| 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. |
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