The start of the Kolob Canyon |
The red in the rocks comes from Ferric Oxide. |
The trail and the creek interweaved for the entire length of the walk. We must have crossed it some 50-60 times. It was quite a gentle flow and very easily negotiated - just slosh across. |
The creek - again. |
The trail went between the walls of Tucupit and Paria Points and, as we went further in, the walls got narrower and our steady ascent got steeper. |
I'm not sure how high these peaks were. We started walking at around 5000ft. The vegetation was manily sage, juniper and pinon trees. |
Looking back down the trail. |
The folds in the rock formations were neverendingly fascinating. Not a bit like Dartmoor granite. |
The distance between the walls of the canyon got narrower and narrower as we reached the top. |
Looking up. |
The creek bed mirrors the surrounding geology, with its multicoloured rocks. Compare and contrast with the shades of grey we'd see in a stream on Dartmoor. |
Just an interesting pattern on an old tree stump. |
I found the colours in the rocks fascinating. |
And this is the waterfall where the walls of the canyon meet at the Double Arch Alcove. |
Another one of nature's interesting patterns. I presume the holes were the result of the activity of some wood boring insect. |
No comments:
Post a Comment