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  • A bolt of lightning strikes the Chesapeake Bay during a brief and fast moving storm. As seen from North Beach in Calvert County, Maryland.
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  • The mouth of the Potomac river fades into the distance at first light at Point Lookout State Park, MD. Where the Potomac River meets the Chesapeake Bay.
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  • Water gushes through a canal lock on the historic C&O canal. As seen from Thomas Jefferson Street in the Georgetown Neighborhood of Washington, D.C. Short for Chesapeake & Ohio, the canal was intended to connect the eastern seaboard with the Ohio river valley region. With construction beginning in the 1830's, the canal was overtaken by the faster and more efficient B&O railroad, and construction was halted as far as Cumberland, Maryland.
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  • The view South while standing on the roof of a building on Solomon's Island, where the Patuxent River empties into the Chesapeake Bay.
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  • The view South while standing on the roof of a building on Solomon's Island, where the Patuxent River empties into the Chesapeake Bay.
    maryland019.JPG
  • A long exposure turns the churning waters where the Potomac River and Chesapeake Bay meet seemingly to glass at the tip of Point Lookout State Park in St. Mary's County, MD.
    maryland015.JPG
  • The C&O Canal (short for Chesapeake and Ohio) is seen at dusk along the towpath at Great Falls in Potomac, MD. <br />
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The C&O Canal was created in the 1830's in an effort to connect the Ohio River Valley frontier with the East Coast. However, trains were beginning to come onto the scene around the time of construction. Beginning with the B&O Railroad based out of Baltimore, trains could carry much larger cargos than canal boats, travel faster and be constructed far easier than digging and dredging canals. Construction was halted at Cumberland Maryland, 100 miles west of Washington, as the railroad arrived at Pittsburgh, making the canals original purposes obsolete. Nonetheless, the canal was widely used for transportation of raw materials such as coal from mines in West Virginia. The canal fell into disuse by the 20th century, and the National Parks Service purchased the canal in the 1930's.
    maryland003.JPG
  • Rays of light from the setting sun illuminate the ruins of Seneca Stone Cutting Mill.<br />
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Located on the banks of Seneca Creek and the Potomac River, Seneca Quarry provided Washington D.C. with a steady supply of sandstone that was both durable and beautiful for itís unique bright-crimson hue. This "Seneca redstone", finely cut and polished in this mill, is everywhere throughout the District, from the Smithsonian Castle, Cabin John Bridge, Arlington National Cemeteryís boundary wall and Luther Place Church in Thomas Circle to numerous houses throughout Dupont Circle and Adams Morgan. <br />
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Beginning in the 1870ís, The millís fortunes declined through financial mismanagement and flood damages. By the turn of the century the quality of the quarried stone had degraded significantly, and the victorian architecture that relied on material such as seneca redstone fell out of popularity. The Seneca quarry shut down operations for good in 1901, leaving the mill to crumble and decay.
    maryland018.JPG
  • Located 14 miles upstream from DC, Great Falls lies along the Atlantic Seaboard Fall Line where the Piedmont Plateau meets the Atlantic Coastal Plain. The series of cascades descend a total of 76 feet over less than a mile, making it the steepest fall line rapids of any river on the Eastern Seaboard. The falls themselves were created over thousands of years dating from the last ice age when the sea level dropped, resulting in the Potomac carving deep into the surrounding rock as it made its way to the Chesapeake.
    maryland009.JPG
  • Located 14 miles upstream from DC, Great Falls lies along the Atlantic Seaboard Fall Line where the Piedmont Plateau meets the Atlantic Coastal Plain. The series of cascades descend a total of 76 feet over less than a mile, making it the steepest fall line rapids of any river on the Eastern Seaboard. The falls themselves were created over thousands of years dating from the last ice age when the sea level dropped, resulting in the Potomac carving deep into the surrounding rock as it made its way to the Chesapeake.
    maryland008.JPG
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Craig Hudson Photography

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