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41-523: The lake is connected to the Gulf of Venezuela to the north by a narrow spit . It is fed by numerous rivers, the biggest being the Catatumbo River . The fault in the northern section has collapsed and is rich in oil and gas resources. It is Venezuela's main oil producing area and an important fishing and agricultural producing area. Eutrophication caused by oil pollution is a major environmental problem facing

82-503: A five kilometer thick deposit of sediment on the bedrock. In the Pliocene , the depression of today's Lake Maracaibo reached what would be practically its current form. The numerous rivers that flow into the lake have been defining its banks, especially those that form the southern delta of the lake, where the Escalante , Catatumbo and Santa Ana rivers converge. Lake Maracaibo is located in

123-481: A hook or recurved spit. Refraction in multiple directions may create a complex spit. Waves that arrive in a direction other than obliquely along the spit will halt the growth of the spit, shorten it, or eventually destroy it entirely. The sediments that make up spits come from a variety of sources including rivers and eroding bluffs, and changes there can have a major effect on spits and other coastal landforms. Activities such as logging and farming upstream can increase

164-412: A river) becomes too great to allow the sand to deposit. Vegetation may then start to grow on the spit, and the spit may become stable and often fertile. A spit may be considered a special form of a shoal . As spits grow, the water behind them is sheltered from wind and waves, and a salt marsh is likely to develop. Wave refraction can occur at the end of a spit, carrying sediment around the end to form

205-544: Is 28 °C, the precipitation is more in the south and less in the north, and the average annual rainfall in the south is 1400 mm. The mountain wind from the Andes at night contacts the warm and humid air on the lake surface, forming an average of 297 mm per year. The meteorological phenomenon known as Catatumbo lightning takes place in southern part of the lake, characterized by a continuous series of lightnings that are almost continuous and silent. This makes Lake Maracaibo

246-742: Is called the proximal end, and the end jutting out into water is called the distal end. There is debate as to the longest spit in the world, with both the Arabat Spit in the Sea of Azov and the Younghusband Peninsula in South Australia approximately 110 kilometres (68 mi) long. Alternatively, with the natural closing of the Roanoke inlet in 1811, Bodie Island in North Carolina may qualify as

287-417: Is deep in the south and shallow in the north. The northern half of the lake, which looks like a bottleneck, is 55 kilometers long. The southeastern edge of the lake basin with a flat bottom is steep and the northwestern edge is gentle. The southern part is lighter due to river water injection, while the northern part is slightly salty due to tidal influence. The Catatumbo River forms a bird-foot-shaped delta in

328-643: Is geographically a peninsula), while others like Toad have tectonic origins. The majority of the islands are located in the area of the Tablazo Bay and forms the Almirante Padilla municipality  [ es ] . The islands of Burro, Providencia, Hijacal, Pájaros, and the artificial islands are located at the neck of the lake and belong to other municipalities. Natural islands of Lake Maracaibo: Artificial islands of Lake Maracaibo: The 8,678 metres (28,471 ft) long General Rafael Urdaneta Bridge connects

369-788: The Curonian Lagoon from the Baltic Sea ; it is 98 km long (61 mi). In a similar fashion, the Vistula Spit separates the Vistula Lagoon from the Gdańsk Bay off the coast of Poland . Zlatni Rat , a popular pebble beach jutting southward from the harbor town of Bol , on the Croatian island of Brač , is formed by Adriatic currents flowing east and west through the Hvar Channel , along

410-641: The Maracaibo lowland in the faulted basin between the Perija Mountains and the Merida Mountains of the Eastern Cordillera Mountains in northwestern Venezuela. The lake is in the shape of a vase. It is 210 kilometers long from north to south, 121 kilometers wide from east to west, covers an area of 13,512 square kilometers, the deepest is 35 meters, the shore length is about 1000 kilometers, and

451-1086: The Morro Bay is one such location. Pueblo a%C3%B1%C3%BA Look for Pueblo añú on one of Misplaced Pages's sister projects : [REDACTED] Wiktionary (dictionary) [REDACTED] Wikibooks (textbooks) [REDACTED] Wikiquote (quotations) [REDACTED] Wikisource (library) [REDACTED] Wikiversity (learning resources) [REDACTED] Commons (media) [REDACTED] Wikivoyage (travel guide) [REDACTED] Wikinews (news source) [REDACTED] Wikidata (linked database) [REDACTED] Wikispecies (species directory) Misplaced Pages does not have an article with this exact name. Please search for Pueblo añú in Misplaced Pages to check for alternative titles or spellings. You need to log in or create an account and be autoconfirmed to create new articles. Alternatively, you can use

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492-810: The West Indian manatee and the Amazon river dolphin . About 145 species of fish inhabit the lake, including many endemic species such as the Maracaibo half-hooked catfish ( Hypostomus maracaiboensis ), the Maracaibo hairy catfish ( Trichomycterus maracaiboensis ), the Maracaibo Lake Lamont catfish ( Lamontichthys maracaibero ), Lake Maracaibo tetra ( Bryconamericus motatanensis ), and Maracaibo wolf anchovies ( Lycengraulis limnichthys ) living in surface waters. The lake has been drilled about 14,000 times, and more than 15,000 miles of oil and gas pipelines criss-cross

