An ocean of rolling sandstone slickrock...

is to be enjoyed on the famous Slickrock Trail. Don’t let the seemingly flat expanse in the image below deceive you but I cranked slightly more than 2,000 feet (610 m) of vertical ascent on the 10 mile (~16 km) trail. I first rode this line in the early 1980s on the upswing of mountain biking and it hasn’t gotten any easier at three score and nine years in age.

GPS track from my Garmin watch, color reflects speed.

Castle Valley Drive has finally reopened...

above the newly constructed monstrous arch culvert near the entrance to the community. It is astonishing that the natural streambed was not carried through the oversized rip-rap that is placed directly in the channel, choking it, rather than simply protecting the side slopes.

The natural cobble bed channel of Castle Creek versus the newly engineered channel choked with rip-rap.

The cherry on top...

of my typical daily 18 mile (29 km) ride is the long and flowy descent on the singletrack from this high point on the trail, about 900 feet (274 m) above my residence in the lower valley. It’s all about the downhill flow!

Finally nearing completion...

with the road grade reestablished atop the new arch culvert on Castle Creek. Road paving and placement of rip-rap still remain as tasks to be completed before the main entrance to our community reopens to traffic.

It will be interesting to observe the backwater effects of the new structure and the rough, bouldery channel created by use of oversized rip-rap during future flood events. Upstream pooling of water, slower, less efficient passage of flood flow, increased deposition of fine sediments in the channel and increased bank erosion upstream are likely going to occur.