Santurtzi is a port town in the province of Biscay, in the autonomous community of Basque Country, Spain. It is located in the Bilbao Abra bay, near the mouth of the Nervión river, on its left bank, 14 km downriver from Bilbao and forms part of the Greater Bilbao agglomeration, it has a population of 47,320 and a land area of 6.77 km². The district of Santurce of the city of San Juan, Puerto Rico derives its name from Santurtzi. Santurce has a rough orography although excluding Mount Serantes - one of its most symbolic topographic elements, it is not at high altitude, the significant heights being spurs of the Serantes: The Mallet and the Fortified heights, its relief is within the north flank of the anticline of Biscay. It is a relief of a structural type corresponding to a series of materials of the Cretaceous period throughout Punta Lucero-Serantes smoothly inclined towards the Estuary of Bilbao; the climate in Santurce is of the humid oceanic climate type. The temperatures are moderate throughout the year, with more frequent rains in spring and autumn, winters are benign and summers not excessively warm.
The average temperature is 8 °C in winter. The beauty of the landscape and the quality of the gastronomy along with the hospitality of the Santurtziarrak are some of the attractions which the visitor can enjoy. Santurce is a marine town that has succeeded in conserving many of its traditions, in spite of its great growth; the life in this area is focused on the sea, which inspires its leisure. Fishing boat and rowing boat races, the celebrations of the Virgin of the Carmen keep their traditions alive. Gastronomy is based on fish sardines. Easter Monday - Pascua - Cornites April 23, San Jorge June 24, San Juan, San Juan neighbourhood June 29, San Pedro July 16, Virgen del Carmen September 8, Virgen del Mar San Jorge church House Toasts Town Hall Monument to Cristóbal Murrieta Patronato Santa Eulalia Home and clinical San Juan de Dios Oriol Palace Science of navigation school and Hijas de la Cruz college Virgen del Mar church Fishermen Confraternity Town Park and Central Kiosk Mamariga fountain Monument to the Sardinera Fishing Port and Virgin of Carmen Museum of Sculptures Monument to Miguel de Unamuno Señorío de Vizcaya Square Official website Santurce-Santurtzi in the Bernardo Estornés Lasa - Auñamendi Encyclopedia
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 called a gulf, sound, or bight. A cove is a type of smaller bay with narrow entrance. A fjord is a steep bay shaped by glacial activity. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may be nested within each other; some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay reduces the strength of winds and blocks waves. Bays were significant in the history of human settlement because they provided safe places for fishing, they were important in the development of sea trade as the safe anchorage they provide encouraged their selection as ports. The United Nations Convention on the Law of the Sea called the Law of the Sea, defines a bay as a well-marked indentation whose penetration is in such proportion to the width of its mouth as to contain land-locked waters and constitute more than a mere curvature of the coast.
An indentation shall not, however, be regarded as a bay unless its area is as large as, or larger than, that of the semi-circle whose diameter is a line drawn across the mouth of that indentation. There are various ways; the largest bays have developed through plate tectonics. As the super-continent Pangaea broke up along curved and indented fault lines, the continents moved apart and left large bays. Bays form through coastal erosion by rivers and glaciers. A bay formed by a glacier is a fjord. Rias are characterised by more gradual slopes. Deposits of softer rocks erode more forming bays, while harder rocks erode less leaving headlands. Bay platform Great capes Headlands and bays
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are made from rock, such as sand, shingle, pebbles; the particles can be biological in origin, such as mollusc shells or coralline algae. Some beaches have man-made infrastructure, such as lifeguard posts, changing rooms, showers and bars, they may have hospitality venues nearby. Wild beaches known as undeveloped or undiscovered beaches, are not developed in this manner. Wild beaches can be preserved nature. Beaches occur in areas along the coast where wave or current action deposits and reworks sediments. Although the seashore is most associated with the word beach, beaches are found by lakes and alongside large rivers. Beach may refer to: small systems where rock material moves onshore, offshore, or alongshore by the forces of waves and currents; the former are described in detail below. There are several conspicuous parts to a beach that relate to the processes that shape it; the part above water, more or less influenced by the waves at some point in the tide, is termed the beach berm.
