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Puente Viesgo

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100-496: Puente Viesgo is a municipality in Cantabria , Spain. Caves have been discovered near Puente Viesgo that contain rock art and artefacts dating back to the Middle and Upper Paleolithic . The various populations of Puente Viesgo (Viesgo Bridge) are documented since the year 1000 by the abbey of Santillana del Mar . These documents describe a bridge over the river Pas , from which comes

200-588: A conurbation known as the Santander-Torrelavega metropolitan area. Castro Urdiales has an official population of 28,542, making it the fourth largest in the region because of its proximity to the Bilbao metropolitan area, there are a large number of people not registered in Castro Urdiales, and the true count may be double the official figure. The most populated municipalities of Cantabria as of 2018 are

300-422: A density of 78 inhabitants per square kilometre. Cantabria Cantabria ( / k æ n ˈ t eɪ b r i ə / , also UK : /- ˈ t æ b -/ ; Spanish: [kanˈtaβɾja] ) is an autonomous community and province in northern Spain with Santander as its capital city. It is called a comunidad histórica , a historic community , in its current Statute of Autonomy . It

400-475: A dominant effect on local microclimate in Cantabria. It is the main cause of the peculiar meteorologic situations like the so-called "suradas" ( Ábrego wind), due to the foehn effect : the southerly wind coming down from the mountains blows strongly and dry, increasing the temperature closer to the coast. This causes a decrease in air humidity and rainfall. These conditions are more frequent in autumn and winter, and

500-873: A few highland areas of Tasmania , and the Australian and Southern Alps . This type of climate is even found in very remote parts of the New Guinea Highlands . The classification used for this regime is Cfc. Temperatures above 30 °C (86 °F) and below −20 °C (−4 °F) are rare. In the most marine areas under this regime, temperatures above 20 °C (68 °F) are extreme weather events, even during summer. Small areas in Yunnan, Sichuan ; parts of Bolivia and Peru ; and parts of Mount Kilimanjaro in Tanzania have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This

600-548: A framework was established and formal steps began to be taken, leading to administrative and legal unity in 1778. This all culminated in the success of the Assembly held in the Assembly House of Puente San Miguel on 28 July 1778, where the province of Cantabria was constituted. It was achieved by passing the common ordinances which had been developed to that end, and which had been discussed and approved previously in councils of all

700-461: A lack of resources, continued to be the main reason for Cantabria's weakness, aggravated by the progressive advance of the Bourbonic centralism and its administrative efficiency. The latter continually emphasised the impossibility of the smaller territories facing a multitude of problems on their own: from communications to the exercise of justice, from putting aside adequate reserves for hard times to

800-509: A product and reflection of the cool ocean adjacent to them. In the autumn, winter, and early spring, when the polar jet stream is most active, the frequent passing of marine weather systems creates the frequent fog, cloudy skies, and light drizzle often associated with oceanic climates. They are typically found poleward of Mediterranean climates , except in Australia where they are poleward of both such climates and humid subtropical climates due to

900-534: A region stretching out far into the east. From this period on, source documents barely reference Cantabria by name, with Asturias featuring in names of the comarcas called Asturias de Santillana , Asturias de Trasmiera and Asturias de Laredo . From a central core formed by the Hermandad de las Cuatro Villas ( Brotherhood of the Four Cities ) (Santander, Laredo, Castro Urdiales and San Vicente de la Barquera ),

1000-561: A relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates , represented as Cwb or Cfb , and subpolar oceanic or cold subtropical highland climates , represented as Cfc or Cwc . Subtropical highland climates occur in some mountainous parts of

1100-612: A result of their location, these regions tend to be on the cool end of oceanic climates, approaching polar regions . Snowfall tends to be more common here than in other oceanic climates. Subpolar oceanic climates are less prone to temperature extremes than subarctic climates or continental climates , featuring milder winters than these climates. Subpolar oceanic climates feature only one to three months of average monthly temperatures of at least 10 °C (50 °F). As with oceanic climates, none of its average monthly temperatures fall below -3.0 °C (26.6 °F) or 0 °C depending on

