Michael Durham Photography

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  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-189.jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-202.jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-202-...jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-201.jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-201-...jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-191.jpg
  • The Cathedral Rock feature of the John Day Fossil Beds National Monument; Oregon.
    oregon_cathedral_rock_12510JDFB-191-...jpg
  • Entrance to Craters of the Moon National Monument, Idaho.
    craters_of_the_moon_62710Bctr-106.jpg
  • Colorful layers of minerals create bands of color at Painted Hills State park, Oregon. The black soil is lignite that was vegetative matter that grew along the floodplain. The grey coloring is mudstone, siltstone, and shale. The red coloring is laterite soil that formed by floodplain deposits when the area was warm and humid
    oregon_painted_hills_41009JBf-Pn1.jpg
  • Colorful layers of minerals create bands of color at Painted Hills State park, Oregon. The black soil is lignite that was vegetative matter that grew along the floodplain. The grey coloring is mudstone, siltstone, and shale. The red coloring is laterite soil that formed by floodplain deposits when the area was warm and humid
    oregon_painted_hills_41009JBf-27-1.jpg
  • Entrance to Craters of the Moon National Monument, Idaho.
    craters_of_the_moon_62710Bctr-109.jpg
  • Colorful layers of minerals create bands of color at Painted Hills State park, Oregon. The black soil is lignite that was vegetative matter that grew along the floodplain. The grey coloring is mudstone, siltstone, and shale. The red coloring is laterite soil that formed by floodplain deposits when the area was warm and humid
    oregon_painted_hills_41009JBf-Pn2.jpg
  • Quartz is revelaed inside a broken rock retrieved from a rock slide on Forest Road 57 in the Mount Hood National Forest, Oregon.
    quartz-rock-21613Qtz-102.jpg
  • The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-171.jpg
  • The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-168.jpg
  • The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-166.jpg
  • Detail of the volcanic tuff of the Blue Basin feature in the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    volcanic_tuff_12510JDFB-161.jpg
  • Water runs green in the The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    green_runoff_12510JDFB-154.jpg
  • A landslide blocks Forest Road 57 in Mount Hood National Forest, Oregon.
    landslide-blocking-road-21613Qtz-109.jpg
  • A glacial erratic rock from Canada, deposited in Oregon by the Missoula floods, atop a foothill of the Northern Oregon Coast Range in Yamhill County between Sheridan and McMinnville off Oregon Route 18.  The rock is argillite believed to be 600 million years old and is also the only rock of its type outside of Canada.
    glacial_erratic_12812ERt-114.jpg
  • A sign forbidding removal of rocks or fossils at the Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    removal_of_rocks_prohibited_12510JDF...jpg
  • The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-182.jpg
  • The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-181.jpg
  • Volcanic rocks mixed with light snow within the Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    blue_basin_john_day_12510JDFB-176.jpg
  • detail of the volcanic tuff of the Blue Basin feature in the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    volcanic_tuff_12510JDFB-146.jpg
  • detail of the volcanic tuff of the Blue Basin feature in the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    volcanic_tuff_12510JDFB-145.jpg
  • detail of the volcanic tuff of the Blue Basin feature in the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    volcanic_tuff_12510JDFB-145-Edit.jpg
  • The crumbling crust of an ancient lava flow called the "blue dragon lava flow". The blue color comes from a thin outer layer of lava that contains titanium magnetite crystals. Craters of the Moon National Monument, Idaho
    blue_lava_7710Sdr-104.jpg
  • A sign forbidding removal of rocks or fossils at the Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    removal_of_rocks_prohibited_12510JDF...jpg
  • A sign marking the end of the trail at The Blue Basin feature of the John Day Fossil Beds National Monument; Oregon. Formed from 29-million-year-old volcanic tuff, The erosion scarred slopes of these hills are slowly yielding fossils of ancient animals and plants.
    end_of_trail_12510JDFB-178.jpg
  • volcanic tuff, blue basin, john day fossil beds national monument, green hills, volcanic landscape, fossil bed, fossil beds, oregon, ancient geology,
    blue_basin_john_day_12510jDFBPAn1V2.jpg
  • volcanic tuff, blue basin, john day fossil beds national monument, green hills, volcanic landscape, fossil bed, fossil beds, oregon, ancient geology,
    blue_basin_john_day_12510jDFBPAn1.jpg
  • Goose Rock, a geologic formation above the John Day River in the John Day Fossil Beds National Monument, Oregon. Please note: a filter has been applied to give this image a vintage look.
    john_day_river_cliff_102210cCO_PAN1V...jpg
  • Goose Rock, a geologic formation above the John Day River in the John Day Fossil Beds National Monument, Oregon.
    john_day_river_cliff_102210cCO_PAN1.jpg
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