The berm is the deposit of material comprising the active shoreline. The berm has a crest and a face—the latter being the slope leading down towards the water from the crest. At the bottom of the face, there may be a trough, further seaward one or more long shore bars: raised, underwater embankments formed where the waves first start to break; the sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests resulting from large storm waves and beyond the influence of the normal waves. At some point the influence of the waves on the material comprising the beach stops, if the particles are small enough, winds shape the feature. Where wind is the force distributing the grains inland, the deposit behind the beach becomes a dune; these geomorphic features compose. The beach profile changes seasonally due to the change in wave energy experienced during summer and winter months. In temperate areas where summer is characterised by calmer seas and longer periods between breaking wave crests, the beach profile is higher in summer.
The gentle wave action during this season tends to transport sediment up the beach towards the berm where it is deposited and remains while the water recedes. Onshore winds carry it further inland enhancing dunes. Conversely, the beach profile is lower in the storm season due to the increased wave energy, the shorter periods between breaking wave crests. Higher energy waves breaking in quick succession tend to mobilise sediment from the shallows, keeping it in suspension where it is prone to be carried along the beach by longshore currents, or carried out to sea to form longshore bars if the longshore current meets an outflow from a river or flooding stream; the removal of sediment from the beach berm and dune thus decreases the beach profile. In tropical areas, the storm season tends to be during the summer months, with calmer weather associated with the winter season. If storms coincide with unusually high tides, or with a freak wave event such as a tidal surge or tsunami which causes significant coastal flooding, substantial quantities of material may be eroded from the coastal plain or dunes behind the berm by receding water.
This flow may alter the shape of the coastline, enlarge the mouths of rivers and create new deltas at the mouths of streams that had not been powerful enough to overcome longshore movement of sediment. The line between beach and dune is difficult to define in the field. Over any significant period of time, sediment is always being exchanged between them; the drift line is one potential demarcation. This would be the point at which significant wind movement of sand could occur, since the normal waves do not wet the sand beyond this area. However, the drift line is to move inland under assault by storm waves; the development of the beach as a popular leisure resort from the mid-19th century was the first manifestation of what is now the global tourist industry. The first seaside resorts were opened in the 18th century for the aristocracy, who began to frequent the seaside as well as the fashionable spa towns, for recreation and health. One of the earliest such seaside resorts, was Scarborough in Yorkshire during the 1720s.
The first rolling bathing machines were introduced by 1735. The opening of the resort in Brighton and its reception of royal patronage from King George IV, extended the seaside as a resort for health and pleasure to the much larger London market, the beach became a centre for upper-class pleasure and frivolity; this trend was praised and artistically elevated by the new romantic ideal of the picturesque landscape. Queen Victoria's long-standing patronage of the Isle of Wight and Ramsgate in Kent ensured that a seaside residence was considered as a fashionable possession for those wealthy enough to afford more than one home; the extension of this form of leisure to the middle and working classes began with the development of the railways in the 1840s, which offered cheap fares to fast
Bay of Biscay
The Bay of Biscay is a gulf of the northeast Atlantic Ocean located south of the Celtic Sea. It lies along the western coast of France from Point Penmarc'h to the Spanish border, the northern coast of Spain west to Cape Ortegal; the south area of the Bay of Biscay washes over the northern coast of Spain and is known as the Cantabrian Sea. The average depth is 1,744 metres and the greatest depth is 4,735 metres; the Bay of Biscay is named after Biscay on the northern Spanish coast standing for the western Basque districts. Its name in other languages is: Asturian: golfu de Biscaya Basque: Bizkaiko golkoa Breton: pleg-mor Gwaskogn French: golfe de Gascogne Galician: golfo de Biscaia Gascon and Occitan: golf de Gasconha Latin: Sinus Biscaiensis Spanish: Golfo de Vizcaya Parts of the continental shelf extend far into the bay, resulting in shallow waters in many areas and thus the rough seas for which the region is known. Large storms occur in the bay during the winter months; the Bay of Biscay is home to some of the Atlantic Ocean's fiercest weather.
Up until recent years it was a regular occurrence for merchant vessels to founder in Biscay storms. The International Hydrographic Organization defines the limits of the Bay of Biscay as "a line joining Cap Ortegal to Penmarch Point"; the southernmost portion is the Cantabrian Sea. The main rivers that empty into the Bay of Biscay are Loire, Garonne, Adour, Bidasoa, Urumea, Urola, Artibai, Oka, Nervión, Agüera, Asón, Pas, Nansa, Sella, Nalón, Esva, Eo, Landro and Sor. In late spring and early summer a large fog triangle fills the southwestern half of the bay, covering just a few kilometers inland; as winter begins, weather becomes severe. Depressions enter from the west frequently and they either bounce north to the British Isles or they enter the Ebro Valley, dry out, are reborn in the form of powerful thunderstorms as they reach the Mediterranean Sea; these depressions cause severe weather at sea and bring light though constant rain to its shores. Sometimes powerful windstorms form if the pressure falls traveling along the Gulf Stream at great speed, resembling a hurricane, crashing in this bay with their maximum power, such as the Klaus storm.