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1200-738: A strict air-mass sense, not oceanic: they are affected by southerlies directly from the Mediterranean, and polar intrusions from Siberia. Yet their position near the Black Sea makes them too wet in summer to be Mediterranean , too mild during winter to be humid continental , and not hot enough in summer to be humid subtropical ; therefore Köppen classifies them as oceanic. Despite their anomalous position, however, their temperatures, around 4–5 °C (39–41 °F) in winter and 20–22 °C (68–72 °F) in summer, are not wholly atypical for European oceanic climates. Some Eastern European regions such as

1300-411: A surge of eucalyptus – see eucalyptus article on Spanish Misplaced Pages – plantations (and to a less extent of pines ) which often hid the illegal destruction of native forests, just as the spread of livestock farming had done in the past by the endemic conversion of forest into prairie. These acts have been laxly controlled by the local councils or the central governments, in a process that clearly follows

1400-485: Is Campoo , in southern Cantabria, with its Pyrenean oak. There are seven natural areas in this autonomous community designated as Natural or national parks : The most important of these is the Picos de Europa National Park, which affects Castile and León and Asturias in addition to Cantabria, the three autonomous communities sharing its management. Santoña, Victoria and Joyel marshes are also Special Protection Areas for

1500-425: Is a climate variety, often grouped together with oceanic climates, which exists in some mountainous or elevated portions of the world in either the subtropics or tropics. Despite the latitude, the higher elevations of these regions mean that the climate shares characteristics with oceanic climates. Subtropical highland climates with uniform rainfall ( Cfb ) usually have rainfall spread relatively evenly throughout

1600-463: Is below 18 °C (64 °F). Without their elevation, many of these regions would likely feature either humid subtropical or tropical climates. This type of climate exists in parts of east, south and southeastern Africa , interior southern Africa and elevated portions of eastern Africa as far north as Ethiopia and of western Africa (west region of Cameroon) up to the southwestern Angola highlands also share this climate type. It also exists in

1700-608: Is bordered on the east by the Basque autonomous community ( province of Biscay ), on the south by Castile and León ( provinces of León , Palencia and Burgos ), on the west by the Principality of Asturias , and on the north by the Cantabrian Sea , which forms part of the Bay of Biscay . Cantabria belongs to Green Spain , the name given to the strip of land between the Bay of Biscay and

1800-571: Is climatically Mediterranean , some parts of Southern Europe also have oceanic climates. However, these instances of the climate are highly variable, and often somewhat anomalous. The north coast of Spain , the western Azores off the coast of Portugal are too wet in summer to be Mediterranean, and too mild in summer to be humid subtropical , though they often have winter means above 9 °C (48 °F), unusual for European oceanic climates. Another anomalous case can be found in northwestern Turkey, including northern Istanbul . These places are, in

1900-594: Is found in parts of coastal Iceland , the Faroe Islands , upland/mountainous parts of Scotland and Northern England , northwestern coastal areas of Norway (most of Lofoten , Vesterålen , warmest part of Tromsø reaching to 71°N on some islands), uplands/highlands in western Norway, the Aleutian Islands of Alaska and northern parts of the Alaskan Panhandle , the southwest of Argentina and Chile , and

2000-704: Is in South Africa from Mossel Bay on the Western Cape coast to Plettenberg Bay (the Garden Route ), with additional pockets of this climate inland of the Eastern Cape and KwaZulu-Natal coast. It is usually warm most of the year with no pronounced rainy season, but slightly more rain in autumn and spring. The Tristan da Cunha archipelago in the South Atlantic also has an oceanic climate. Although oceanic climate

2100-448: Is more frequent and commonplace in the subpolar oceanic climates due to the colder weather in those locations. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature. In the Köppen climate classification , oceanic climates have a mean temperature of 0 °C (32 °F) or higher (or −3 °C (27 °F) or higher) in

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2200-678: Is more rain. The rivers of Cantabria are short and rapid, descending steeply because the sea is so close to their source in the Cantabrian Mountains. They flow perpendicular to the coastline, except for the Ebro . They also generally flow year round due to constant rainfall. Nevertheless, the rate of flow is modest (20 m /s annual average) compared to the other rivers of the Iberian Peninsula . The rapidness of their waters, caused by their steep descents, gives them great erosive power, creating

2300-695: Is rare in Asia, subtropical highland climates and cold subtropical highland climates can be found in parts of Southwestern China , and the Himalayan regions of the northern Indian subcontinent . The oceanic climate is prevalent in the more southerly parts of Oceania . A mild maritime climate is in existence in New Zealand. In Australia, the climate is found in Tasmania , southern half of Victoria and southeastern New South Wales (southwards from Wollongong ). Some parts of

