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  • Immature yellow-crowned night heron, Nyctanassa violacea, at the shore of the Tarcoles River, Costa Rica
    09061254-night-heron.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040212.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040209.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040208.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040211.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040210.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040207.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040206.jpg
  • A juvenile Black-crowned Night Heron, Nycticorax nycticorax, stands on the shore of a small lake in Papago Park, part of the Phoenix Mountains Preserve near Phoenix, Arizona
    19040205.jpg
  • Juvenile Yellow-crowned Night Heron, Nyctanassa violacea, near the Tortuguero River (Rio Tortuguero) in Tortuguero National Park, Costa Rica
    17050183.jpg
  • A previously undescribed species of night skink, tentatively called Eremiascincus sp. A, from Ermera Province, Timor-Leste (East Timor).
    10040395-skink.jpg
  • Black-crowned Night Herons, Nycticorax nycticorax, at Colusa National Wildlife Refuge, California
    19050124.jpg
  • A previously undescribed species of night skink, tentatively called Eremiascincus sp. A, from Ermera Province, Timor-Leste (East Timor).
    10040411-skink.jpg
  • A previously undescribed species of night skink, tentatively called Eremiascincus sp. B, from Ermera Province, Timor-Leste (East Timor).
    10040408-skink.jpg
  • A previously undescribed species of night skink, tentatively called Eremiascincus sp. B, from Ermera Province, Timor-Leste (East Timor).
    10040406-skink.jpg
  • A previously undescribed species of night skink, tentatively called Eremiascincus sp. A, from Ermera Province, Timor-Leste (East Timor).
    10040398-skink.jpg
  • Sphinx moth, Manduca sexta, approaches a Sacred Datura flower, Datura wrightii, at night in Joshua Tree National Park, California
    639-31.jpg
  • Sphinx moth, Manduca sexta, approaches a Sacred Datura flower, Datura wrightii, at night in Joshua Tree National Park, California
    639-33.jpg
  • Northern Cat-eyed Snake, Leptodeira septentrionalis, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050413.jpg
  • Glasswing Butterfly, Greta morgane, perched on a leaf at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050460.jpg
  • Glasswing Butterfly, Greta morgane, perched on a leaf at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050457.jpg
  • Taylor's Leopard Frog (Peralta Frog), Lithobates taylori (formerly Rana taylori), metamorph, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050410.jpg
  • Masked Treefrog, Smilisca phaeota, near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called the New Granada Cross-banded Treefrog.
    17050409.jpg
  • Vaillant's Frog, Lithobates vaillanti (formerly Rana vaillanti), near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050405.jpg
  • Rain Frog eggs, probably from Fitzinger's Rainfrog or Robber Frog, Craugastor fitzingeri, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050398.jpg
  • Brilliant Forest Frog, Lithobates warszewitschii, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050392.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140161-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140158-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140155-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140144-mono-lake.jpg
  • Moonlit ruins of the Porter Brothers Store building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140695-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140692-rhyolite.jpg
  • Cloudy Snail-eating Snake, Sibon nebulatus, near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called Slugeater or Snail Sucker
    17050411.jpg
  • Slender Anole, Anolis limifrons (Norops limifrons), on a leaf near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050391.jpg
  • Web-casting spider, Deinopis longipes, at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050466.jpg
  • Glasswing Butterfly, Greta morgane, perched on a leaf at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050459.jpg
  • Glasswing Butterfly, Greta morgane, perched on a leaf at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050458.jpg
  • Glasswing Butterfly, Greta morgane, perched on a leaf at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050456.jpg
  • Masked Treefrog, Smilisca phaeota, poses for a smartphone photo near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called the New Granada Cross-banded Treefrog. This is a composite image; the smartphone photo is simulated.
    17050407.jpg
  • Rain Frog eggs, probably from Fitzinger's Rainfrog or Robber Frog, Craugastor fitzingeri, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050399.jpg
  • Bransford's Litterfrog or Robber Frog, Craugastor bransfordii, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050393.jpg
  • Bransford's Litterfrog or Robber Frog, Craugastor bransfordii, Near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050389.jpg
  • Masked Treefrog, Smilisca phaeota, in Arenal Volcano National Park, Costa Rica. Also called the New Granada Cross-banded Treefrog.
