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  • Water droplets cling to the back of a Wych elm (Ulmus glabra) leaf.
    Elm_Leaf_Back_Droplets_Macro_Lynnwoo...jpg
  • Water droplets cling to the back of a Wych elm (Ulmus glabra) leaf.
    Elm_Leaf_Back_Droplets_Macro_Lynnwoo...jpg
  • Water droplets cling to moss growing on an old tree in Snohomish County, Washington.
    Moss_Water-Droplets_1741.jpg
  • Water droplets are forced into the air as the Little White Salmon River crashes into rocks in Skamania County, Washington, near the Columbia River Gorge. A fast shutter speed captures the droplets suspended in air against the sunlit turquoise-colored backdrop of the silt-filled river.
    WA_LittleWhiteSalmonRiver_Splash_729...jpg
  • Water droplets are forced into the air as the Little White Salmon River crashes into rocks in Skamania County, Washington, near the Columbia River Gorge. A fast shutter speed captures the droplets suspended in air against the sunlit turquoise-colored backdrop of the silt-filled river.
    WA_LittleWhiteSalmonRiver_Splash_740...jpg
  • A hole-punch cloud is typically formed when an airplane passes through altocumulus clouds. Altocumulus clouds are made up of small, super cooled water droplets. When aircraft pass through these clouds, the rapid pressure changes they cause can cool the air further. That, in turn, causes the water droplets to form heavy ice crystals, which then drop from the sky, leaving behind a "hole punch." This hole-punch cloud was observed in Thurston County, Washington. Hole-punch clouds are also sometimes called sky-punch clouds.
    Cloud_HolePunch_1831.jpg
  • Water droplets cling to a wild daffodil (Narcissus pseudonarcissus) after a rain storm. They are shown here in an extreme macro view of approximately four times life-size.
    Daffodil-Wild_Rain-Drops_Macro_0561.jpg
  • Water droplets cling to a wild daffodil (Narcissus pseudonarcissus) after a rain storm. They are shown here in an extreme macro view of approximately five times life-size.
    Daffodil-Wild_Rain-Drops_Macro_0613.jpg
  • Water droplets cling to a wild daffodil (Narcissus pseudonarcissus) after a rain storm. They are shown here in an extreme macro view of approximately five times life-size.
    Daffodil-Wild_Rain-Drops_Macro_0599.jpg
  • Hundreds of water droplets cling to blades of grass on a lawn in Snohomish County, Washington.
    Grass_Dew-Drops_Lynnwood_0278.jpg
  • After a rainstorm, water drops cling to the flowers of a red-flowering currant (Ribes sanguineum).
    Currant-Flowering_Blooming_Water-Dro...jpg
  • A gadwall (Anas strepera) uses its wings to splash water so it can bathe on one of the Promontory Ponds in Magnuson Park, Seattle, Washington.
    Gadwall_Bathing_Magnuson-Park_2387.jpg
  • A female harlequin duck (Histrionicus histrionicus) splashes in the water to shower off West Beach in Deception Pass State Park on Whidbey Island, Washington. During the winter months, harlequin ducks are found along the northern Pacific and Atlantic coasts, most commonly along rocky coastlines in the crashing surf.
    Duck_Harlequin_Splashing_Deception-P...jpg
  • After a rainstorm, water drops cling to the flowers of a red-flowering currant (Ribes sanguineum).
    Currant-Flowering_Blooming_Water-Dro...jpg
  • After a rainstorm, water drops cling to the flowers of a red-flowering currant (Ribes sanguineum).
    Currant-Flowering_Blooming_Water-Dro...jpg
  • Numerous stalks of Northern Giant Horsetail (Equisetum telmateia braunii) are clustered together in the Grays Harbor National Wildlife Refuge near Hoquiam, Washington.
    Horsetail_Stalks_Young_7653.jpg
  • An extreme macro view — approximately five times life-size — and shallow focus isolate a water drop clinging to a blade of moss growing on a tree in Snohomish County, Washington.
    Moss_Water-Drop_Macro_2088.jpg
  • Rain falls and drips from the leaves of a vine maple tree in Twin Falls State Park near North Bend, Washington.
    Rain_VineMapleLeaves_7160.jpg
  • An extreme macro view — approximately five times life-size — and shallow focus isolate a water drop clinging to a blade of moss growing on a tree in Snohomish County, Washington.
    Moss_Water-Drop_Macro_2098.jpg
  • Dew collects on the back of a fallen maple leaf in Carkeek Park, Seattle, Washington.
    Fall_Leaf_DewDrops_Carkeek_5119.jpg
  • A drop of water splashes in a glass.
    WaterDrop_Splash_6030.jpg
  • An extreme macro view — approximately five times magnification — contrasts the leg of a garden spider against a spiderweb in high-contrast light. The colorful streaks on the web are the result of iridescence — light being bent into different wavelengths by the tiny droplets on the threads.
    Spider_Leg_Web_Iridescence_Macro_235...jpg
  • A moose (Alces alces) shakes to dry off as it emerges from Fishercap Lake, located in Glacier National Park, Montana. The moose and the flying water droplets are blurred by a long exposure to capture their movement.
    moose-FishercapLake-0377.jpg
  • Bright, rainbow-like colors are visible in thin clouds known as iridescent clouds over Bryce Canyon in Utah. Iridescent clouds are relatively rare and appear in clouds formed of small water droplets of nearly uniform size. Commonly, iridescent clouds are near much thicker clouds that partially hide the sun.
    Cloud_Iridescent_Bryce_1071.jpg
  • Delicate stalactites, called soda straws, hang from the ceiling of the Painted Grotto in Carlsbad Caverns National Park, New Mexico. Soda straws develop where water droplets hang from the ceiling. Initially, a calcite ring forms on the ceiling. Calcite deposits continue to accumulate on the initial ring, and the straw grows longer as the deposits build up. If enough calcite deposits build up, the soda straws can develop into large stalactites. Calcite is a colorless mineral in its pure form. The presence of other minerals causes the stalactites in the cavern to take on yellow, orange, red, or brown coloration.
    CarlsbadCaverns_PaintedGrotto_1205.jpg
  • A cap cloud covers the summit of Mount Baker, a 10,778 feet (3,285 m) volcano in Washington state. Cap clouds, technically called orographic stratiform clouds, form when moist air is forced over a mountaintop. The moisture condenses into water droplets as it climbs in elevation.
    Baker_CapCloud_0523.jpg
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