amazing what Steve can tell us just by examining this photo and knowing its location. He said, “The sandstone has horizontal layers but also has inclined layers internally (25 degrees). The cliff shows these inclined layers because rockfall has sculpted the surface. These inclined layers were formed in underwater sand dunes by flow velocity of 2 meters/second.”
Sedona’s West Fork Trail is described in the guide books as iconic with towering cliffs and 13 stream crossings as you follow Oak Creek for 6.4 miles round trip. The elevation change is moderate (245 ft.), so I considered it doable with camera equipment on my back.
It took us 3.5 hours to reach the end point, as I stopped for photos so often, but the exertion was well worth it. You know you have reached the end when you can’t go further without getting wet, and in November it’s too cold for that!
The cave like erosion you can see along the left side of the creek reminded me of “the subway” in Zion National Park created by the Virgin River. I had to explain myself to my husband after exclaiming, “there is the subway!”
I find myself fascinated by the power of moving water that erodes rock over time. Are you?
If you visit Abiquiu, New Mexico to tour Georgia O’Keeffe’s home, which I highly recommend, you may wish to find the White Place (Plaza Blanca) before you drive back to Santa Fe. You just need to make a 30 minute detour off route US-84 onto a dirt road. You can get a map and directions when you have lunch at the Abiquiu Inn, which I also recommend.
You can’t beat the clear, dry air in New Mexico as well as the wide open spaces. Santa Fe and its environs are a wonderful destination for scenic beauty, art and delicious food.