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Younger Lagoon Reserve

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Younger Lagoon Reserve is a 72-acre (28-hectare) University of California Natural Reserve System reserve on the northern shore of Monterey Bay in Santa Cruz County, California . The site is owned by the University of California and managed for teaching and research. It is adjacent to Long Marine Laboratory .

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27-466: The reserve encompasses a pocket beach, seasonal lagoon , wetlands, and coastal prairie on the western edge of the city of Santa Cruz . Other features include a sea stack , sea caves, and tidepools. Donald and Marion Younger, whose family had owned a ranch in the area for over a century, donated the reserve to the University of California in 1972 to enable development of Long Marine Laboratory and protect

54-465: A coastal stream when ocean waves eroded the sea caves beneath the coastal bluffs. The Y-shaped lagoon is seasonal, filling with winter and spring rains until winter storms erode the sandy berm at its mouth. At this point, the entire lagoon drains over the course of a few hours. Ocean waters fill the lagoon until waves reform the berm, enabling rain and runoff to freshen the waters again. The federally endangered tidewater goby ( Eucyclogobius newberryi )

81-523: A lake is hu ( 湖 ), and a lagoon is xihu ( 潟湖 ). In the French Mediterranean several lagoons are called étang ("lake"). Contrariwise, several other languages have specific words for such bodies of water. In Spanish, coastal lagoons generically are laguna costera , but those on the Mediterranean coast are specifically called albufera . In Russian and Ukrainian, those on

108-422: A regular flow of fresh water an "estuary". Davis does state that the terms "lagoon" and "estuary" are "often loosely applied, even in scientific literature". Timothy M. Kusky characterizes lagoons as normally being elongated parallel to the coast, while estuaries are usually drowned river valleys, elongated perpendicular to the coast. Coastal lagoons are classified as inland bodies of water. When used within

135-521: Is a shallow body of water separated from a larger body of water by a narrow landform , such as reefs , barrier islands , barrier peninsulas, or isthmuses . Lagoons are commonly divided into coastal lagoons (or barrier lagoons ) and atoll lagoons . They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries . Lagoons are common coastal features around many parts of

162-453: Is actually the third-largest lake by area in the country. The brackish water lagoon may be thus explicitly identified as a "coastal lagoon" ( laguna costera ). In Portuguese, a similar usage is found: lagoa may be a body of shallow seawater, or a small freshwater lake not linked to the sea. Lagoon is derived from the Italian laguna , which refers to the waters around Venice ,

189-494: Is also noted for its duck and goose hunting. 36°17′01″N 75°52′14″W  /  36.28361°N 75.87056°W  / 36.28361; -75.87056 This article about a location in Currituck County , North Carolina is a stub . You can help Misplaced Pages by expanding it . This City of Virginia Beach, Virginia state location article is a stub . You can help Misplaced Pages by expanding it . This article about

216-844: Is separated from the Atlantic Ocean by the Currituck Banks Peninsula (formerly Bodie Island ), part of the Outer Banks . On the northeast, it extends to Back Bay in northeast Virginia Beach, Virginia . A fork on the northwest leads to the Albemarle and Chesapeake Canal , which is a part of the Atlantic Intracoastal Waterway that connects the sound to Hampton Roads and the Chesapeake Bay . It ranges from 1 to 3 feet deep. Although several inlets connected it directly to

243-533: Is the major force that moves water. Currituck County 's Mackay Island and Currituck National Wildlife Refuge as well as Back Bay National Wildlife Refuge and False Cape State Park in Virginia Beach border the sound and are winter habitats on the Atlantic Flyway . Many watersports activities occur in the sound, including parasailing , sea kayaking , and jet skiing . An area of barrier beaches , it

270-403: Is the most abundant fish species in the lagoon. Surrounding terrestrial habitats feature willow thickets, dune plants, and pickleweed marsh. Common animals range from brush rabbits and striped skunks to coyote and bobcat . Shorebirds such as willets and sanderlings forage on the beach. Younger Lagoon deploys interns and students to restore native vegetation around the lagoon and along

297-612: The Black Sea are liman ( лиман ), while the generic word is laguna ( Лагуна ). Similarly, in the Baltic , Danish has the specific Nor  [ da ] , and German the specifics Bodden and Haff , as well as generic terms derived from laguna . In Poland these lagoons are called zalew ("bay"), in Lithuania marios ("lagoon, reservoir"). In Jutland several lagoons are known as fjord . In New Zealand

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324-523: The Māori word hapua refers to a coastal lagoon formed at the mouth of a braided river where there are mixed sand and gravel beaches, while waituna , an ephemeral coastal waterbody, is neither a true lagoon, lake nor estuary. Some languages differentiate between coastal and atoll lagoons. In French, lagon  [ fr ] refers specifically to an atoll lagoon, while coastal lagoons are described as étang  [ fr ] ,

351-592: The Venetian Lagoon . Laguna is attested in English by at least 1612, and had been Anglicized to "lagune" by 1673. In 1697 William Dampier referred to a "Lagune or Lake of Salt water" on the coast of Mexico. Captain James Cook described an island "of Oval form with a Lagoon in the middle" in 1769. Atoll lagoons form as coral reefs grow upwards while the islands that the reefs surround subside, until eventually only