2400-761: The Cantabrian Armaments in Santander, a section of the army whose purpose was to travel to all the mountain passes from the Central Plateau to detain any French troop. Although defeated, he managed later to regroup in Liébana under the command of General Juan Díaz Porlier, calling his forces the Cantabrian Division , in which there were various regiments and battalions, such as the Hussars of Cantabria ( cavalry ) or

2500-538: The Cantabrian Mountains , so called because of its particularly lush vegetation, due to the wet and temperate oceanic climate . The climate is strongly influenced by Atlantic Ocean winds trapped by the mountains; the average annual precipitation is about 1,200 mm (47 inches). Cantabria has archaeological sites from the Upper Paleolithic period, although the first signs of human occupation date from

2600-587: The Civil War . Following the war and the subsequent marginalization of such efforts under the Francoists regime , the use of the name of Cantabria decreased, to the point that for official purposes it was relegated to sports associations, the only arena in which Cantabria was noted as a region. In 1963, the president of the Provincial Council, Pedro Escalante y Huidobro, proposed reapplying the name of Cantabria to

2700-686: The Grand Banks of Newfoundland , is thought to greatly modify the climate of northwest Europe. As a result of the North Atlantic Current , west coast areas located in high latitudes like Ireland, the UK, and Norway have much milder winters (for their latitude) than would otherwise be the case. The lowland attributes of western Europe also help drive marine air masses into continental areas, enabling cities such as Dresden , Prague , and Vienna to have maritime climates in spite of being located well inland from

2800-800: The Guiana Shield , The highest elevations of the Brazilian Highlands , and due to variations in rainfall and temperature patterns in some places of the Tropical Andes in Bolivia, Perú, Ecuador, Colombia and Venezuela. Most of Yunnan and mountainous areas across Southeast Asia , parts of the Himalayas , parts of Sri Lanka , and parts of the Hawaiian Islands of Maui and Hawaii . In the Caribbean , only

2900-620: The Hermandad de las Marismas ( Brotherhood of the Marshes ) was created, thereby uniting all the important seaports to the East of Asturias. During the period of the Reconquista, the Four Cities actively participated in the re-settling of Andalusia, dispatching men and ships. The coastal port cities of Cádiz and El Puerto de Santa María were settled by families from the Cantabrian Sea ports. Ships from

3000-462: The Lower Paleolithic . The most significant site for cave paintings is in the cave of Altamira , dating from about 37,000 BCE and declared, along with nine other Cantabrian caves, as World Heritage Sites by UNESCO . Historically, the territory sits in the area of Cantabria in the ancient period , but from the late Middle Ages to the early 19th century, the name Cantabria also referred to

3100-752: The Northern Hemisphere include parts of coastal Iceland , the coast of Norway north of Bodø , the Scottish Highlands , the mountains of Vancouver Island , and Haida Gwaii in Canada . In the Southern Hemisphere examples include extreme southern Chile and Argentina (such as Punta Arenas and Ushuaia ), the Tasmanian Central Highlands , and parts of New Zealand . Oceanic climates are not necessarily found in coastal locations on

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3200-601: The Province of Santander , as suggested in an academic report written by the historian Tomás Maza Solano. Although further steps were taken and many of the townships were in favour of the move, the petition did not succeed, mostly due to the opposition of Santander City Council. On 30 December 1981, a process that had been started in April 1979 by the Council of Cabezón de la Sal , under the presidency of Ambrosio Calzada Hernández, culminated in

3300-614: The Reconquista , Cantabria still appears to be acknowledged as a region. In the Albendense Chronicle , when speaking of Alfonso I , it says, "This was the son of Peter , the duke of Cantabria". During the 9th century, on mentioning the monastery of Saint Zacharias, in a letter sent to Wiliesind , bishop of Pamplona, Eulogius of Córdoba pinpoints it in Seburim (maybe Zubiri ) on the river Arga , "waters all of Cantabria", suggesting

3400-805: The Shooters of Cantabria ( infantry ). During the Carlist wars they formed a unit called the Cantabrian Brigade . The use of terms with ancestral resonance through the 18th and 19th centuries continued during the 20th century, taking on a political tone that was distinctly regionalist, until 1936. In fact, the Republican Federal Party produced an autonomy statute for a Cantabrian-Castilian Federal State that year, which would include present-day Cantabria and any neighbouring areas from Castile and Asturias willing to join it. It could not be passed because of

