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  • 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
  • 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
  • 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
  • Double-crested Cormorants (Phalacrocorax auritus) perch on a drowned tree near Obsidian Butte, Sonny Bono Salton Sea Wildlife Refuge (EL -227ft).  This habitat for migratory birds is 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.
    Water Bird Habitat.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
  • 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 5, 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
  • 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
  • Dry mud texture at Dead Vlei in the Namib Desert, Namib-Naukluft Park, central Namibia.
    Dry Mud Texture, Namib Desert.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
  • Late summer sunrise at Waldo Lake 1650m with Three Sisters volcanoes beyond; Oregon Cascades
    Waldo Lake, Oregon.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
  • 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
    Glacier Retreat, Peru.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
  • 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
  • Southwest face of Churup Oeste (West) 5,493m, seen from Laguna Churup 4,450m, Cordillera Blanca, Peru.
    Glacier Retreat, Peru.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 Cooling Towers, Californi...jpg
  • Glacier Retreat on Chopicalqui.  Viewed from Chopicalqui Moraine Camp 5,000m.
    Glacier Retreat, Peru.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
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_06a_June-2020.jpg
  • Quiver trees (Aloe dichotoma), or Kokerboom in Afrikaans, silhoetted against an African dusk near Keetmanshoop in the Karas Region of Southern Namibia. This tree aloe survives in a small area of the southern Namibia desert, where summer temperatures exceed 45° C (113°F).
    Quiver Trees at dusk, Namibia.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
  • Mount Hood 3,426m (11,239 ft), viewed from Mount Tabor Park, Portland, Oregon, USA.
    AJH_181011_4686_MA.jpg
  • Dendritic drainage patterns in the desert hills of Baluchistan on the Afghan border, Pakistan.
    Baluchistan Desert, Pakistan.jpg
  • Continuous pumping is required from a system of channels and dikes around the Salton Sea to limit flooding of farmlands, a wildlife refuge and nearby geothermal energy plants.  The Sonny Bono Salton Sea Wildlife Refuge (EL -227ft) is 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.  The dikes now limit further encroachment.
    Drainage Management.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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