533-465: The article wizard to submit a draft for review, or request a new article . Search for " Pueblo añú " in existing articles. Look for pages within Misplaced Pages that link to this title . Other reasons this message may be displayed: If a page was recently created here, it may not be visible yet because of a delay in updating the database; wait a few minutes or try the purge function . Titles on Misplaced Pages are case sensitive except for

574-539: The Catatumbo River are the main traffic lines for the transportation of commodities in the nearby area, and the city of Maracaibo is the transshipment center of coffee produced in the Andes. The waterway can pass through large sea-going ships and oil tankers, exporting crude oil and agricultural and livestock products from the Andean mountains and lakes. The Lake District is home to a quarter of Venezuela's population, and with

615-667: The banks of the lake refer to it as Coquivacoa. The tribes of Wayuu , Caquetíos , and Quiriquires also lived in the area. When Italian navigator Amerigo Vespucci and Spanish explorer Alonso de Ojeda 's fleet sailed here on August 24, 1499 (the first time Europeans entered this area), the stilt houses in which the Añú lived in reminded Vespucci of the Italian city of Venice , so he named the region Veneziola ( Venezuela in Spanish), or "Little Venice". Spain made two attempts to establish settlements around

656-455: The bottom of the lake to float to the surface of the lake, which in turn allowed the duckweed to rapidly multiply and triggered a bloom that lasted for up to eight months. The blooms were noted in June to have covered 18% of the lake, and the local government had to begin spending about $ 2 million per month on cleanup work. Numerous oil spills , at least partly attributed to deficient maintenance, and

697-406: The city of Maracaibo, the lake water is contaminated with E. coli from feces, oil pollution, and eutrophication caused by agricultural sewage discharged into the lake, as well as domestic and industrial wastewater, resulting in the blooms of duckweed and green algae . The presence of large amounts of duckweed blocks the passage of sunlight, significantly affecting biological cycles, preventing

738-497: The development of native algae and plant species. Additionally, duckweed residues accumulate at the bottom, generating a layer of organic elements that produces large amounts of ammonium, methane and other compounds whose saturation causes eutrophication of the waters. In the spring of 2004, heavy rains fell in the Lake Maracaibo basin, causing a large influx of fresh water into the lake. This caused nutrients originally deposited on

779-417: The direction the waves are breaking, forming an above-water spit. Without the complementary process of littoral drift, the bar would not build above the surface of the waves becoming a spit and would instead be leveled off underwater. Spits occur when longshore drift reaches a section of headland where the turn is greater than 30 degrees. The spit will continue out into the sea until water pressure (e.g. from

820-458: The indiscriminate discharge of sewage without prior treatment, have significantly deteriorated the water quality, to the point that in some parts of the Zulia area, the water presents levels of contamination that are very dangerous for health. Within the existing polluting activities, the mining of mineral coal has started more recently, which further contaminates the basin with pollutants. Likewise,

861-462: The influx of farmers from the nearby Andes, the population of the Lake District increased from about 300,000 in 1936 to over 3.62 million in 2007. Lake Maracaibo possesses highly oxygenated waters which makes it rich in algae, and in turn fish, making it very biologically diverse. It is home to clams, blue crabs , shrimp and other aquatic products, and is also home to two endangered aquatic mammals,

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902-422: The lagoon. The area around the lagoon is inhabited by a quarter of the country's population and is also the place with the most frequent lightning on Earth. The famous Catatumbo lightning can illuminate nighttime navigation. Lake Maracaibo is located within the eponymous basin and is one of the oldest lakes on earth. It was formed 36 million years ago when the faults collapsed when the Andes were uplifted in

943-404: The lake connecting Maracaibo and Santa Rita was completed in 1962. Lake Maracaibo is rich in oil and gas resources and is known as the "oil lake". The first Spaniards who arrived used tar seeping from the lake to fill ship cracks. The Maracaibo oil field was discovered in 1914, the first oil well was constructed in 1917, and large-scale exploitation began in 1922. The oil fields are concentrated in

984-434: The lake floor, but most of these pipelines are half a century old, with oil leaking from many aging underwater pipes. Before the 1950s, the lake water could still be used directly for domestic use, but then due to the intrusion of tidal salt water caused by the widening of the lake mouth channel, the salinity of the northern lake area increased by about 1,000%, and the south also increased by 300–500%. In lakeside towns such as

1025-506: The lake in 1529 and 1569, but it was not until 1574 that the city of Maracaibo was successfully established. The Privateer Henry Morgan raided settlements on the lake in the Spring of 1669 and defeated a Spanish squadron sent to intercept him. On July 24, 1823, Venezuela won the famous Battle of Lake Maracaibo on the lake during the Venezuelan War of Independence . The original depth of

