A short, pleasant woodland walk east of the nature center brings you to these springs. This you can do here. Waters from Buffalo and Antelope Springs eventually end up in the Washita River on their way to the oceans. Bromide Hill is a popular place at Chickasaw. Winding your way along the well-developed foot trail on this northern face you traverse sedimentary rock deposits which are 270 million years old .
Some layers look like the usual sandstones and shales .
Other layers suggest that a concrete truck dumped its payload there. But looking around at the mass of this concrete-like, naturally cemented gravel, sand, and cobble quickly changes your mind. No truck could do it. This conglomerate , as it is called, caps the whole of Bromide Hill. But the view at the top caps your climb.