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  • Slow regrowth of vegetation and trees, 29 years after the intense Rainbow Fire of 1992 is shown on a smoky 21st of August in 2021, in Devils Postpile National Monument, Inyo National Forest, near Mammoth Lakes, California, USA. Smoke drifting from the bad Caldor, Dixie, and other fires frequently smarted our eyes during 3 weeks of hiking in the Eastern Sierra in August of 2021. On September 1, most of California's National Forests were unprecedentedly closed due to fire risk for two weeks! Decades of fire exclusion policies, years of below-normal snow and rainfall, a hot summer, and remote upslope location provided fuel and conditions ripe for the 1992 Rainbow Fire, a conflagration sparked by lightning strikes. Scientists warn that human-caused climate change has made the U.S. West warmer and drier in the past 30 years and will continue to make the weather more extreme and wildfires more destructive.
    2108CA1-698.jpg
  • The San Jacinto Mountains rise above the world's largest California Fan Palm oasis, along the Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0936.jpg
  • Visit the world's largest California Fan Palm oasis on the beautiful Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0897.jpg
  • A curious kea bites a car tire. The kea (Nestor notabilis) is the world's only alpine parrot. In 1986, it received full protection under the Wildlife Act. The kea is one of ten endemic parrot species in New Zealand. Kea are known for their intelligence and curiosity, both vital to their survival in a harsh mountain environment. Kea can solve logical puzzles, such as pushing and pulling things in a certain order to get to food, and will work together to achieve a certain objective. They have been filmed preparing and using tools. Photographed at Homer Tunnel, Fiordland National Park, Southland region, South Island of New Zealand. In 1990, UNESCO honored Te Wahipounamu - South West New Zealand as a World Heritage Area.
    1901NZ1-1379.jpg
  • The kea (Nestor notabilis) is the world's only alpine parrot. In 1986, it received full protection under the Wildlife Act. The kea is one of ten endemic parrot species in New Zealand. Kea are known for their intelligence and curiosity, both vital to their survival in a harsh mountain environment. Kea can solve logical puzzles, such as pushing and pulling things in a certain order to get to food, and will work together to achieve a certain objective. They have been filmed preparing and using tools. Photographed at Homer Tunnel, Fiordland National Park, Southland region, South Island of New Zealand. In 1990, UNESCO honored Te Wahipounamu - South West New Zealand as a World Heritage Area.
    1901NZ1-1362.jpg
  • The Princess Parrot is native Central and West Australia but today is rarely seen in the wild. It's also known as a Princess of Wales Parrot, Queen Alexandra parakeet, Spinifex parrot, Rose-Throated Parrot, or Splendor Parrot. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-054.jpg
  • The Blue and Gold Macaw is native to South America and is  in the Psittacidae family of true parrots. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-030.jpg
  • Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-133.jpg
  • The Gouldian Finch (or Lady Gouldian or Rainbow Finch) is native to tropical Northern Australia and has green or blue back; red, black or orange head; and white or lavender breast. The photo is from Bloedel Conservatory, in Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, atop the City of Vancouver’s highest point, Little Mountain (501 feet). In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls.