    17050382.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140162-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140160-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140156-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140154-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140146-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140145-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140143-mono-lake.jpg
  • Moonlit ruins of the school building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140699-rhyolite.jpg
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140698-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140688-rhyolite.jpg
  • Stars over the Panamint Mountains, Death Valley National Park, California
    08070211-death-valley.jpg
  • Neotropical Green Anole, Anolis serranoi  (Norops biporcatus), near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050416.jpg
  • Casque-headed Lizard, Corytophanes cristatus, near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called Helmet-headed Lizard, Helmeted Basilisk, or Smooth-helmeted Iguana
    17050395.jpg
  • Web-casting spider, Deinopis longipes, at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050465.jpg
  • Stick Insect, Order Phasmatodea, at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050453.jpg
  • Litter Toad (Truando Toad), Rhaebo haematiticus (formerly Bufo haematiticus), near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050415.jpg
  • Hourglass Treefrog, Dendropsophus ebraccatus (formerly Hyla ebraccata), on a leaf near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called the Harlequin Treefrog.
    17050414.jpg
  • Eggs of Hourglass Treefrog, Dendropsophus ebraccatus (formerly Hyla ebraccata), on a leaf near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called the Harlequin Treefrog.
    17050412.jpg
  • Vaillant's Frog, Lithobates vaillanti (formerly Rana vaillanti), near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050406.jpg
  • Common Mexican Treefrog, Smilisca baudinii, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050402.jpg
  • Rain Frog eggs, probably from Fitzinger's Rainfrog or Robber Frog, Craugastor fitzingeri, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050400.jpg
  • Bransford's Litterfrog or Robber Frog, Craugastor bransfordii, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050394.jpg
  • Masked Treefrog, Smilisca phaeota, in Arenal Volcano National Park, Costa Rica. Also called the New Granada Cross-banded Treefrog.
    17050383.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140157-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140153-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140152-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140149-mono-lake.jpg
  • Moonlit ruins of the school building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140700-rhyolite.jpg
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140696-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140693-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140690-rhyolite.jpg
  • One-room schoolhouse at Ryan, California, a 1920s mining camp in the Greenwater Range on the Eastern edge of Death Valley
    08070003-ryan-school.jpg
  • Casque-headed Lizard, Corytophanes cristatus, near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called Helmet-headed Lizard, Helmeted Basilisk, or Smooth-helmeted Iguana
    17050396.jpg
  • Stick Insect, Order Phasmatodea, at Bosque Eterno de los Niños (Children’s Eternal Rainforest), Monteverde, Costa Rica
    17050467.jpg
  • Masked Treefrog, Smilisca phaeota, near Arenal Volcano National Park, La Fortuna, Costa Rica. Also called the New Granada Cross-banded Treefrog.
    17050408.jpg
  • Rain Frog eggs, probably from Fitzinger's Rainfrog or Robber Frog, Craugastor fitzingeri, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050401.jpg
  • Rain Frog eggs, probably from Fitzinger's Rainfrog or Robber Frog, Craugastor fitzingeri, near Arenal Volcano National Park, La Fortuna, Costa Rica
    17050397.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140165-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140164-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140148-mono-lake.jpg
  • Tufa towers in moonlight at the South Tufa Area, Mono Lake Tufa State Natural Reserve, Mono Lake, California. Tufa is formed when springs under the lake mix calcium-rich freshwater with alkaline lakewater, precipitating deposits of calcium carbonate. The lake level has dropped more than 30 feet since 1941, when the city of Los Angeles began diverting water from the streams that feed it, exposing the formerly submerged tufa.
    11140147-mono-lake.jpg
  • Moonlit ruins of the Overbury Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140697-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140694-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140687-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140686-rhyolite.jpg
  • Moonlit ruins of the Cook Bank building in the ghost town of Rhyolite, Nevada, a mining boomtown that, at its peak between 1905 and 1912, had a population of 5,000 to 10,000.
    10140684-rhyolite.jpg
  • Sacred datura (jimson weed, thorn apple, angel trumpet), Datura wrightii, Mojave Desert, California. Also available: pollination by sphinx moth. Datura is a powerful and dangerous hallucinogen that has been used ceremonially by Native Americans, as well as recreationally by more recent arrivals.
    639-07seq.jpg