3500-770: The Vascones . To the north of this cordon, however, the Cantabri continued to live independently until the Arab invasion. In 714, a mixed Arab / Berber army of Muslim Moors invaded the upper valleys of the Ebro and succeeded in capturing Amaya, the Cantabrian capital, forcing the Cantabrians back to their traditional frontiers, where they joined forces with the Kingdom of Asturias . In the first chronicles of

3600-425: The subtropics or tropics , some of which have monsoon influence, while their cold variants and subpolar oceanic climates occur near polar or tundra regions. Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in

3700-893: The subtropics . It exists in both hemispheres between 35° and 60°: at low altitudes between Mediterranean , humid continental , and subarctic climates. Western sea breezes ease temperatures and moderates the winter, especially if warm sea currents are present, and cause cloudy weather to predominate. Precipitation is constant, especially in colder months, when temperatures are warmer than elsewhere at comparable latitudes. This climate can occur farther inland if no mountain ranges are present or nearby. As this climate causes sufficient moisture year-round without permitting deep snow cover, vegetation typically prospers in this climate. Deciduous trees are predominant in this climate region. However, conifers such as spruce , pine , and cedar are also common in few areas, and fruits such as apples , pears , and grapes can often be cultivated here. In

3800-686: The territory of the Basques , especially the lordship of Biscay . The modern province of Cantabria was constituted on 28 July 1778 at Puente San Miguel, Reocín . The yearly Day of the Institutions holiday on 28 July celebrates this. The Organic Law of the Autonomy Statute of Cantabria , approved on 30 December 1981, gave the region its own institutions of self-government. Numerous authors, including Isidore of Seville , Julio Caro Baroja , Aureliano Fernández Guerra and Adolf Schulten , have explored

3900-745: The Ancient Cantabria, as opposed to Castile , which referred solely to the Central Plateau . This distinction has survived into modern times. With the rise of the Catholic Monarchs , the Brethren of the Marshes disappeared, leaving the Coregiment of the Four Villas, which included the whole area of influence of the old Brethren of the Four Villas (almost all of Cantabria). During the ancien régime ,

4000-684: The Basque Country, especially the lordship of Biscay, and the Basques . Cantabria is a mountainous and coastal region, with important natural resources. It has two distinct areas which are well differentiated morphologically: Towards the south are higher mountains, the tops of which form the watershed between the drainage basins of the Rivers Ebro , Duero and the rivers that flow into the Bay of Biscay. These peaks generally exceed 1,500 m (4,900 ft) from

4100-421: The Cantabri, particularly concerning the precise location of the territory that this people had occupied. It was not until the 18th century that the debate about the location and size of Ancient Cantabria was settled in a series of works which described the history of the region such as La Cantabria by the Augustinian father and historian Enrique Flórez de Setién. Concurrent with the resurgence of this interest in

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4200-521: The Cantabrian Sea, the Atlantic Ocean and the Mediterranean Sea. The variation in the altitude of the region, which in a short distance ranges from sea level to 2,600 meters in the mountains, leads to a great deal of diversity in vegetation and a large number of biomes . Cantabria has vegetation typical of the Atlantic side of the Iberian Peninsula. It is characterized by forests of leafy deciduous trees such as oak and European beech . Nevertheless, human intervention dating back to ancient times has favored

4300-425: The Cantabrians and the clarification of the aforementioned polemic, many institutions, organizations and jurisdictions in the mountainous territory received the name of "Cantabrian" or "of Cantabria". In 1727, the first attempt to unify what would later become the province of Cantabria occurred. Despite this, the high level of autonomy that the small entities of the fractured estate of Cantabria enjoyed, combined with

4400-470: The Celtic root "kant" or "cant" meaning edge or rim thus "coastal district," or "corner-land", "land on the edge" thus having the same probable derivation as the name of the English county of Kent and Canterbury , one of its major cities. During the Spanish liberal regimes of the 19th century, the term came to be increasingly associated to the province of Santander. However, in late medieval and Modern Period literature, Cantabria and Cantabrians refer to

