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  • 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
  • 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
  • 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
  • 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
  • Dendritic drainage patterns on the Tsauchab Plains of the Namib Desert.  Aerial view from above the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Drainage Pattern 3, Namib Desert.jpg
  • Dendritic drainage patterns on the Tsauchab Plains of the Namib Desert.  Aerial view from above the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Drainage Pattern 2, Namib Desert.jpg
  • Dendritic drainage patterns on the Tsauchab Plains of the Namib Desert.  Aerial view from above the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Drainage Pattern 1, Namib Desert.jpg
  • Glacier Retreat on Chopicalqui.  Viewed from Chopicalqui Moraine Camp 5,000m.
    38_AJH_080626_1912_DRV.jpg
  • Dendritic drainage patterns on the Tsauchab Plains of the Namib Desert.  Aerial view from above the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Drainage Pattern 5, Namib Desert.jpg
  • Aerial view of wildlife fence and its shadow falling across a gravel maintenance road, viewed from directly overhead the Tsauchab Plains of the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Aerial Fence and Shadow
  • Joshua Tree (Yucca brevifolia) in the Mojave Desert, is ironically inundated by surface rain water runoff after a heavy rain storm in Joshua Tree National Park, California.  Several studies have been done on these centuries-old trees.  In a current study, ecologists from the US Geological Survey linked climate change to population decline and are modeling the impacts of climate change on their survival, and the possibility that 90 percent will be wiped out of their current range (and out of this national park) in 60 to 90 years.
    Joshua Tree - victim of climate chan...jpg
  • Dendritic drainage patterns on the Tsauchab Plains of the Namib Desert.  Aerial view from above the Namib-Naukluft Park near Sossusvlei in central Namibia, southwest Africa.
    Drainage Pattern 4, Namib Desert.jpg
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_06a_June-2020.jpg
  • Dry mud texture at Dead Vlei in the Namib Desert, Namib-Naukluft Park, central Namibia.
    Dry Mud Texture, Namib Desert.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
  • 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
  • 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
  • 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
  • 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
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m.
    Churup SW Vertical
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m
    Glacier Retreat, Peru.jpg
  • September 8, 2020 - Wildfire smoke begins to engulf the Portland Metro area at sunset on Tuesday September 8, 2020. Viewed from Mount Tabor towards Kelly Butte (L) and Mount Scott (R). Smoke from multiple fires burning in Clackamas County, and as close as Estacada, is moving north towards Portland as fires spread and strong easterly blocking winds in the Columbia Gorge subside.
    Wildfire Smoke Portland 2020.jpg
  • Reflection of three dead trees near Red Hill Marina, Hazard Tract, Salton Sea, California.  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
  • 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
  • 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
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_181011_4686_MA.jpg
  • 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.
    Geothermal Cooling Towers, Californi...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.
    Salton Sea, California.jpg
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m, Cordillera Blanca, Peru.
    Glacier Retreat, Peru.jpg
  • Glacier Retreat on Chopicalqui.  Viewed from Chopicalqui Moraine Camp 5,000m.
    Glacier Retreat, Peru.jpg
  • Dead camelthorn trees (Acacia erioloba) at Dead Vlei, Namib Desert, Namibia. The clay pan was formed after rainfall and flooding of the Tsauchab River.  Once abundant water allowed camel thorn trees to thrive.  Climate change brought drought, which killed the trees.  The dunes encroached and isolated the pan.  The extreme dryness preserves the trees from decomposing.
    Dead Vlei, Namib Desert.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
  • Photographs from an 8-day sailboat delivery from Cowes, England to Copenhagen, Denmark, across the English Channel, the North Sea and the Baltic. The passage was made via the 98km Kiel Canal, with stops in Brunsbuttel, Kiel, Laboe, Rodbyhavn, Klintholm, Copenhagen and Rungsted. The vessel was the Sparkman & Stephens designed Swan 76 ketch named Tigris, built in 1981.
    AJH_230406_2782_MA.jpg
  • Warm to cool; sun's last rays on the curved wall of Gatehouse 5, Mount Tabor Park, Portland, Oregon, USA.
    AJH_190930_5966_MA.jpg
  • Warm to cool; sun's last rays on the curved wall of Gatehouse 5, Mount Tabor Park, Portland, Oregon, USA.
    AJH_08b_August-2020.jpg
  • Mariners' Warning.  The remains of the wreck of the Peter Iredale contrast with the warm glow of two fishing vessels beyond the horizon, working beneath a Pacific winter squall hitting the Oregon coast at midnight.  Once a two-thousand ton four-masted steel barque, this bow section is all that remains of the sailing vessel that ran aground on 25 October 1906.  Nikon D700, 20-35/2.8D.
    peter-iredale-shipwreck-fishing-vess...jpg
  • Spray swirls and batters a dead tree at the discharge pipe from Upper Snow Lake 1,650m (5,415ft) above Nada Lake in the Snow Creek Valley, Snow Lakes Basin in the Alpine Lakes Wilderness.  The Snow Lake Reservoir and tunnel was built by the Bureau of Reclamation (1939 to 1942) to serve as a supplemental water source for the Leavenworth Hatchery during the summer months when flows in Icicle Creek run low and warm.  Okanogan–Wenatchee National Forest near Leavenworth, Washington.
    Battered Tree, Snow Lake
  • Franklin High School's north facade is bathed in warm evening light in 2018, after completion of an extensive seismic upgrade and remodel project. Between 2015 and 2017, the school was modernized and expanded, with funding from a $482 million bond measure in 2012. The modernization included a new arts center, a new gym, biomedical, and culinary arts building, seismic retrofitting, and a new entrance. The main building was designed by Floyd Naramore, modeled on the Colonial Revival architectural style, and completed in 1917.
    franklin-high-school-portland-oregon.jpg
  • Sunrise Alpenglow warms the basalt cliffs of Beacon Buttress 3121m (10,240 ft), also known as Western Buttress, with Eastern Buttress 3047m (9,996 ft), Devil's Tooth 3019m (9,902 ft) and Inner Tower 3044m (9,986 ft). Ukhahlamba-Drakensberg Park, KwaZulu-Natal, South Africa.  Nikon F90, 24/2.8D. Fuji RDP. September 1994
    Beacon Buttress Drakensberg.jpg
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Andrew Haliburton

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