One of the defining features of our land is the 2-3 tiered mesas that bisect the lot. The lower tier is still collapsing and leaves hanging sandstone ledges that can extend several feet while only being 2″ thick. The second interesting feature we found were gypsum crystal seams that criss cross through the entire property. There are multiple sites where the surrounding ground has eroded leaving large areas covered with large exposed crystals. All of this land was submerged and was part of the Western Interior Seaway during the Cretaceous period(100-66 million years ago). We see proof of this from the mosasaur bones, ammonites, and giant clam fossils found throughout the property.