4500-439: The Country in Cantabria, and presides over the Government, coordinating its activities. Oceanic climate An oceanic climate , also known as a marine climate or maritime climate , is the temperate climate sub-type in Köppen classification represented as Cfb , typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with

4600-414: The Four Cities took part in the taking of Seville , destroying the ship bridge linking Triana and Sevilla, a victory that is represented by the Carrack and the Torre del Oro of Sevilla in the coat of arms of Santander , Coat of arms of Cantabria and Avilés (Asturias). In the 16th century, the name La Montaña ( The Mountain ) was widespread in popular usage and in literature, as a designation of

4700-505: The Iberian Peninsula and elsewhere. It is certain that they participated in the Second Punic War , from references by Silius Italicus and Horace . When C. Hostilius Mancinus was besieging Numantia , he withdrew upon learning that Cantabri and Vaccaei were present among his auxiliaries . The Cantabrian Wars began in 29 BC. They were defeated by Agrippa with great slaughter in 19 BC , but they revolted again under Tiberius and were never entirely subdued. In older geographers,

4800-431: The Parliament are: to exercise the legislative power , to approve the budgets of the Autonomous Community, to motivate and control the actions of the government, and to develop the rest of the competences that the Spanish Constitution , the Autonomy Statute and the rest of the legal order bestow on it. The President of the Autonomous Community holds the highest representation of the Community and ordinary representation of

4900-439: The Pass of San Glorio in the west to the Pass of Los Tornos in the eastern part: Peña Labra, Castro Valnera and the mountain passes of Sejos, El Escudo and La Sía. The great limestone masses of Picos de Europa also stand out in the southwest of the region: most of their summits exceed 2,500 m (8,200 ft), and their topography is shaped by the former presence of glaciers . Due to the Gulf Stream , Cantabria, as well as

5000-424: The Villa of Pujayo, the Villa of Pie de Concha y Bárcena, the Valley of Anievas, and the Valley of Toranzo. Having learned lessons from the failed attempt of 1727, the first objective of the new entity was to obtain approval from King Charles III for the union of all the Cantabrian jurisdictions into one province. The royal ratification was granted on 22 November 1779. The 28 jurisdictions that initially comprised

5100-424: The aforementioned parallels; however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream , which moves in a west to east direction across the middle latitudes, advances low pressure systems, storms, and fronts. In coastal areas of the higher middle latitudes (45–60° latitude), the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are

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5200-491: The approval of the General Courts on 15 December 1981, the King of Spain signed the corresponding Organic Law of Autonomy Statute for Cantabria on 30 December of the same year. Thus, the province of Santander broke its link to Castile, and left the former region of Castile and León to which it had belonged up to that time, together with the provinces of Ávila , Burgos , León , Logroño , Palencia , Salamanca , Segovia , Soria , Valladolid and Zamora . On 20 February 1982,

5300-402: The birds (ZEPA ). Furthermore, nine Sites of Community Importance (LIC ) have been declared: Western Mountain, Eastern Mountain, Western Rias and Oyambre Dunes, Dunes of Liencres and Estuary of the Pas, El Puntal Dunes and Estuary of the Miera, Ria de Ajo, Marshes of Noja - Santoña , Escudo de Cabuérniga Range and several caves with important bat colonies. According to the 2009 census,

5400-550: The cave wall. These are believed to be the oldest examples of rock art in the region. They could not be dated by radiocarbon techniques because the pigments contained no organic matter, but were dated by assessing the age of the calcium carbonate deposit that had formed over the surface. One red disc was found to be 40,800 years old. Another cave nearby is the Cueva de las Monedas . The paintings here are black, being made with coal, and depict horses, goats, bears, bison and reindeer. The pictures of reindeer are believed to date back to

5500-570: The coldest month, compared to continental climates where the coldest month has a mean temperature of below 0 °C (32 °F) (or −3 °C (27 °F)) in the coldest month. Summers are warm but not hot, with the warmest month having a mean temperature below 22 °C (72 °F). Poleward of the latter is a subtype of it, the subpolar oceanic climate (Köppen Cfc ), with long but relatively mild (for their latitude) winters, and cool and short summers with average temperatures of at least 10 °C (50 °F) for one to three months. Examples in

