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Geology { 15 images } Created 5 Sep 2009

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  • BubbleRockErratic1.tif
  • BubbleRockErratic2.tif
  • BubbleRockErratic3.tif
  • BubbleRockErratic4.tif
  • An abstract of fractured talus boulders taken near sunset at Blackrock Summit, Shenandoah National Park, VA
    ShenandoahBlackrockTalus1.tif
  • An HDR abstract of fractured talus boulders and lichen taken near sunset at Blackrock Summit, Shenandoah National Park, VA
    ShenandoahBlackrockTalus2.tif
  • Small cascade, pothole, and autumn willow above the Great Falls of the Potomac, Great Falls National Park, VA
    GreatFallsPotholeCascadeWillow.tif
  • Denail viewed from the road to Wonder Lake and terminal moraine left from the last advance of the Muldrow Glacier, Denali National Park, Alaska
    DenaliGlacialMoraine.tif
  • Late November sunrise on the Susquehanna River just below the Conowingo Dam, Conowingo, Maryland.  The Susquehanna River provides a large amount of the freshwater inflow and pollution going into to the Chesapeake Bay, which is a ria of the Susquehanna.
    ConowingoSunrise.tif
  • Collection of river stones covered by snow along the banks of the Potomac River just above the Great Falls, Mather Gorge, Great Falls National Park, Great Falls, VA
    GreatFallsRocksAndSnow.tif
  • Metamorphic river rocks and overflowing water from the rapids photographed at twilight near the bottom of the Great Falls of the Potomac, Chesapeake and Ohio National Historic Park, Potomac, Maryland. Sepia toned Black and White Image.
    RiverRocksTwilightGreatFalls.tif
  • A chipped quartz stone has become lodged in between two boulders along the side of the Potomac River by the force of the current, Fisherman's Eddy, Great Falls National Park, Great Falls, Virginia
    GreatFallsRock1BW.tif
  • Sandstone and white quartz boulders from the Pottsville Conglomerate with black huckleberry (Gaylussacia baccata) in the foreground, Bear Rocks Preserve, Dolly Sods, West Virginia.  The formation in the background is known informally as "The Dragon of Dolly Sods" and has been formed over the past 60,000 to 240,000 years by chemical and physical weathering processes.
    BearRocksDragon1BW.tif
  • Wave-formed ripple marks in a sandbar exposed at low tide, Cape Henlopen State Park, Lewes, Delaware
    WaveFormedRippleMarksSunset1.tif
  • Wave-formed ripple marks in a sandbar exposed at low tide, Cape Henlopen State Park, Lewes, Delaware
    WaveFormedRippleMarksSunset2.tif