Dan Suzio Photography

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  • Folded rock strata, Wildrose Canyon, Death Valley National Park, California
    07100444-death-valley-geology.jpg
  • Folded rock strata, Wildrose Canyon, Death Valley National Park, California
    07100453-death-valley-geology.jpg
  • Folded rock strata, Wildrose Canyon, Death Valley National Park, California
    07100452-death-valley-geology.jpg
  • Folded rock strata, Wildrose Canyon, Death Valley National Park, California
    07100445-death-valley-geology.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140179-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140161-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140155-mono-lake.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140388-mosaic-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140216-golden-canyon-death-valley.jpg
  • Sun and clouds over the Devil's Golf Course, an area of wind- and rain-sculpted salt and mud  in Death Valley National Park, California.
    10140113-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070195-death-valley.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140170-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140169-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140168-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140158-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140156-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140154-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140149-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140145-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140144-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140143-mono-lake.jpg
  • Golden Canyon, Death Valley National Park, California
    10140212-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140198v-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140198-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140194-golden-canyon-death-valley.jpg
  • Red Cathedral, a natural amphitheater at the head of Golden Canyon, Death Valley National Park, California
    10140190-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140179-golden-canyon-death-valley.jpg
  • Natural Bridge, Death Valley National Park, California
    10140140-natural-bridge-death-valley.jpg
  • Salt and mud are shaped by wind and rain at the Devil's Golf Course, Death Valley National Park, California.
    10140116-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070200-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070202-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070204-death-valley.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140174-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140167-mono-lake.jpg
  • Tufa towers at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140166-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140162-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140160-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140152-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140146-mono-lake.jpg
  • Polished marble in the narrows of Mosaic Canyon, Death Valley National Park, California
    10140395-mosaic-canyon-death-valley.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140392-mosaic-canyon-death-valley.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140391-mosaic-canyon-death-valley.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140383-mosaic-canyon-death-valley.jpg
  • Breccia in Mosaic Canyon, Death Valley National Park, California
    10140378-mosaic-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140208-golden-canyon-death-valley.jpg
  • Manly Beacon, viewed from Golden Canyon, Death Valley National Park, California
    10140204-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140202-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140196v-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140195v1-golden-canyon-death-valle...jpg
  • Golden Canyon, Death Valley National Park, California
    10140191-golden-canyon-death-valley.jpg
  • Red Cathedral, a natural amphitheater at the head of Golden Canyon, Death Valley National Park, California
    10140190v-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140185-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140180-golden-canyon-death-valley.jpg
  • A cloudy sky mutes the colors of the rock at Artist's Palette, Death Valley National Park, California
    10140150-artists-palette-death-valle...jpg
  • Dry falls in Natural Bridge Canyon, Death Valley National Park, California
    10140145-death-valley.jpg
  • Natural Bridge, Death Valley National Park, California
    10140144-natural-bridge-death-valley.jpg
  • Salt and mud are shaped into an arch by wind and rain at the Devil's Golf Course, Death Valley National Park, California.
    10140124-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070188-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070189-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070197-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070203-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070206-death-valley.jpg
  • Red Rock Canyon State Park, California
    06112142.jpg
  • Patterns in rock, Organ Pipe Cactus National Monument, Arizona.
    06110586.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140164-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140157-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140153-mono-lake.jpg
  • Moon over cliffs, Red Rock Canyon National Conservation Area, Nevada
    07101267-moon.jpg
  • Moon over cliffs, Red Rock Canyon National Conservation Area, Nevada
    07101176.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140386-mosaic-canyon-death-valley.jpg
  • Mosaic Canyon, Death Valley National Park, California
    10140385-mosaic-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140215-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140213-golden-canyon-death-valley.jpg
  • Manly Beacon, viewed from Golden Canyon, Death Valley National Park, California
    10140206-golden-canyon-death-valley.jpg
  • Manly Beacon, viewed from Golden Canyon, Death Valley National Park, California
    10140205-golden-canyon-death-valley.jpg
  • Manly Beacon, viewed from Golden Canyon, Death Valley National Park, California
    10140203-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140200-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140192-golden-canyon-death-valley.jpg
  • Salt and mud are shaped into an arch by wind and rain at the Devil's Golf Course, Death Valley National Park, California.
    10140122-death-valley.jpg
  • Salt and mud are shaped by wind and rain at the Devil's Golf Course, Death Valley National Park, California.
    10140114-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070187-death-valley.jpg
  • Students and faculty from San Jose State University, in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070194-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070198-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070199-death-valley.jpg
  • Desert varnish on rocks in the Greenwater Range on the eastern edge of Death Valley National Park, California
    08070207-death-valley.jpg
  • Dead grebe, Podiceps sp, on the shore of Mono Lake. South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140176-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140165-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140148-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140147-mono-lake.jpg
  • Moon over Golden Canyon, Death Valley National Park, California
    10140210-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140196-golden-canyon-death-valley.jpg
  • Golden Canyon, Death Valley National Park, California
    10140195v2-golden-canyon-death-valle...jpg
  • Golden Canyon, Death Valley National Park, California
    10140195-golden-canyon-death-valley.jpg
  • Natural Bridge Canyon, Death Valley National Park, California
    10140146-death-valley.jpg
  • Salt and mud are shaped by wind and rain at the Devil's Golf Course, Death Valley National Park, California.
    10140137-death-valley.jpg
  • Clouds over the Devil's Golf Course, an area of wind- and rain-sculpted salt and mud  in Death Valley National Park, California.
    10140127-death-valley.jpg
  • Clouds over the Devil's Golf Course, an area of wind- and rain-sculpted salt and mud  in Death Valley National Park, California.
    10140126-death-valley.jpg
  • Sun and clouds over the Devil's Golf Course, an area of wind- and rain-sculpted salt and mud  in Death Valley National Park, California.
    10140125-death-valley.jpg