Dan Suzio Photography

  • Home
  • Photo Catalog
    • All Galleries
    • Search
    • Cart
    • Lightbox
    • Client Area
  • About
  • Contact
  • Facebook
  • Twitter
x

Search Results

Refine Search
Match all words
Match any word
Prints
Personal Use
Royalty-Free
Rights-Managed
(leave unchecked to
search all images)
Next
156 images found
twitterlinkedinfacebook

Loading ()...

  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101556-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101514-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101536-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101535-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101527-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101515-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101503-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101495-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101491-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101558-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores. Sloan Canyon National Conservation Area, Nevada
    07101486-collared-lizard.jpg
  • Great Basin collared lizard, Crotaphytus bicinctores, stalking butterfly. Sloan Canyon National Conservation Area, Nevada
    07101513-collared-lizard.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100227-whiptail-lizard.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100283-whiptail-lizard.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100240-whiptail-lizard.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100236-whiptail-lizard.jpg
  • Great Basin gopher snake, Pituophis catenifer deserticola, crossing Titus Canyon Road in Death Valley National Park, California
    08092091-gopher-snake.jpg
  • Great Basin gopher snake, Pituophis catenifer deserticola, crossing Titus Canyon Road in Death Valley National Park, California
    08092090-gopher-snake.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100231-whiptail-lizard.jpg
  • Great Basin whiptail, Cnemidophorus tigris tigris.  Wildrose Canyon, Death Valley National Park, California
    07100229-whiptail-lizard.jpg
  • Great Basin gopher snake, Pituophis catenifer deserticola, crossing Titus Canyon Road in Death Valley National Park, California
    08092092-gopher-snake.jpg
  • This Great Basin whiptail, Cnemidophorus tigris tigris, was killed and partially swallowed by a juvenile California king snake, Lampropeltis getula californiae. The lizard was too big to swallow and the snake eventually abandoned it. Desert Tortoise Natural Area, Mojave Desert, California.
    11040826.jpg
  • This Great Basin whiptail, Cnemidophorus tigris tigris, was killed and partially swallowed by a juvenile California king snake, Lampropeltis getula californiae. The lizard was too big to swallow and the snake eventually abandoned it. Desert Tortoise Natural Area, Mojave Desert, California.
    11040828.jpg
  • This Great Basin whiptail, Cnemidophorus tigris tigris, was killed and partially swallowed by a juvenile California king snake, Lampropeltis getula californiae. The lizard was too big to swallow and the snake eventually abandoned it. Desert Tortoise Natural Area, Mojave Desert, California.
    11040827.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
  • 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.
    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.
    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.
    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.
    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
  • 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.
    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.
    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.
    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.
    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.
    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.
    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.
    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
  • 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
  • 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.
    11140148-mono-lake.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101377-petroglyph.jpg
  • Burned branch of Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101292-joshua-tree.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101275-desert-scrub-oak.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101272-desert-scrub-oak.jpg
  • A strong wind blows the leaves from a quaking aspen, Populus tremuloides, in autumn. Hart Mountain National Antelope Refuge, in the high desert of eastern Oregon.
    09120203-quaking-aspen.jpg
  • Mojave yucca, Yucca schidigera. Sloan Canyon National Conservation Area, Nevada
    07101580-mojave-yucca.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101450-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101443-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101434-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101424-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101420-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101418-petroglyph.jpg
  • Burned Joshua trees, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101308-joshua-tree.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101168-joshua-tree.jpg
  • Pronghorn (American antelope), Antilocapra americana, at Hart Mountain National Antelope Refuge, Oregon
    09120043-pronghorn.jpg
  • Pronghorn (American antelope), Antilocapra americana, at Hart Mountain National Antelope Refuge, Oregon
    09120032-pronghorn.jpg
  • Pronghorn (American antelope), Antilocapra americana, at Hart Mountain National Antelope Refuge, Oregon
    09120024-pronghorn.jpg
  • Pronghorn (American antelope), Antilocapra americana, at Hart Mountain National Antelope Refuge, Oregon
    09120022-pronghorn.jpg
  • Pronghorn (American antelope), Antilocapra americana, at Hart Mountain National Antelope Refuge, Oregon
    09120017-pronghorn.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101577-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101574-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101456-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101454-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101447-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101431-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101416-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101412-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101411-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101403-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101400-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101396-petroglyph.jpg
  • Petroglyphs, Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada. This area contains one of the greatest concentrations of Native American rock art in the United States, with more than 1,700 petroglyphs made over a period of about 2,000 years.
    07101380-petroglyph.jpg
  • Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada
    07101372-sloan-canyon.jpg
  • Weathered rock, Sloan Canyon National Conservation Area, Nevada
    07101367-rock-pattern.jpg
  • Encelia, Sloan Canyon National Conservation Area, Nevada
    07101365-encelia.jpg
  • Petroglyph Canyon, Sloan Canyon National Conservation Area, Nevada
    07101342-sloan-canyon.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101334-joshua-tree.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101331-joshua-tree.jpg
  • Burned Joshua trees, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101296-joshua-tree.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101289-desert-scrub-oak.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101278-desert-scrub-oak.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101276-desert-scrub-oak.jpg
  • Burned desert scrub oak, Quercus turbinella. Red Rock Canyon National Conservation Area, Nevada
    07101269-desert-scrub-oak.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101260-joshua-tree.jpg
  • Burned Joshua trees, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101244-joshua-tree.jpg
  • Burned Joshua trees, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101239-joshua-tree.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101160-joshua-tree.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101154-joshua-tree.jpg
  • Burned Joshua tree, Yucca brevifolia. Red Rock Canyon National Conservation Area, Nevada
    07101136-joshua-tree.jpg
Next