The Gulf Stream enters the bay following the continental shelf's border anti-clockwise, keeping temperatures moderate all year long. The main cities on the shores of the Bay of Biscay are Bordeaux, Biarritz, Nantes, La Rochelle, Donostia-San Sebastián, Santander, Gijón and Avilés; the southern end of the gulf is called in Spanish "Mar Cantábrico", from the Estaca de Bares, as far as the mouth of Adour river, but this name is not used in English. It was named by Romans in the 1st century BC as Sinus Cantabrorum and Mare Gallaecum. On some medieval maps, the Bay of Biscay is marked as El Mar del los Vascos; the Bay of Biscay has been the site of many famous naval engagements over the centuries. In 1592 the Spanish defeated an English fleet during the eponymous Battle of the Bay of Biscay; the Biscay campaign of June 1795 consisted of a series of manoeuvres and two battles fought between the British Channel Fleet and the French Atlantic Fleet off the southern coast of Brittany during the second year of the French Revolutionary Wars.
USS Californian sank here after striking a naval mine on 22 June 1918. In 1920 SS Afrique sank after losing power and drifting into a reef in a storm with the loss of 575 lives. On 28 December 1943, the Battle of the Bay of Biscay was fought between HMS Glasgow and HMS Enterprise and a group of German destroyers as part of Operation Stonewall during World War II. U-667 sank on 25 August 1944 in position 46 ° 00 ′ N 01 ° 30 ′ W. All hands were lost. On 12 April 1970, Soviet submarine K-8 sank in the Bay of Biscay due to a fire that crippled the submarine's nuclear reactors. An attempt to save the sub failed, resulting in the death of forty sailors and the loss of four nuclear torpedoes. Due to the great depth, no salvage operation was attempted; the car ferries from Gijón to Nantes/Saint-Nazaire, Portsmouth to Bilbao and from Plymouth and Poole to Santander provide one of the most convenient ways to see cetaceans in European waters. Specialist groups take the ferries to hear more information. Volunteers and employees of ORCA observe and monitor cetacean activity from the bridge of the ships on Brittany Ferries' Portsmouth to Santander route.
Many species of whales and dolphins can be seen in this area. Most it is one of the few places in the world where the beaked whales, such as the Cuvier's beaked whale, have been observed frequently. Biscay Dolphin Research monitored cetacean activity from the P&O Ferries cruiseferry Pride of Bilbao, on voyages from Portsmouth to Bilbao. North Atlantic Right Whales, one of the most endangered whales, once came to the bay for feeding and for calving as well, but whaling activities by Basque people wiped them out sometime prior to 1850s; the eastern population of this species are considered to be extinct, a
Estuary of Bilbao
The Estuary of Bilbao lies at the common mouth of the rivers Nervion and Cadagua, that drain most of Biscay and part of Alava in the Basque Country, Spain. In this instance, the Spanish word estuario is used to describe what in English would be called part estuary, part tidal river; the estuary becomes a tidal river which extends 16 km into the city of Bilbao, starting from the Bilbao Abra bay. It hosts the port of Bilbao throughout its length, although the Port Authority has restored most of the upper reaches to Bilbao and other municipalities for their urban regeneration; the port is now being transferred to the seaboard on the coast at Zierbena. Downstream from Bilbao the river divides its metropolitan area in its left bank (Barakaldo, Sestao and Santurtzi and its right bank; the estuary and tidal river of Bilbao have always been a significant part of the city. Bilbao was born 700 years ago on the banks of the river Nervión as a trading village, it expanded downstream until arriving at the sea.
