Cerro Castellan
Cerro Castellan - also known as Castolon Peak or Castellan Peak, is a conical volcanic mountain in West Texas that rises 1000 feet above the desert floor (3,293 feet above sea level) in Big Bend National Park. Cerro Castellan itself is part of an ancient series of summits once known as the Corazones Peaks that has since succumbed to millennia of erosion by wind, precipitation, searing heat and bitterly cold winters. Geologically, this ancient mountain range remnant is a high stack of volcanic rocks, including ash, lava, and tuffaceous rocks. It is capped by a dense lava flow underlain by various tuffs and basalts. A somewhat northwest fault cuts the eastern face of Cerro Castellan. Although little vegetation grows on the sheer cliffs and steep, pointed profile of its peak, the lower slopes of Cerro Castellan support a sparse growth of Chihuahuan Desert scrub, including most prominently such characteristic species as creosote bush and ocotillo.
Cerro Castellan - Different Angle
The Chiricahua Desert of West Texas
Mule Ears
One of the many great rock formations in the Chiso Mountains in Western Texas' Big Bend National Park and is known as the "Mule Ear Peaks." These twin peaks are formed from a part of a dike-like intrusion of relatively young rhyolite, and rise about 1040 feet (3,881 above sea level) above the desert floor.
Cerro Castellan
Cerro Castellan (from below)
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Oh my word!
Never been here. Added to bucketlist.
Thanks Rich! Lovely pics.
Thanks Roman! You absolutely have to go. I highly recommend going in April when all the cacti are in bloom. The whole place looks surreal!