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Little Assawoman Bay
Little Assawoman Bay is a body of water in Sussex County, Delaware, Sussex County, Delaware. It is connected from Assawoman Bay to the south by a narrow canal known locally as "The Ditch," and is connected to Indian River Bay to the north by the Assawoman Canal. It is separated from the Atlantic Ocean by the Fenwick Island (Delaware–Maryland), Fenwick Island barrier spit. References Bays of Delaware Bays of Sussex County, Delaware {{Delaware-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Assawoman Bay DE1
Little is a synonym for small size and may refer to: Arts and entertainment *Little (album), ''Little'' (album), 1990 debut album of Vic Chesnutt *Little (film), ''Little'' (film), 2019 American comedy film *The Littles, a series of children's novels by American author John Peterson **The Littles (TV series), ''The Littles'' (TV series), an American animated series based on the novels Places *Little, Kentucky, United States *Little, West Virginia, United States Other uses *Clan Little, a Scottish clan *Little (surname), an English surname *Little (automobile), an American automobile manufactured from 1912 to 1915 *Little, Brown and Company, an American publishing company *USS Little, USS ''Little'', multiple United States Navy ships See also * * *Little Mountain (other) *Little River (other) *Little Island (other) {{disambiguation, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sussex County, Delaware
Sussex County is located in the southern part of the U.S. state of Delaware, on the Delmarva Peninsula. As of the 2020 census, the population was 237,378. The county seat is Georgetown. The first European settlement in the state of Delaware was founded by the Dutch in 1631 near the present-day town of Lewes on the Atlantic Coast. However, Sussex County was not organized until 1683 under English colonial rule. Sussex County is included in the Salisbury, MD-DE Metropolitan Statistical Area which encompasses much of central Delmarva. History Beginnings Archaeologists estimate that the first inhabitants of Sussex County, the southernmost county in Delaware, arrived between 10,000 and 14,000 years ago. Various indigenous cultures occupied the area, especially along the river and the coast, often having seasonal fishing villages. Historic Native Americans in Sussex County were members of Algonquian-speaking tribes, as were most coastal peoples along the Atlantic Coast. By the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Delaware
Delaware ( ) is a state in the Mid-Atlantic region of the United States, bordering Maryland to its south and west; Pennsylvania to its north; and New Jersey and the Atlantic Ocean to its east. The state takes its name from the adjacent Delaware Bay, in turn named after Thomas West, 3rd Baron De La Warr, an English nobleman and Virginia's first colonial governor. Delaware occupies the northeastern portion of the Delmarva Peninsula and some islands and territory within the Delaware River. It is the second-smallest and sixth-least populous state, but also the sixth-most densely populated. Delaware's largest city is Wilmington, while the state capital is Dover, the second-largest city in the state. The state is divided into three counties, having the lowest number of counties of any state; from north to south, they are New Castle County, Kent County, and Sussex County. While the southern two counties have historically been predominantly agricultural, New Castle is more ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assawoman Bay
Assawoman Bay (), once called Assawoman Sound, is a lagoon that is located between Ocean City, Maryland and mainland Delmarva. The bay is located on the northern end of the city, the bay on the southern end is called the Isle of Wight Bay. Another bay called Little Assawoman Bay extends into southern Delaware, and is geologically separated from the main estuaries, by a narrow strait locally referred to as "The Ditch" which crosses the Transpeninsular Line. The larger bay is sometimes called "Big Assawoman Bay", to distinguish it from the smaller bay, though this is often meant to be a tongue-in-cheek The idiom tongue-in-cheek refers to a humorous or sarcastic statement expressed in a serious manner. History The phrase originally expressed contempt, but by 1842 had acquired its modern meaning. Early users of the phrase include Sir Walter Scott ... rendering of the name. External linksAssawoman Bay watershed profile delawarewatersheds.org Bays of Delaware Bays of Maryland B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indian River Bay
Indian River Bay is a body of water in Sussex County, Delaware. It is part of Delaware's inland bay system, along with Little Assawoman Bay and Rehoboth Bay. Fed by the Indian River at its western end, the bay is connected to the Atlantic Ocean to the east via the Indian River Inlet. A natural waterway that shifted up and down a two-mile (3.2 km) stretch of the coast until 1928, the inlet was kept in its current location by dredging between 1928 and 1937, and in 1938 was fixed in place by the construction of jetties. The Charles W. Cullen Bridge, commonly known as the Indian River Inlet Bridge, spans the inlet. Indian River Bay is unique among Delaware's inland bays in that it is a drowned river valley, whereas Delaware's other bays are estuaries built on sand bars.Delaware Inland Bays Compreh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assawoman Canal
The Assawoman Canal is a canal in Sussex County, Delaware. The canal links the Indian River Bay to the north with the Little Assawoman Bay to the south. It is bordered by Bethany Beach and South Bethany to the east and Ocean View to the west. Because of it, Fenwick Island is detached from the Delaware mainland. First proposed in 1884, the Assawoman Canal was constructed by the U.S. Army Corps of Engineers in 1891 for the purpose of moving goods by boat without having to travel into the Atlantic Ocean. The canal was initially dug by hand in the 1890s by immigrant labor. The canal was not dredged from the 1950s until 2006. By the early 2000s, it was no longer deep enough to handle the boat traffic that once passed through it when it was part of the Intracoastal Waterway The Intracoastal Waterway (ICW) is a inland waterway along the Atlantic and Gulf of Mexico coasts of the United States, running from Massachusetts southward along the Atlantic Seaboard and around the south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fenwick Island (Delaware–Maryland)
Fenwick Island is a barrier island along the Atlantic Ocean in Delaware and Maryland in the United States. It contains the communities of South Bethany and Fenwick Island in Delaware along with Ocean City, Maryland. Until 1933, it was attached to Assateague Island to the south. That year, a hurricane carved an inlet between the two landforms, which was made permanent. If not for the Assawoman Canal, constructed by the U.S. Army Corps of Engineers , colors = , anniversaries = 16 June (Organization Day) , battles = , battles_label = Wars , website = , commander1 = ... in 1891, the island would be attached to the mainland of Delaware. References Barrier islands of Delaware Barrier islands of Maryland Landforms of Sussex County, Delaware Landforms of Worcester County, Maryland Spits of the United States Islands of Maryland {{Worcest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barrier Spit
A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sediment in the direction the waves are breaking, forming an above-water spit. Without the co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bays Of Delaware
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace".Maurice Schwartz, ''Encyclopedia of Coastal Science'' (2006), p. 129. Bays were sig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