The river reached high levels of contamination because of the industrial activities during the past century. See page:http://bilbaoenconstruccion.com/2010/07/06/bilbao-recupera-su-alma-plan-integral-de-saneamiento-de-la-ria/ Bilbao Ria 2000
Getxo is a town located in the province of Biscay, in the autonomous community of the Basque Country, in Spain. It is part of Greater Bilbao, has about 80,000 inhabitants. Getxo is an affluent residential area, as well as being the third largest municipality of Biscay. Getxo was a parish a rural area, including a large beach at the mouth of the Estuary of Bilbao, centered on the little fishing village of Algorta; the parish council met at the church of Getxoko Andra Mari or Santa María de Getxo, not far from the headland called Punta Galea. The town's coat of arms has an oak with two cauldrons chained to its branches and the motto Kaltea Dagianak Bizarra Lepoan. With industrialisation in the 19th century, some parts of Getxo evolved into residential areas for the rich bourgeois class. A residential area called; the village of Algorta grew around the church of Saint Nicholas and the canalisation of the firth, provided for the colonisation of the beach, where a district called Areeta in Basque and Las Arenas was built.
Near Areeta / Las Arenas, on the other side of the road to Bilbao, there grew a working-class district called Erromo, similar to the one that grew near Neguri: Neguri Langile. In the 20th century, urban development reached the rural areas of Getxoko Andra Mari. Getxo, as well as the surrounding area known as Uribe-Kosta, grew in the last decades of the 20th century. While in the early 1980s the town had only 50,000 inhabitants, it has now more than 83,000; the surrounding towns of Leioa and Sopelana have multiplied their population in the same period. Getxo was hit by the Basque Conflict several times, with the town being the location of many ETA attacks; the deadliest of these was an ambush in October 1978 when three civil guards were killed and the most recent the car bomb attack on May 19, 2008. Many activists of the organisation have been born in Getxo, such as Arkaitz Goikoetxea, it is located 14 km north of Bilbao, in the province and historical Territory of Biscay, in the community of the Basque Country, in the north of Spain.
It has an area of 11.64 square kilometres. It borders in the north with Sopelana, in the east with Berango and Leioa, in the south with Portugalete and in the west with the Bay of the Cove; the municipality encompasses the neighborhoods of Las Arenas, Romo and Santa María de Getxo. But for the inhabitants of Getxo there is a more thorough division: Las Arenas: Las Mercedes, Santa Ana, Zugazarte y Antiguo Golf. Neguri: Neguri, San Ignacio. Algorta: Algorta centre, María Cristina, Arrigunaga, Villamonte, La Humedad, Fadura, Usategui, Portu Zaharra / Puerto Viejo and Bidezábal. Aiboa Santa María de Guecho / Getxoko Andra Mari: Aixerrota, Punta Galea, Avenida del Ángel, La Venta y Azkorri. RomoThe founding nucleus of the town of Getxo, the elizate or anteiglesia is what is known as Santa María or Andra Mari, a group of country houses or "baserris" around Saint Mary's church. Las Arenas and Neguri arose in the late nineteenth century as residential areas for the Basque industrial bourgeoisie. Neguri neighborhood is characterized by the palaces in which lived the elite of the bourgeoisie and where nowadays many of the people with more resources of Getxo live.
The name of Neguri was coined by Resurrección María de Azkue, since it was called Aretxetaurre. Neguri comes from the merger of two Basque words: negu and uri: Neguko hiri, the winter city designed, as has been noted, for the Basque bourgeoisie; the neighborhood of Algorta is the district of largest population of Getxo. The greatest expansion was in the 70s when middle-class families decided to find a more comfortable place to live rather than in the neighborhoods of the left bank of the Nervion. Romo neighborhood was built in the beginning to house the working class separated by the train barriers from Las Arenas. Nowadyas reaches the traffic circle of Romo; the district was shaped like a horseshoe. It borders the neighbourhood of Ibaiondo, so much so that the road from the roundabout Romo until the bank of the estuary of Bilbao is the municipal border between Getxo and Leioa. One sidewalk belongs to each municipality; the neighborhood of Santa María de Getxo stood longer as a rural area until the last third of the 20th century.
It still has several farmhouses, arable fields and pastures and but there are many villas and houses built in the 1990s. This romanesque church built in the 12th century took in the first inhabitants; this church suffered diverse reformations and the church that nowadays we can admire is from the 17th century based on the Baroque period. Inside the church is a sculpture of the Virgin and her son; this monument is the only antique windmill. The construction of the windmill was undertaken between 1726 and 1727 due to a huge drought and was focused on corn and feed production; the windmill, ones in lack of use, was set up as a home during all the 19th century. The name of Aixerrota comes from basque Aixe "wind" and errota "mill"; the construction of this windmill was motivated due to the drought, originated in Biscay at the beginning of the 18th century. It produces two types of flour: ordinary; the first historic date make reference to the windmill property is