378-452: The Wadden Sea , have strong tidal currents and mixing. Coastal lagoons tend to accumulate sediments from inflowing rivers, from runoff from the shores of the lagoon, and from sediment carried into the lagoon through inlets by the tide. Large quantities of sediment may be occasionally be deposited in a lagoon when storm waves overwash barrier islands. Mangroves and marsh plants can facilitate

405-723: The Atlantic at one time or another, they have all since closed and there is now no direct access to the Ocean from the Sound. Thus contemporary salinity levels are very low, usually around 2-3 ‰ at the north end and 4-5‰ at the sound. Currently, the only access to the ocean is through the Albemarle Sound , which joins the Currituck to the South, meaning that the sound has no lunar or solar tides. Instead, wind

432-534: The International Drought Experiment. Published work from the reserve indicates that certain traits such as slow growth rates and high leaf lobedness can decrease mortality risk when plants experience drought. Studies at the International Drought Experiment plots also indicate that nonperiodic restoration activities, such as one-off planting or weeding events, can facilitate coyote bush invasion in restored coastal grasslands. Lagoon A lagoon

459-402: The accumulation of sediment in a lagoon. Benthic organisms may stabilize or destabilize sediments. Currituck Sound Currituck Sound ( / ˈ k ʊr ɪ t ʌ k / ) is a lagoon located in northeastern part of North Carolina and extreme southeastern Virginia . 36 miles (58 km) long north-south and 8 miles (13 km) at its widest, this shallow, island-filled sound

486-431: The coastal prairie. Their experiments revegetating bluffs covered with non-native iceplant and remnants of brussels sprout fields inform research on habitat restoration. Cape Ivy has spread throughout some areas. Other experiments include understanding the effects of extreme drought on coastal prairie restoration across time. These studies were set up in collaboration with a global network of drought researchers called

513-614: The context of a distinctive portion of coral reef ecosystems, the term "lagoon" is synonymous with the term "back reef" or "backreef", which is more commonly used by coral reef scientists to refer to the same area. Many lagoons do not include "lagoon" in their common names. Currituck , Albemarle and Pamlico Sounds in North Carolina , Great South Bay between Long Island and the barrier beaches of Fire Island in New York , Isle of Wight Bay , which separates Ocean City, Maryland from

540-583: The generic word for a still lake or pond. In Vietnamese, Đầm san hô refers to an atoll lagoon, whilst Đầm phá is coastal. In Latin America, the term laguna in Spanish, which lagoon translates to, may be used for a small fresh water lake in a similar way a creek is considered a small river. However, sometimes it is popularly used to describe a full-sized lake , such as Laguna Catemaco in Mexico, which

567-611: The lagoon. Lagoons with little or no interchange with the open ocean, little or no inflow of fresh water, and high evaporation rates, such as Lake St. Lucia , in South Africa , may become highly saline. Lagoons with no connection to the open ocean and significant inflow of fresh water, such as the Lake Worth Lagoon in Florida in the middle of the 19th century, may be entirely fresh. On the other hand, lagoons with many wide inlets, such as

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594-525: The lagoon. The reserve was made part of the UC Natural Reserve System in 1987. The university added 47 acres of adjacent farm fields, an area known as Terrace Point, to the 25-acre reserve in 2008 as part of the establishment of its Coastal Science Campus. The reserve sits on the lowest and southernmost of the series of marine terraces that make up the Santa Cruz coastline. The lagoon was formed by

621-556: The land along the coast). Coastal lagoons do not form along steep or rocky coasts, or if the range of tides is more than 4 metres (13 ft). Due to the gentle slope of the coast, coastal lagoons are shallow. A relative drop in sea level may leave a lagoon largely dry, while a rise in sea level may let the sea breach or destroy barrier islands, and leave reefs too deep underwater to protect the lagoon. Coastal lagoons are young and dynamic, and may be short-lived in geological terms. Coastal lagoons are common, occurring along nearly 15 percent of

648-407: The reefs remain above sea level. Unlike the lagoons that form shoreward of fringing reefs, atoll lagoons often contain some deep (>20 m (66 ft)) portions. Coastal lagoons form along gently sloping coasts where barrier islands or reefs can develop offshore, and the sea-level is rising relative to the land along the shore (either because of an intrinsic rise in sea-level, or subsidence of

675-606: The rest of Worcester County, Maryland , Banana River in Florida , US, Lake Illawarra in New South Wales , Australia, Montrose Basin in Scotland , and Broad Water in Wales have all been classified as lagoons, despite their names. In England, The Fleet at Chesil Beach has also been described as a lagoon. In some languages the word for a lagoon is simply a type of lake: In Chinese

702-510: The world's shorelines. In the United States, lagoons are found along more than 75 percent of the Eastern and Gulf Coasts . Coastal lagoons can be classified as leaky, restricted, or choked. Coastal lagoons are usually connected to the open ocean by inlets between barrier islands. The number and size of the inlets, precipitation, evaporation, and inflow of fresh water all affect the nature of

729-582: The world. Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal , coral reef , or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity . The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis Jr. restricts "lagoon" to bodies of water with little or no fresh water inflow, and little or no tidal flow, and calls any bay that receives

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