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  • Glacier Retreat on Chopicalqui.  Viewed from Chopicalqui Moraine Camp 5,000m.
    Glacier Retreat, Peru.jpg
  • Glacier Retreat on Chopicalqui.  Viewed from Chopicalqui Moraine Camp 5,000m.
    38_AJH_080626_1912_DRV.jpg
  • Mount Hood 3,426m (11,239ft) at sunrise, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with World Climate Change.  Nikon D700. AF300/4.
    AJH_02b_February-2019.jpg
  • Glacier retreat from the lateral moraine below Pisco Col 5,300m (17,390ft), and Nevado Pisco Oeste (West) 5,752m (18,870ft), Cordillera Blanca, Peru.  Ricoh GR-1v; 28mm/2.8.  Fuji RVP100F.  20 June 2008.
    Lateral Moraine, Peru.jpg
  • Steve Cooke abseils the Southwest Ridge Route of Mount Kenya as a storm clears.  The summit of Point John 4883m (16,020ft) is visible behind and below.  Point Slade 4750m (15,584ft) is the pinnacle on the right.
    Batian, Mount Kenya
  • Illumination Rock 2,909m (9,543ft) and Illumination Saddle 2,865m (9,400ft).  Illumination Rock is a spectacular spire of rotten basalt on the southwest side of Mt Hood, a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  Powerful glacial forces have eroded down a former rock ridge, leaving this sprire shaped like the fin of a fish.  The mountain's twelve glaciers are thinning as a result of glacial retreat.
    Illumination Rock, Mt Hood
  • Mount Hood 3,426m (11,239ft) viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with World Climate Change.  Nikon D700. Nikon AF Nikkor 300mm f/4 IF-ED.
    AJH_160916_9117.jpg
  • Castle Crags from Illumination Saddle 2,865m (9,400ft), with Leuthold Couloir (FA 1932) far left, and the Yocum Ridge above the couloir.  Castle Crag is a spectacular spire of rotten basalt on the southwest side of Mt Hood, a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  Powerful glacial forces have eroded down a former rock ridge, leaving this fantasy sprire.  The mountain's twelve glaciers are thinning as a result of glacial retreat.
    Castle Crags, Mt Hood
  • Mount Hood 3,426m (11,239ft) at sunrise, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with World Climate Change.  Nikon D700. AF300/4.
    AJH_130118_0285.jpg
  • Mount Hood 3,426m (11,239ft) at sunrise, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with World Climate Change.  Nikon D700. Nikon AF Nikkor 300mm f/4 IF-ED.
    AJH_160224_8039_MA.jpg
  • Mount Hood 3426m (11,239ft) casts its own shadow at sunrise, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with World Climate Change.  Nikon F4, AF300/4. Kodak E100VS
    Mount Hood Shadow, Mt Tabor Park.jpg
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m
    Glacier Retreat, Peru.jpg
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m, Cordillera Blanca, Peru.
    Glacier Retreat, Peru.jpg
  • Mount Hood 3,426m (11,239ft) viewed from Portland, Oregon.  The left skyline is the Northwest Ridge (named Cathedral Ridge); the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon. Sunrise provides backlighting glow to radiation fog (Valley Fog) filling the valleys on this cool autumn morning. Radiation fog results from radiation cooling of the ground and adjacent air under clear night skies and elevated relative humidity, most common in autumn. Normally, this fog dissipates within a few hours of sunrise as the sun warms the ground.
    AJH_221008_1243.jpg
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_06a_June-2020.jpg
  • Super Blood Moon Lunar Eclipse of 2015.  This image captures the total lunar eclipse of the Harvest Moon supermoon as it rises over Mount Hood 3,426m (11,239 ft), Portland, Oregon on 27 September 2015.  Time of maximum eclipse 1947 PDT.
    Super Blood Moon Lunar Eclipse 2015.jpg
  • Sonny Bono Salton Sea Wildlife Refuge (EL -227ft), located along the course of the Pacific Flyway in the Imperial Valley of California.  Flooding by the Salton Sea has reduced the manageable area from 36,700 acres to 2,200 acres.  Dykes (dikes) now limit further encroachment.
    Geothermal Energy, California.jpg
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m.
    Churup Summit
  • Late summer sunrise at Waldo Lake 1650m with Three Sisters volcanoes beyond; Oregon Cascades
    Waldo Lake, Oregon.jpg
  • Mount St Helens ash eruption, 2005, viewed from Portland, Oregon.  As if to signal the 25th anniversary of the devastating 1980 eruption, Mount St. Helens released this symbolic outpouring of ash and steam at 17:30 on Tuesday evening, March 8, 2005.  Volcanic ash rose to 36,000 feet and fell as far away as 125 miles east of the mountain. The eruption began with practically no warning, an hour after a magnitude 2.0 earthquake on the volcano's east side, and lasted 30 minutes.  Mount St. Helens, a 8,364-foot (2550m) volcano, is located about 40 miles (60km) northeast of Vancouver, Washington, Portland's sister city across the Columbia River which divides the states of Oregon and Washington.  The river in the photograph is the Willamette River, which divides Portland's east and west sides.  The Columbia River is not visible in this image; it runs perpendicular to the Willamette.  Mount St. Helens was named for British diplomat Alleyne Fitzherbert whose title was Baron St. Helens.  The mountain was named by Commander George Vancouver and the officers of H.M.S. Discovery while exploring the northern Pacific coast from 1792 to 1794.  Mount St. Helens erupted violently at 08:32 on Sunday, May 18, 1980.  Nikon F4S, 70-300/4-5.6D. Fuji RVP100F..
    Mount St Helens Eruption 2005.jpg
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m.
    Churup SW Vertical
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_181011_4686_MA.jpg
  • Sean Bartleet climbing the West Ridge of Mount Jefferson 3,199m (10,497ft), via the Milk Creek/West Ridge route; Grade II, Class 4.  This route is approached from Pamelia Lake and Point 4400 (ft).  Nikon F100, 24-50/3.3-4.5D, Kodak E100VS.
    West Ridge, Mt Jefferson
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m.
    Churup SW Face
  • Sonny Bono Salton Sea Wildlife Refuge (EL -227ft), located along the course of the Pacific Flyway in the Imperial Valley of California.  Flooding by the Salton Sea has reduced the manageable area from 36,700 acres to 2,200 acres.  Dykes (dikes) now limit further encroachment.
    Salton Sea, California.jpg
  • Backlit morning valley mist with Mount Hood 3,426m (11,239ft) beyond, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with world climate change.
    Mt Hood and East Portland.jpg
  • Backlit morning valley mist with Mount Hood 3,426m (11,239ft) beyond, viewed from Mount Tabor Park in Portland.  The left skyline is Cathedral Ridge, and the right skyline is the Southeast Ridge.  The bulge in the Southeast Ridge is called the Steel Cliff.  Mount Hood is a stratovolcano in the Cascade Volcanic Arc of Northern Oregon.  The mountain's twelve glaciers are thinning as a result of glacial retreat attributed to Global Warming associated with world climate change.
    Mt Hood and Valley Mist.jpg
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