Leighton Photography & Imaging

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  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • One of the best things about the Pacific Northwest on the eastern side of the Cascade Mountains is the big, open sky and hundreds of miles of sagebrush in all directions.
    Sagebrush Country and the Big Sky
  • The Chisos Mountains of West Texas is the southernmost mountain range in the United States, and is surrounded by the Chihuahuan Desert on the US-Mexico border. Located wholly within the borders of Big Bend National Park, this incredible view of this ancient volcanic mountain range was photographed on a late spring afternoon as the sun began to set in the "golden hour".
    Chisos Mountains of West Texas
  • One of the many great rock formations in the Chisos 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.
    Mules Ears
  • 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. <br />
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
  • El Capitan in West Texas' Guadalupe Mountains (100 miles east of El Paso) is the world's premier example of an exposed fossil reef from the Permian Era, dated at about 260 million years old - much older than the golden age of dinosaurs. This whole part of Texas back in this time was once covered in a shallow sea that geologists call the Delaware Sea, in a time when all of Earth's continents were still joined into one supercontinent that we call Pangaea. The entire top of El Capitan is made of limestone formed from the fossilized remains of aquatic plant and animal remains such as corals, algae, shellfish and plankton, and now stands at just above 8000 feet above sea level. The base is formed by layer upon layer of sand laid down over millions of years, in the manner you would expect from the ocean floor resulting in a very typical sedimentary rock formation,  further eroded by millions of years of desert heat, rain, abrasion and wind.
    El Capitan, West Texas
  • Standing at 7,325 ft, Casa Grande (Spanish for "Big House") is the fourth highest peak in Texas' Chisos Mountains and is found in the heart of Big Bend National Park.
    Casa Grande in the High Chisos Mountains
  • Saguaro cacti stand tall as sunset fades in the Puerto Blanco Mountains in Organ Pipe Cactus National Monument along the US-Mexico border in Arizona. Truly one of my favorite places in the Sonoran Desert.
    Sunset in the Puerto Blanco Mountains
  • Once an ancient Permian ocean reef, these hills and cliffs that are part of the Guadalupe Mountains in Northwestern Texas near Salt Flat are an example of one the world's very best and oldest fossilized coral reefs. Now part of the Chihuahuan Desert the area is teeming with sea life fossils.
    McKittrick Canyon in the Guadalupe M..ains
  • Some of the amazingly beautiful rock formations photographed here at dusk in Arches National Park in Eastern Utah.
    Moab Rock Formations
  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • The famous Delicate Arch stands 65 feet (20 meters) above its sandstone base in the surrounding canyons and ravines in Arches National Park in eastern Utah's Moab Desert.
    Delicate Arch
  • Ancient basalt columns are a typical sight in Central Washington. They are formed by cooling lava, forming cracks that create these columns by contracting. The faster the lava cools, the thinner the columns. These thick columns cooled gradually over some time. The presence of the lichens that now cover the stony face is an indicator of very good air quality and a lack of pollution.
    Lichen-Covered Basalt Cliff in Cowic..nyon
  • Sunset is almost always a dramatic show of light and shadow, as witnessed here in Cowiche Canyon, just west of Yakima, WA. Strong beams of sunlight beautifully backlit these desert wildflowers (Carey's balsamroot).
    Sunset in the Sagebrush Desert
  • This rock was once molten lava forced from deep within the earth as it covered most of Central Washington, up to three miles deep in some places. Many thousands of years of erosion, weathering and exposure to the elements has left us with massive crumbling rock formations like this basalt rock wall.
    Rocky Basalt Bluffs of Cowiche Canyon
  • Rolling arid hills and miles upon miles of aromatic sagebrush, crumbled basalt rocks and heat in this desert-like landscape in Central Washington near Vantage, WA.
    Sagebrush Country
  • 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. <br />
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
  • 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. <br />
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
  • 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. <br />
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
  • Golden hour near the Ajo Mountains in the Sonoran Desert! Big skies, lowlands filled with saguaro and organ pipe cacti, and loads of wildlife and incredible wildflowers - springtime in Arizona is about as beautiful as nature gets!
    Ajo Mountains
  • The eastern part of the Cascades mountains in Washington state couldn't be more different from the western side. Instead of wet, green and cloudy slopes, there are dry, columnar igneous rock structures, desert scrub plants and big skies!
    Basalt Cliffs at White Pass