    1402VAN-100.jpg
  • Palm Canyon seen from Victor Trail. We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looped back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. The beautiful Palm Canyon Trail takes you through the world's largest California Fan Palm oasis. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A1047-1048-Pano.jpg
  • Stone Pools with palms along Indian Potrero Trail. Indian Canyons, Palm Springs, California, USA. We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looped back via Victor Trail, in the Indian Canyons, just west of the city of Palm Springs. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A1018-1027-Pano.jpg
  • A sign lists "No water, no shade, and no cell service" as "hazardous conditions beyond this point." Visit the world's largest California Fan Palm oasis on the beautiful Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0941.jpg
  • Visit the world's largest California Fan Palm oasis on the beautiful Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0934.jpg
  • Visit the world's largest California Fan Palm oasis on the beautiful Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0895.jpg
  • Scenes from hiking the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The beautiful Palm Canyon Trail visits the world's largest California Fan Palm oasis. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0892-893-Pano.jpg
  • The beautiful Palm Canyon Trail visits the world's largest California Fan Palm oasis, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0869-870-Pano.jpg
  • 49 Palms Oasis, palm panorama in Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0535-564-Pano.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0574.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0568.jpg
  • 49 Palms Oasis, vertical panorama, in Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0437-445-Pano.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0493.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0492.jpg
  • A peek-a-boo view of the City of Twentynine Palms from 49 Palms Oasis Trail. Joshua Tree National Park, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0419.jpg
  • The kea (Nestor notabilis) is the world's only alpine parrot. In 1986, it received full protection under the Wildlife Act. The kea is one of ten endemic parrot species in New Zealand. Kea are known for their intelligence and curiosity, both vital to their survival in a harsh mountain environment. Kea can solve logical puzzles, such as pushing and pulling things in a certain order to get to food, and will work together to achieve a certain objective. They have been filmed preparing and using tools. Photographed at Homer Tunnel, Fiordland National Park, Southland region, South Island of New Zealand. In 1990, UNESCO honored Te Wahipounamu - South West New Zealand as a World Heritage Area.
    1901NZ1-1380.jpg
  • The kea (Nestor notabilis) is the world's only alpine parrot. In 1986, it received full protection under the Wildlife Act. The kea is one of ten endemic parrot species in New Zealand. Kea are known for their intelligence and curiosity, both vital to their survival in a harsh mountain environment. Kea can solve logical puzzles, such as pushing and pulling things in a certain order to get to food, and will work together to achieve a certain objective. They have been filmed preparing and using tools. Photographed at Homer Tunnel, Fiordland National Park, Southland region, South Island of New Zealand. In 1990, UNESCO honored Te Wahipounamu - South West New Zealand as a World Heritage Area.
    1901NZ1-1375.jpg
  • Historic late-1800s log cabin. Independence has been a ghost town since about 1899, when trains came into Aspen and the gold played out. Supposedly founded on Independence Day July 4, 1879 when gold was discovered, Independence was the first community in the Roaring Fork River Valley, a tributary of the Colorado River. Independence lies in a harsh environment at 10,830 feet elevation, 13.5 miles east of Aspen on Highway 82, and four miles west of Independence Pass on the Continental Divide, in Pitkin County, Colorado, USA. The remaining buildings are on land near the river owned by the Loughren Trust, and the upper site is in White River National Forest. In its short life, few could agree on a name for Independence, which was also known as Farwell, Chipeta City, Sparkill, Mammoth Mountain, Mount Hope, and Hunter's Pass. This image was stitched from multiple overlapping photos.
    1709US1-0696-p1-Pano_Independence_CO.jpg
  • Historic late-1800s log cabin. Independence has been a ghost town since about 1899, when trains came into Aspen and the gold played out. Supposedly founded on Independence Day July 4, 1879 when gold was discovered, Independence was the first community in the Roaring Fork River Valley, a tributary of the Colorado River. Independence lies in a harsh environment at 10,830 feet elevation, 13.5 miles east of Aspen on Highway 82, and four miles west of Independence Pass on the Continental Divide, in Pitkin County, Colorado, USA. The remaining buildings are on land near the river owned by the Loughren Trust, and the upper site is in White River National Forest. In its short life, few could agree on a name for Independence, which was also known as Farwell, Chipeta City, Sparkill, Mammoth Mountain, Mount Hope, and Hunter's Pass. This image was stitched from multiple overlapping photos.
