The river here runs on sand rather than clay, and that change is the beginning of something: the highway is entering the belt of deep sandy soils that supports the isolated pine forest a few miles ahead. Sandbars, clear runs and a bottom of loose quartz grains distinguish this reach from the muddy Colorado further down. The sand came from the same source as the pines' foothold — an ancient river delta laid down about 50 million years ago and left as a stripe of loose sediment running across the state.
Getting there
30.0128, -97.1611
Locations are approximate and may be inaccurate, on private land, or otherwise inaccessible. Check before you travel.