Backcountry Camping Closures
Pope Bay, Green Run, Pine Tree & Tingles Island backcountry campsites will be closed on these dates due to hunting seasons: October 15-25, 2014; November 13-15, 2014; November 29-December 13, 2014; January 16-19, 2015 More »
Coasts / Shorelines
Barrier islands like Assateague are highly dynamic places, as currents and storms work to continuously reshape the land form. Though changing course periodically throughout the year, long shore currents continuously transport sand south along the coast. On a seasonal basis, harsh winter weather pulls sand from dunes and upper beaches, depositing it into offshore sand bars and reducing beach width. This process is reversed during milder summer weather, as gentler wave action acts to restore the shoreline.
Assateague is also moving westward as a result of sea-level rise and the force of the surf through a process called “island rollover.” During severe storm events, sand is eroded from the ocean beaches and carried across the island by flood waters and re-deposited in marshes along the western shore, steadily narrowing the bay that separates the island from the mainland. These events can break through dunes, spilling sand in fanlike deposits or even carving inlets, such as the one that has separated Assateague and Ocean City since 1933. Long shore currents will eventually deposit sediments and close these gaps unless, like the Ocean City inlet, it is maintained with jetties and dredging.
Did You Know?
Prickly pear cactus is native to dry, sandy areas on Assateague Island. American Indians applied peeled pads to wounds and drank pad tea for lung ailments. Fruits were eaten fresh or dried for winter use.