5600-416: The collapse of the Roman Empire, Cantabria regained its independence from the rule of the Visigoths . In 574, King Liuvigild attacked Cantabria and managed to capture the south of the country, including the city of Amaya , where he established a Visigothic province called the Duchy of Cantabria (see picture), which would serve as a limes or frontier zone to contain the Cantabri as well as their neighbors

5700-430: The creation of pastures, allowing the existence of large areas of grassland and prairies suitable for grazing cattle. These grasslands are mingled with plantations of eucalyptus and native oak. The southern part of Cantabria, including the comarca of Campoo the fringes of the Castilian plateau, is characterized by the transition to drier vegetation. Another diversifying factor which contributes to local variation within

5800-402: The desire to respect fundamental rights and public freedom, at the same time as consolidating and stimulating regional development through democratic channels. This document gathers all competences of the Autonomous Community that were transferred from the Government of Spain . As in other Autonomous Communities, some competences were not transferred, for example, Justice. The Statute also defines

5900-487: The east, and (in some locations) summers become hotter. The line between oceanic Europe and Mediterranean Europe normally runs west to east and is related to changes in precipitation patterns and differences to seasonal temperatures; although intrusions of polar air, remnants of marine air-masses, and higher summer precipitation can create oceanic climates in Eastern Europe and transcontinental regions as far south as 40°N. The oceanic climate exists in an arc spreading across

6000-439: The etymology of the name Cantabria , yet its origins remain uncertain. The Online Etymology Dictionary states the root cant- is said to come from the Celtic for "rock" or "rocky", while -abr was a common suffix used in Celtic regions. Thus, Cantabrian could mean "people who live in the rocks" or " highlanders ", a reference to the steep and mountainous territory of Cantabria. The name Cantabria could also be related to

6100-425: The exposed areas of the High Atlas , some mountainous areas across southern Europe , mountainous sections of North America , including parts of the southern Appalachians and the Central America Volcanic Arc . In South America , it can be found mainly in temperate mountainous areas in the Tropical Andes , Venezuelan Coastal Range , the highest elevations of Serra do Mar in Southeastern Brazil , and tepuis of

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6200-521: The first Regional Assembly (now Parliament) was formed, with provisional status. From this time, the former province of Santander has been known as Cantabria and has thereby regained its historic name. The first home-rule elections were held in May 1983. The 4th Legislature (1995–1999) brought into effect the first great reform of the Autonomy Statute of Cantabria, approved by all the parliamentary groups. The Autonomy Statute of Cantabria of 30 December 1981, established that Cantabria has in its institutions

6300-413: The following joined in quick succession: the Abbey of Santillana , the Valleys of Tudanca , Polaciones , Herrerías , Castañeda , the Villa of Torrelavega and environs, Val de San Vicente , Valle de Carriedo , Tresviso , and the Pasiegan Villas of La Vega , San Roque and San Pedro , as well as the city of Santander with its abbey. Competition between the townships of Laredo and Santander led to

6400-507: The following: The first written reference to the name Cantabria emerges around 195 BC, in which the historian Cato the Elder speaks in his book Origines about the source of the Ebro River in the country of the Cantabri : ...The Ebro River starts in the land of the Cantabri , large and beautiful, with abundant fish... There are about 150 references to Cantabria or the Cantabri in surviving Greek and Latin texts. The Cantabri were used as mercenaries in various conflicts, both within

6500-427: The granting of self-rule to Cantabria, outlined in Article 143 of the Spanish Constitution . Cantabria based its claim to autonomy on the constitutional precept that made provision for self-government for " provinces with a historic regional character ". A Mixed Assembly formed out of provincial deputies and national members of parliament began the task of drawing up an Autonomy Statute on 10 September 1979. Following

6600-439: The greatest jurisdictional lordships of Cantabria were mainly under the control of three of the Grandee families of Spain: that of Mendoza ( Dukes of Infantado , Marquises of Santillana), of Manrique de Lara (Marquises of Aguilar de Campoo, Counts of Castañeda ), and to a lesser extent that of Velasco ( Dukes of Frías , Constables of Castile ). From the 16th century on, there was renewed interest in studying Cantabria and

6700-817: The hottest month, the average temperature is below 22 °C (72 °F), and at least four months feature average temperatures higher than 10 °C (50 °F). The average temperature of the coldest month must not be colder than −3–0 °C (27–32 °F), or the climate will be classified as continental. The average temperature variations in the year are between 10–15 °C (50–59 °F), with average annual temperatures between 6–13 °C (43–55 °F). Rain values can vary from 50–500 cm (20–197 in), depending on whether mountains cause orographic precipitation . Frontal cyclones can be common in marine west coast regions, with some areas experiencing more than 150 rainy days annually, but strong storms are rare. Cfb climates are predominant in most of Europe except