    1709US1-0665-71-Pano_Independence_CO.jpg
  • The Princess Parrot is native Central and West Australia but today is rarely seen in the wild. It's also known as a Princess of Wales Parrot, Queen Alexandra parakeet, Spinifex parrot, Rose-Throated Parrot, or Splendor Parrot. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-065.jpg
  • The Blue and Gold Macaw is native to South America and is  in the Psittacidae family of true parrots. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-044.jpg
  • The Blue and Gold Macaw is native to South America and is  in the Psittacidae family of true parrots. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-036.jpg
  • The Pied Imperial Pigeon (or Arboreal Dove; or Nutmeg, Torresian Imperial, or Torres Strait Pigeon; Ducula bicolor) is found in forest, woodland, mangrove, plantations and scrub in Southeast Asia, ranging from Myanmar and Thailand south to Java and east to the Philippines and the Bird's Head Peninsula in New Guinea. Photographed in Bloedel Conservatory, Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point, Little Mountain (501 feet). In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls.
    1402VAN-136.jpg
  • The Lineolated Parakeet (or Linnie, Barred, or Catherine Parakeet, Bolborhynchus lineola) is native to highland forests of southern Mexico to Peru and Venezuela. The bird is green with black bars on the wings, plus many color mutations from breeding. Photographed in Bloedel Conservatory, Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-128.jpg
  • A green parrot. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-106.jpg
  • Orange-yellow bird. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-110.jpg
  • Scenes from hiking the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The beautiful Palm Canyon Trail visits the world's largest California Fan Palm oasis. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0926-927-Pano.jpg
  • Visit the world's largest California Fan Palm oasis on the beautiful Palm Canyon Trail, a great "tour de fronds." We hiked the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0904.jpg
  • The "tour de fronds." A traditional Indian thatched dwelling is dwarfed by tall trees along the Palm Canyon Trail in the Indian Canyons, Palm Springs, California, USA. The beautiful Palm Canyon Trail visits the world's largest California Fan Palm oasis. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. California fan palms (Washingtonia filifera in the palm family Arecaceae) are native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves. Multiple overlapping photos were stitched to make this panorama.
    2103SW-A0884-889-Pano.jpg
  • Traditional Indian thatched dwelling, on the Reservation of the Agua Caliente Band of Cahuilla Indians. Scenes from hiking the Palm Canyon Trail to Indian Potrero Trail to Stone Pools, and looping back via Victor Trail, in the Indian Canyons, Palm Springs, California, USA. The beautiful Palm Canyon Trail takes you through the world's largest California Fan Palm oasis. The Indian Canyons are the ancestral home of the Agua Caliente Band of Cahuilla Indians. The California fan palm (Washingtonia filifera in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0883.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0515.jpg
  • 49 Palms Oasis Trail. Joshua Tree National Park, near the City of Twentynine Palms, California, USA. The park straddles the cactus-dotted Colorado Desert and the Mojave Desert, which is higher and cooler. The California fan palm (Washingtonia filifera, in the palm family Arecaceae) is native to the far southwestern United States and Baja California. Today's oasis environment was protected from a drying climate, restricting this cold-tolerant palm to widely separated relict groves.
    2103SW-A0411.jpg
  • The kea (Nestor notabilis) is the world's only alpine parrot. In 1986, it received full protection under the Wildlife Act. The kea is one of ten endemic parrot species in New Zealand. Kea are known for their intelligence and curiosity, both vital to their survival in a harsh mountain environment. Kea can solve logical puzzles, such as pushing and pulling things in a certain order to get to food, and will work together to achieve a certain objective. They have been filmed preparing and using tools. Photographed at Homer Tunnel, Fiordland National Park, Southland region, South Island of New Zealand. In 1990, UNESCO honored Te Wahipounamu - South West New Zealand as a World Heritage Area.
