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Rehoboth Bay
Rehoboth Bay
	Rehoboth Bay in Delaware
	Rehoboth Bay
Location	Delaware
Coordinates	38°39′50.7″N 75°06′16.2″W / 38.664083°N 75.104500°W
Type	estuary
Primary inflows	White Oak Creek, Love Creek, Herring Creek, and Guinea Creek
Primary outflows	Atlantic Ocean
Basin countries	United States
Surface area	13 sq mi (34 km2)
Average depth	6 ft (1.8 m)
Settlements	Rehoboth Beach, Delaware and Long Neck, Delaware

Rehoboth Bay is a body of water in Sussex County, Delaware. It is connected to the Broadkill River by the Lewes and Rehoboth Canal. It is part of Delaware's inland bay system, along with Little Assawoman Bay and Indian River Bay.^[1]^[2]

Of Delaware's inland bays, both Rehoboth Bay and Little Assawoman Bay are barbuilt estuaries, while Indian River Bay is a drowned river valley.^[2] Rehoboth Bay is the northernmost of Delaware's inland bays. Its depth is generally shallow, less than 6 to 7 feet below Mean Lower Low Water. The surface area of the bay is approximately 13 square miles. Rehoboth Bay receives fresh water discharges from a number of small creeks along the bay, including White Oak Creek, Love Creek, Herring Creek, and Guinea Creek. Rehoboth Bay is linked to Indian River Bay to the south, providing tidal exchange with the Atlantic Ocean through Indian River Inlet, which is stabilized by two parallel stone jetties. At the north end of the Bay, the Lewes-Rehoboth Canal connects Rehoboth Bay to the Delaware Bay as part of the Intracoastal Waterway. Tidal flow provides some exchange of water between the Delaware Bay and Rehoboth Bay through the canal.^[3]

References

^ "About the Bays". Rehoboth Beach, DE: Delaware Center for the Inland Bays. Retrieved 2024-08-01.
^ ^a ^b Sediment Management Plan. Rehoboth Bay, Sussex County, Delaware (PDF) (Report). Dover, DE: Delaware Department of Natural Resources and Environmental Conservation. 7 November 2007.
^ Wong, Kuo-Chuin (1991). "The effect of coastal sea level forcing on Indian River Bay and Rehoboth Bay, Delaware". Estuarine, Coastal and Shelf Science. 32 (3). Elsevier BV: 213–229. doi:10.1016/0272-7714(91)90016-5. ISSN 0272-7714.