6800-654: The immediate west and northwest in transition for humid continental , the remainder of Cape Cod ) and northeastern Georgia both in the eastern United States . It is also found in the highest portions of the Brazilian state of Bahia and Roraima (in transition or strongly influenced for Cwb ), Brønnøy Municipality in Nordland at 65.28 °N ( Norway north-central coast), the provinces of Sabah (northeastern Malaysia ), and Baluchistan , Pakistan . Although there are more or less rare places associated with relatively isolated mountainous regions (e.g., North Oceania islands and China ). The subtropical highland climate

6900-471: The indiscriminate levees for soldiers, and above all the progression of fiscal impositions. All of this led to an acceleration of contact between villas, valleys and jurisdictions, which tended to focus on the Assemblies of the provinces of the Nine Valleys, led by the deputies elected by the traditional entities of self-government. There were two events that triggered the culmination of the integration process in this second attempt: In this General Assembly

7000-505: The isotherm used. Typically, these areas in the warmest month experience daytime maximum temperatures below 17 °C (63 °F), while the coldest month features highs slightly above freezing and lows near or just below freezing while keeping the average warm enough. It typically carries a Cfc designation, though very small areas in Argentina and Chile have summers sufficiently short to be Cwc with fewer than four months over 10 °C (50 °F). This variant of an oceanic climate

7100-409: The last ice age, about 13,000 years ago. Also in the municipality is the Cueva de La Pasiega , part of the World Heritage Site that includes the "Cave of Altamira and palaeolithic cave art of Northern Spain". Puente Viesgo is in the valley of the River Pas and is located in the central part of Cantabria, about 30 kilometres (19 mi) west of the regional capital, Santander . It is surrounded by

7200-416: The latter, having initially allowed the name of Cantabria for the province created at the beginning of the 19th century, later retracting its consent and demanding that it bear the name of Santander, so there would be no doubt as to which was the capital. When in 1821 the Provincial Council presented before the constitutional Courts its definitive plan for the provincial borders and legal entities, it proposed

7300-508: The name of province of Cantabria, to which the Township of Santander replied that " this province must retain the name of Santander ". However, many newspapers still showed in their headings the name of Cantabria, or Cantabrian. During the War of Independence (1808–1814), Bishop Rafael Tomás Menéndez de Luarca, a strong defender of absolutism, promoted himself as the "Regent of Cantabria" and established

7400-501: The name of the municipality. The Cave of El Castillo was discovered in 1903 by the Spanish archaeologist Hermilio Alcalde del Río and was first explored and excavated by the German prehistorian Hugo Obermaier , with further excavation taking place in 1980. There are paintings of bison and horses, and large numbers of handprints, made by blowing mineral particles onto a hand pressed against

7500-421: The narrow V-shaped valleys characteristic of Green Spain. The environmental condition of the rivers is generally good, although increasing human activity due to rising population in the valleys continues to pose a challenge. The main rivers of the region, sorted by drainage basin , are: Cantabria is the only autonomous community whose rivers flow into every one of the seas which surround the Iberian Peninsula :

7600-531: The north of Croatia and Serbia and some parts of the Czech Republic , also have oceanic climates; these are generally near the boundary for being humid continental . The line between oceanic and continental climates in Europe runs in a generally north to south direction. For example, western Germany is more impacted by milder Atlantic air masses than eastern Germany. Thus, winters across Europe become colder to

7700-792: The northeast, as global temperatures became warmer towards late 20th and early 21st century. They are the main climate type in New Zealand and the Australian states of Tasmania , Victoria , and southeastern New South Wales (starting from the Illawarra region). In North America, they are found mainly in Vancouver Island and neighbouring parts of British Columbia , as well as many coastal areas of southeast Alaska . There are pockets of this iteration of Cfb climates in South American countries, mostly in regions of southern Chile and Argentina, parts of

