Michael Durham Photography

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  • 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
  • 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
  • An abandoned structure in the high-desert of Oregon, near Painted Hills State Park.
    leaning_shack_41009JBf-108.jpg
  • a sample of the mineral graphite which is an allotrope of carbon. It is often used to make pencil lead.
    graphite_rock__5508Graph.jpg
  • A sample of galena or lead sulfide. It finds limited use in electronic devices. Also known as galena, it is the principal ore and most important compound of lead.
    lead_sulfide_5508Galena1.jpg
  • a sample of a pyrite
    iron_pyrite_5508pyrite.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
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