    1901NZ1-1364.jpg
  • Historic late-1800s log cabin. Independence has been a ghost town since about 1899, when trains came into Aspen and the gold played out. Supposedly founded on Independence Day July 4, 1879 when gold was discovered, Independence was the first community in the Roaring Fork River Valley, a tributary of the Colorado River. Independence lies in a harsh environment at 10,830 feet elevation, 13.5 miles east of Aspen on Highway 82, and four miles west of Independence Pass on the Continental Divide, in Pitkin County, Colorado, USA. The remaining buildings are on land near the river owned by the Loughren Trust, and the upper site is in White River National Forest. In its short life, few could agree on a name for Independence, which was also known as Farwell, Chipeta City, Sparkill, Mammoth Mountain, Mount Hope, and Hunter's Pass.
    1709US1-0684_Independence_CO.jpg
  • Historic late-1800s log cabin. Independence has been a ghost town since about 1899, when trains came into Aspen and the gold played out. Supposedly founded on Independence Day July 4, 1879 when gold was discovered, Independence was the first community in the Roaring Fork River Valley, a tributary of the Colorado River. Independence lies in a harsh environment at 10,830 feet elevation, 13.5 miles east of Aspen on Highway 82, and four miles west of Independence Pass on the Continental Divide, in Pitkin County, Colorado, USA. The remaining buildings are on land near the river owned by the Loughren Trust, and the upper site is in White River National Forest. In its short life, few could agree on a name for Independence, which was also known as Farwell, Chipeta City, Sparkill, Mammoth Mountain, Mount Hope, and Hunter's Pass. This image was stitched from multiple overlapping photos.
    1709US1-0679-80-Pano_Independence_CO.jpg
  • The Yellow Headed Amazon Parrot is native to the Amazon Basin, Northern Brazil, and the Eastern Andes. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-073.jpg
  • The Blue and Gold Macaw is native to South America and is  in the Psittacidae family of true parrots. Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-028.jpg
  • The Eclectus Parrot (or Grand Eclectus or King Parrot, Eclectus roratus, a male shown here) is native to the Solomon Islands, Sumba, New Guinea and nearby islands, northeastern Australia and the Maluku Islands (Moluccas). Unusual in the parrot family, it has extreme sexual dimorphism of plumage colors, with the male mostly bright emerald green and the female mostly bright red and purple/blue plumage. Photographed in Bloedel Conservatory, Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point, Little Mountain (501 feet). In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls.
    1402VAN-139.jpg
  • Bloedel Conservatory, Queen Elizabeth Park, Vancouver, British Columbia, Canada. Address: 4600 Cambie St. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-105.jpg
  • The Gouldian Finch (or Lady Gouldian or Rainbow Finch) is native to tropical Northern Australia and has green or blue back; red, black or orange head; and white or lavender breast. The photo is from Bloedel Conservatory, in Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, atop the City of Vancouver’s highest point, Little Mountain (501 feet). In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls.
    1402VAN-085.jpg
  • The Owl Finch (or Bicheno or Double-barred Finch, Taeniopygia bichenovii) is native to northern and eastern Australia. Bloedel Conservatory, Queen Elizabeth Park, 4600 Cambie St, Vancouver, British Columbia, Canada. Bloedel Conservatory is a domed lush paradise where you can experience the colors and scents of the tropics year-round, within Queen Elizabeth Park, atop the City of Vancouver’s highest point. From Little Mountain (501 feet), see panoramic views over the city crowned by the mountains of the North Shore. A former rock quarry has been converted into beautiful Queen Elizabeth Park with flower gardens, public art, grassy knolls. In Bloedel Conservatory, more than 200 free-flying exotic birds, 500 exotic plants and flowers thrive within a temperature-controlled environment. A donation from Prentice Bloedel built the domed structure, which was dedicated in 1969 "to a better appreciation and understanding of the world of plants," and is jointly operated by Vancouver Park Board and VanDusen Botanical Garden Association.
    1402VAN-081.jpg
  • Walk the trail behind Lower Emerald Pool waterfall in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 5 overlapping photos.
