El Caballo Blanco trace back to Bodeguero and those first mares. El Caballo Resort was established in 1974 at Wooroloo and their dancing horses were a popular tourist attraction. Williams established the El Caballo Blanco theme park at Catherine Field near the Sydney suburb of Narellan. Its main attraction was its Andalusian dancing stallions, but the park also featured miniature Fallabella horses, and a number of non-equestrian related amusements such as water slides, train rides, and a small wildlife zoo. Williams then went on to establish an El Caballo Blanco park at Disneyland in the US. After Williams' death in the US, the
Caballo Mountains Nakaye Formation of limestone, the Bar B Formation of interbedded limestone, dolomite, shale, and conglomerate, and the red shale beds of the Abo Formation. All of those strata are Pennsylvanian in age. Above them is thePermian Yeso Formation, which consists of sandstones, siltstone-dolomites, and limestones. The Paleozoic strata are completed by the Meseta Blanca Sandstone. Most of the Mesozoic rocks are missing from the Caballo geological history. A second unconformity lies above the Meseta Blanca Sandstone, and includes all of the Triassic and Jurassic periods. The next oldest rocks are of Cretaceous age and include: The Mesozoic rocks terminate below