Dan Suzio Photography

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  • Pacific madrone, Arbutus menziesii. Mendocino County, California
    12100170.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.
    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.
    11140155-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
  • Moonlit ruins of the school building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140699-rhyolite.jpg
  • Moonlit ruins of the Porter Brothers Store building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140695-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140692-rhyolite.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.
    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.
    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
  • 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.
    11140143-mono-lake.jpg
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140698-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140688-rhyolite.jpg
  • Stars over the Panamint Mountains, Death Valley National Park, California
    08070211-death-valley.jpg
  • Clouds over the eastern face of the Sierra Nevada, near Lone Pine, California
    11040442.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.
    11140149-mono-lake.jpg
  • Moonlit ruins of the school building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140700-rhyolite.jpg
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140696-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140693-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140690-rhyolite.jpg
  • Great blue heron, Ardea herodias, flying in fog on the Tarcoles River, Costa Rica
    09061094.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.
    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.
    11140153-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
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140697-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140694-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140687-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140686-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140684-rhyolite.jpg
  • Northern Shovelers, Anas clypeata, at sunset in Sacramento National Wildlife Refuge, California
    19050067.jpg
  • California giant salamander, Dicamptodon ensatus. Armstrong Redwoods State Park, Sonoma County, California.
    a68.jpg
  • Nest of dark-eyed junco, Junco hyemalis, Point Reyes National Seashore, California
    07150040-junco-nest.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130122.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130118.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130117.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130115.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130110.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130107.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130106.jpg
  • Dark-backed Wood-Quail, Odontophorus melanonotus, Refugio Paz de las Aves, Ecuador
    15130116.jpg
  • Nest of dark-eyed junco, Junco hyemalis, Point Reyes National Seashore, California
    07150038-junco-nest.jpg
  • Tropical Kingbird, Tyrannus melancholicus, perched in a tree after dark at Monteverde, Costa Rica
    17050442.jpg