    1303UT-1236-1240pan_Lower-Emerald-Fa...jpg
  • Spring snow coats red sandstone and melts into a waterfall along West Rim Spring and the West Rim Trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2112-13pan_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2277_Zion-NP-Utah.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1186.jpg
  • Hikers walk a dog along a rock face near Northgate Peaks trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1053.jpg
  • The sandstone cliffs of the Court of the Patriarchs tower over the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2007-12pan_Zion-NP-Utah.jpg
  • Cliff near Upper Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1215.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1209.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1118.jpg
  • Hikers ascend impressive switchbacks of the West Rim Trail on the way to Angels Landing and Scout Lookout. Zion National Park adjoins Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2220_Zion-NP-Utah.jpg
  • Spring snow coats red sandstone and melts on the West Rim Trail on the way to Angels Landing and Scout Lookout, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2167_Zion-NP-Utah.jpg
  • Snow coats a tree in a mossy canyon in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2055_Zion-NP-Utah.jpg
  • Snow coats a tree in a mossy canyon in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2052_Zion-NP-Utah.jpg
  • Morning sun backlights a cottonwood tree in Zion National Park, which adjoins Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2022_Zion-NP-Utah.jpg
  • The sandstone cliffs of the Court of the Patriarchs tower over the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2001-06pan_Zion-NP-Utah.jpg
  • View from Kolob Terrace Road towards peaks of Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1057.jpg
  • A hiker rests at the end of Northgate Peaks trail, in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 5 overlapping photos.
    1303UT-1031-35pan_Zion_Northgate-Pea...jpg
  • Upper Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 7 overlapping photos.
    1303UT-1220-1226PAN_Upper-Emerald-Po...jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1212.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1205.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1196.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1195.jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1191.jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 10 overlapping photos.
    1303UT-1139-1148pan_Zion-NP_Kolob-Te...jpg
  • Ice on branches, Lower Emerald Pool waterfall, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1184.jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. The panorama was stitched from 8 overlapping photos.
    1303UT-1122-1129pan_Zion-NP_Kolob-Te...jpg
  • Kolob Terrace Road entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1134-p1.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1105.jpg
  • Deer cross Kolob Terrace Road at entrance to Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UT-1103.jpg
  • Patterns of desert varnish coat canyon walls near Lower Emerald Pool waterfall in Zion National Park, Springdale, Utah, USA. Manganese-rich desert varnish requires thousands of years to coat a rock face that is protected from precipitation and wind erosion. The varnish likely originates from airborne dust and external surface runoff, including: clay minerals, oxides and hydroxides of manganese (Mn) and/or iron (Fe), sand grains, trace elements, and usually organic matter. Streaks of black varnish often occur where water cascades over cliffs, but wind doesn't sculpt its shape. Varnish color varies from shades of brown to black. Manganese-poor, iron-rich varnishes are red to orange, and intermediate concentrations are shaded brown. Manganese-oxidizing microbes may explain the unusually high concentration of manganese in black desert varnish, which can be smooth and shiny where densest. More about Zion: The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    1303UTC-5012.jpg
  • A female lava lizard sheds skin on Santiago (or San Salvador, or James) Island, in the Galápagos archipelago, a province of Ecuador. Collectively known as lava lizards, seven ground lizard species of the reptile genus Tropidurus are endemic to the Galápagos Islands (and commonly placed in the genus Microlophus). All seven most likely evolved from a single ancestral species, demonstrating the principal of adaptive radiation that is typical of the inhabitants of the Galapagos archipelago. One lava lizard species occurs on all the central and western islands, which were perhaps connected during periods of lower sea levels, while one species each occurs on six other more peripheral islands. Males and females of all Tropidurus species are marked differently. The male is usually much larger than the female, and its body is more brightly colored and distinctly patterned. Markings vary considerably, even within an individual species. Animals living mainly on dark lava are darker than ones which live in lighter, sandy environments. Like many lizards, they show changes of color with mood and temperature. Santiago is equivalent to Saint James in English; and its alternative name San Salvador refers to the island discovered by Columbus in the Caribbean Sea. Santiago Island has a maximum altitude of 907 metres (2976 feet). Human-introduced pigs and goats caused great harm to the endemic species, but have been subsequently eradicated (pigs in 2002; goats almost all eliminated).