1066-407: The lake mouth, which was only more than 4 meters deep, was increased to 8 meters after dredging in the 1930s, and the 3-kilometer-long stone breakwater was further increased to 11 meters after its completion in 1957, allowing ocean-going tankers to enter the lake, At the same time, the northern part, which was originally fresh water, became brackish. The 8,678-meter General Rafael Urdaneta Bridge over

1107-472: The late Eocene . In the geological history, sea water and fresh water have alternated many times, and have flooded the area. At the end of the last glacial period , the sea level rose, connecting Lake Maracaibo directly with the Atlantic Ocean , and the lighter fresh water floated on the heavier salt water, causing nutrients to be deposited on the bottom of the lake, resulting in the accumulation of more than

1148-508: The longest, also measuring in at approximately 70 miles (110 km) to the peninsula's terminus at the Oregon Inlet . The longest spit in a freshwater body of water is Long Point, Ontario , which extends approximately 32 km (20 mi) into Lake Erie . Farewell Spit in New Zealand , at 32 km (20 mi), in the north-west area of South Island , is believed to be caused by

1189-482: The northeast and northwest of the lake, and the oil-producing layers are mainly Tertiary sandstone and Cretaceous limestone, with a hydrocarbon-bearing area of 1,300 square kilometers, mainly concentrated in the coastal waters 105 kilometers long and 32 kilometers wide in the east of the lake. On the northwest coast is the capital of Zulia State , the second largest city in Venezuela and an important oil export port in

1230-536: The place with the most frequent lightning on Earth. There are about 233 lightning strikes per square kilometer in a year on average. The nocturnal thunderstorms occur on average about 297 days per year. At its peak in September, the lake area can experience up to 280 lightning strikes per hour, approximately 28 lightning strikes per minute, lasting up to 9 hours, and is capable of illuminating nighttime navigation. The aboriginal Añú  [ es ] people who lived on

1271-437: The sediment load of rivers, which may hurt the intertidal environments around spits by smothering delicate habitats. Roads or bulkheads built along bluffs can drastically reduce the volume of sediment eroded, so that not enough material is being pushed along to maintain the spit. If the supply of sediment is interrupted the sand at the neck (landward end) of the spit may be moved towards the head, eventually creating an island. If

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1312-494: The so-called cañadas , which are random drainage courses, drag large amounts of garbage from the human settlements that are in their path to the lake. In addition to this, residential waste such as plastic bags and bottles are also added. These pollutants all eventually get carried into the lake. There are many islands in the lake. Some primarily consist of sedimentary rock , such as the Zapara, Pescadores, and San Carlos islands (which

1353-469: The southern side of the island. The spit bends slightly west or east, changing its direction gradually, depending on the conditions of the tides and weather. Since prehistory humans have chosen certain spit formations as sites for human habitation. In some cases, these sites have been chosen for proximity to marine resource exploitation ; the Chumash Native American prehistorical settlement on

1394-457: The southwest of the lake basin, and the surface lake water in the delta has a salinity of only 0.13%. However, the intrusion of seawater from the mouth of the lake makes the salinity of the bottom lake water higher, reaching 0.2–0.3%. The north is connected with the Gulf of Venezuela , and the spit at the mouth of the lake extends for about 26 kilometers. The annual average temperature of the lake area

1435-704: The strong prevailing winds and currents, bringing sand eroded from the Southern Alps of the South Island and depositing these into Golden Bay . A well-known spit in the UK is Spurn Point at the Humber ; it is approximately 4.8 km (3.0 mi) long. Another is Chesil Beach in the UK, which connects the Isle of Portland to the mainland. The Curonian Spit , off the coast of Lithuania and Kaliningrad Oblast of Russia , separates

1476-412: The supply is not interrupted, and the spit is not breached by the sea (or, if across an estuary, the river), the spit may become a bar , with both ends joined to land, and form a lagoon behind the bar. If an island lies offshore near where the coast changes direction, and the spit continues to grow until it connects the island to the mainland, it is called a tombolo . The end of a spit attached to land

1517-491: The volume is about 280 cubic kilometers. The largest river entering the lake, the Catatumbo River , enters the lake from west to east, providing 57% of the water entering the lake. In addition to the influence of the prevailing wind, the lake water circulates counterclockwise. There are also the Santa Ana River, Chama River , Motatán River , Escalante River , and about fifty other rivers which drain into it. Lake Maracaibo

1558-462: The water alongside the beach. These currents are caused by the same waves that cause the drift. 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

1599-489: The western and eastern coast of the lake together. It held the record for being the longest cable-stayed concrete bridge in the world at the time of its inauguration in 1962. Located in the southern part of the Strait of Maracaibo, it is a vehicles-only bridge that accommodates both directions of traffic, while its height allows for the passage of vessels up to 45 meters in height. Spit (landform) A spit ( cognate with

1640-467: The word for a rotisserie bar) 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

1681-413: The world. The lake area is also an important fishing and agricultural production area in Venezuela, supporting more than 20,000 fishermen, many of whom live in colorful traditional stilt houses built with iron sheets on the lake. The main crops on the south bank of the lake are bananas, peanuts, cocoa, coconut, sugar cane and coffee, the western shore of the lake developed dairy industry. Lake Maracaibo and

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