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  • Thick fog covers a high mountain valley beneath Mount Shuksan, a 9,127-foot (2,782-meter) peak located in the North Cascades National Park in Washington state. Valley fog, which is a type of radiation fog, can be incredible dense. It forms when air along ridgetops and mountain slopes cools after sunset. The air then becomes dense and sinks into the valley below where it continues to cool and becomes saturated, causing fog to form. Shuksan is derived from a Skagit Indian word meaning "rocky and precipitous."
    Shuksan_ValleyFog_0716.jpg
  • The nearly full moon shines over Mount Shuksan, a 9,131 foot (2,783 meter) mountain in Washington's North Cascades, which is reflected in Picture Lake. Shown here at about midnight, Mount Shuksan was formed about 120 million years ago when two of Earth's plates collided and were thrust upward in an event known as the Easton collision.
    Shuksan_Moon_Midnight_9616.jpg
  • Mount Shuksan, a 9,127-foot (2,782-meter) peak located in North Cascades National Park, Washington, casts its reflection onto the mostly still waters of Picture Lake at sunset. Shuksan is derived from a Skagit Indian word meaning "rocky and precipitous."
    Shuksan_Picture-Lake_Sunset_Reflecti...jpg
  • A bright fireball meteor from the Perseid meteor shower streaks across the sky over Mount Shuksan in the North Cascades of Washington state. The Perseids are an annual meteor shower that occurs in August when Earth passes through the debris of Comet 109P/Swift-Tuttle. The meteors are comet debris burning up in the Earth's atmosphere.
    Shuksan_Perseid-Meteor_1137.jpg
  • Mount Shuksan reflects on the still waters of Highwood Lake, which is lined by colorful American mountain ash (Sorbus americana). Mount Shuksan, one of the most photographed mountains, is located in Washington's North Cascades. Berries of the American mountain ash remain on the tree all winter, an important source of food for birds.
    Shuksan_MountainAsh_9956.jpg
  • The sun rises over Mount Shuksan, a 9,127-foot (2,782-meter) peak located in North Cascades National Park, Washington. Shuksan is derived from a Skagit Indian word meaning "rocky and precipitous." The mountain is reflected in a tarn near Artist Point.
    Shuksan_Sunburst_0792.jpg
  • A meteor from the Perseid meteor shower streaks across the sky over Mount Shuksan in the North Cascades of Washington state. The Perseids are an annual meteor shower that occurs in August when Earth passes through the debris of Comet 109P/Swift-Tuttle. The meteors are comet debris burning up in the Earth's atmosphere.
    Shuksan_Perseid-Meteor_1195.jpg
  • Mount Shuksan, a 9,131-foot (2,783-meter) mountain located in the North Cascades of Washington state, is covered in fresh snow on a cold winter day.
    Shuksan_Winter_Snowy_Sunset_0386.jpg
  • Mount Shuksan, a 9,131 foot (2,783 meter) mountain in Washington's North Cascades, stands tall over the icy Highwood Lake. Mount Shuksan, located in North Cascades National Park, is 9,131 feet (2,783 meters) tall and was formed about 120 million years ago when two of Earth's plates collided and were thrust upward in an event known as the Easton collision.
    Shuksan_LakeFall_Alpenglow_5222.jpg
  • Several Perseid meteors, including two especially bright ones, streak across the sky over Mount Shuksan in the North Cascades of Washington state. The Perseids are an annual meteor shower that occurs in August when Earth passes through the debris of Comet 109P/Swift-Tuttle. The meteors are comet debris burning up in the Earth's atmosphere.
    Shuksan_Perseid-Meteor_0898.jpg
  • Pink mountain heather (Phyllodoce empetriformis) grows in the cracks on the rocky hillside opposite of Mount Shuksan in the North Cascades of Washington state.
    Mount-Shuksan_Artist-Point_Pink-Moun...jpg
  • Mount Shuksan, 9,127-foot (2,782-meter) peak located in the North Cascades National Park in Washington, stands tall over a fog bank. Shuksan is derived from a Skagit Indian word meaning "rocky and precipitous."
    Shuksan_FogBank_0644.jpg
  • A meteor from the Perseid meteor shower streaks across the sky over Mount Shuksan in the North Cascades of Washington state. The Perseids are an annual meteor shower that occurs in August when Earth passes through the debris of Comet 109P/Swift-Tuttle. The meteors are comet debris burning up in the Earth's atmosphere.
    Shuksan_Perseid-Meteor_1180.jpg
  • A very large flock of snow geese (Chen caerulescens) fly over the Skagit Valley of Washington state with Mount Shuksan in the background. Tens of thousands of snow geese winter in the Skagit Valley, feeding in farmers' fields. They breed during the summer months on the upper reaches of Alaska, Canada, Greenland and Siberia. Mount Shuksan is a 9,131 foot (2,783 meter) mountain in the North Cascades.
    SnowGeese_Flock_Shuksan_Skagit_6176.jpg
  • Light snow on the last traces of fall color and a layer of ice on Highwood Lake illustrate the changing seasons at Mount Shuksan in Washington's North Cascades. Mount Shuksan, located in North Cascades National Park, is 9,131 feet (2,783 meters) tall and was formed about 120 million years ago when two of Earth's plates collided and were thrust upward in an event known as the Easton collision.
    Shuksan_LateFall_FirstSnow_5211.jpg
  • The Skagit River flows away from Mount Baker, a 10781 foot (3286 meter) volcano in the North Cascades of Washington state. Mount Shuksan, a 9131 foot (2783 meter) peak due east of Mount Baker, is visible in the background on the left side of this aerial view over Skagit County.
    Baker_Shuksan_SkagitRiver_Aerial_498...jpg
  • Mount Shuksan, located in the North Cascades of Washington state, is covered in fresh snow on a cold winter day.
    ShuksanWinterSunny.jpg
  • Thick fog shrouds Shuksan Arm, a steep rocky ridge in the North Cascades of Washington state. This was photographed from Artists Ridge, located at the end of the Mount Baker Highway (State Route 542), one of Washington state's scenic byways.
    ShuksanArmFog.jpg
  • Valley fog settles between the Shuksan Arm and several mountains in the North Cascades on the border of Washington and British Columbia. Valley fog is caused by a temperature inversion. Heavier cold air gets trapped in valleys while warmer air passes above.
    NorthCascades_FogBank_0719.jpg
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