    09ECU-4158_Galapagos.jpg
  • A lava lizard rests on the toothy grinning head of a dead Galápagos Sea Lion (Zalophus wollebaeki) carcass drying on Punta (Point) Espinoza on Fernandina (Narborough) Island, Galápagos Islands, Ecuador, South America. Collectively known as lava lizards, seven ground lizard species of the reptile genus Tropidurus are endemic to the Galápagos Islands (and commonly placed in the genus Microlophus). All seven most likely evolved from a single ancestral species, demonstrating the principal of adaptive radiation that is typical of the inhabitants of the Galapagos archipelago. One lava lizard species occurs on all the central and western islands, which were perhaps connected during periods of lower sea levels, while one species each occurs on six other more peripheral islands. Males and females of all Tropidurus species are marked differently. The male is usually much larger than the female, and its body is more brightly colored and distinctly patterned. Markings vary considerably, even within an individual species. Animals living mainly on dark lava are darker than ones which live in lighter, sandy environments. Like many lizards, they show changes of color with mood and temperature. Published in "Light Travel: Photography on the Go" book by Tom Dempsey 2009, 2010.
    09ECU-3547_Galapagos.jpg
  • Lichen grows into polygons on sandstone polished by water, ice, and erosion in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT2-4006_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2270_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2263_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2252_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2250_Zion-NP-Utah.jpg
  • A seasonal waterfall plunges from Weeping Rock in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2247_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2238_Zion-NP-Utah-p2.jpg
  • A foot bridge crosses the Virgin River in Zion National Park, near Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 6 photos.)
    11UT1-2237-42pan_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2236_Zion-NP-Utah.jpg
  • A roayl arch forms on a sandstone cliff in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2233_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2221_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2215-18pan_Zion-NP-Utah.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2164_Zion-NP-Utah.jpg
  • Spring snow coats red sandstone and melts on the West Rim Trail on the way to Angels Landing and Scout Lookout, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2140_Zion-NP-Utah.jpg
  • Spring snow melts beside the West Rim Trail near Angels Landing and Scout Lookout, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet. (Panorama stitched from 2 photos.)
    11UT1-2138-39pan_Zion-NP-Utah.jpg
  • Lichen grows into polygons on sandstone polished by water, ice, and erosion in Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2126_Zion-NP-Utah.jpg
  • Spring snow coats red sandstone and melts on the West Rim Trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2113_Zion-NP-Utah-p2.jpg
  • Spring snow coats red sandstone and melts into a waterfall along West Rim Spring and the West Rim Trail, Zion National Park, Springdale, Utah, USA. The North Fork of the Virgin River carved spectacular Zion Canyon through reddish and tan-colored Navajo Sandstone up to half a mile (800 m) deep and 15 miles (24 km) long. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2112_Zion-NP-Utah-p1.jpg
  • The North Fork of the Virgin River cut Zion Canyon through reddish and tan-colored Navajo Sandstone, in Zion National Park. Springdale, Utah, USA. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3000 m) starting 13 million years ago. Zion and Kolob canyon geology includes 9 formations covering 150 million years of mostly Mesozoic-aged sedimentation, from warm, shallow seas, streams, lakes, vast deserts, and dry near-shore environments. Mormons discovered the canyon in 1858 and settled in the early 1860s. U.S. President Taft declared it Mukuntuweap National Monument in 1909. In 1918, the name changed to Zion (an ancient Hebrew name for Jerusalem), which became a National Park in 1919. The Kolob section (a 1937 National Monument) was added to Zion National Park in 1956. Unusually diverse plants and animals congregate here where the Colorado Plateau, Great Basin, and Mojave Desert meet.
    11UT1-2092-2101pan_Zion-NP-Utah.jpg
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