7800-644: The northeastern coast of Honshu , such as Mutsu, Aomori in Japan, feature this climate, which is rare in Asia due to the lack of a west coast in the middle latitudes. Île Amsterdam and Île Saint-Paul , both part of the French Southern and Antarctic Lands , are located in the subtropics and have an oceanic climate (akin to Tristan da Cunha; see above). Temperate oceanic climates, also known as "marine mild winter" climates or simply oceanic climates, are found either at middle latitudes . They are often found on or near

7900-611: The northwestern coast of North America from the Alaskan panhandle to northern Washington . In addition, some east coast areas such as Block Island , Cape Cod , Martha's Vineyard , and Nantucket have a similar climate. And in the highlands of Central and South America with the variant Cfb. An extensive area of oceanic climates distinguishes the coastal regions of southern Chile and extends into bordering Argentina . The only noteworthy area of maritime climate at or near sea-level within Africa

8000-743: The ocean. Oceanic climates in Europe occupy a large stretch of land, from Norway 's Atlantic coast, Ireland and the United Kingdom and southeast to some parts of Turkey . Western Europe is almost exclusively oceanic between 45°N to 54.913°N; including most of France (away from the Mediterranean), nearly all of Belgium , the Netherlands , Austria , most of Luxembourg , most of Denmark , western Germany , northwestern Switzerland , south coast and western areas of Norway north to Skrova and extreme southern Sweden . While most of Southern Europe

8100-812: The peaks in the highest mountain ranges have this climate (including the Blue Mountains in Jamaica and Cerro Maravilla in Puerto Rico ), with only Hispaniola 's Cordillera Central and Chaîne de la Selle having significant urban settlements under this climate zone, such as cities like Kenscoff in Haiti and Constanza in the Dominican Republic . Areas with subpolar oceanic climates feature an oceanic climate but are usually located closer to polar regions, with long but relatively mild winters and short, cool summers. As

8200-432: The population were immigrants. The predominant countries of origin for immigrants to Cantabria are Colombia , Romania , Ecuador , Peru , Moldova , and Morocco . The majority of the population resides in the coastal area, particularly in two cities: Santander , with 183,000 people, and Torrelavega , the second largest urban and industrial centre in Cantabria, having a population of around 60,000. These two cities form

8300-526: The province of Cantabria were clear in their intention that all the other jurisdictions that formed the Party and Baton of the Four Villas of the Coast should be included in the new province. To this end they set out the steps needed for this to happen as soon as those jurisdictions should request it. They would have to abide by the ordinances, having the same rights and duties as the founders, all on an equal footing. Thus,

8400-629: The provinces of Chubut , Santa Cruz , and southeast Buenos Aires province in Argentina. In Western Asia , the climate can be found on the Black Sea coast of northern Turkey and Georgia , often transitional to humid subtropical . While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa . The climate subtype can also be found in Nantucket , Massachusetts (in

8500-460: The region has a population of 591,886 which constitutes 1.29% of the population of Spain, with the population density numbering 106.8 people per kilometer. The average life expectancy for male inhabitants is 75 years; for female inhabitants, it is 83 years. Eight years later in 2017 the population has fallen to 581,477 according to INE. In relative contrast to other regions of Spain, Cantabria has not experienced much immigration. In 2007, only 4.7% of

8600-469: The region is the Mediterranean ecotone , giving rise to species unique to the region, such as the holm oak and arbutus trees , which are found in poor limestone soils with little moisture. In Cantabria there are several zones of plant life: During the last two decades of the 20th century, and due mainly to European agricultural policies ( CAP ), many farmers substituted forestry for livestock farming, so as to avoid unemployment and poverty. This provoked

8700-419: The regions, but are more common in subtropical highland climates where these air masses meet more frequently due to the influence of hotter weather in the subtropics or tropics, especially in monsoon-influenced climates. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. Most oceanic climate zones, however, experience at least one snowfall per year. Snowfall

8800-611: The rest of "Green Spain", has a much more temperate climate than might be expected for its latitude. The region has a humid oceanic climate , with warm summers and mild winters. Annual precipitation is around 1,200 mm at the coasts and higher in the mountains. The mean temperature is about 14 °C (57.2 °F). Snow is frequent in the higher zones of Cantabria between the months of October and March. Some zones of Picos de Europa, over 2,500 metres high, have an alpine climate with snow persisting year-round. The driest months are July and August. The mountainous relief of Cantabria has

8900-478: The saying: " Pan para hoy, hambre para mañana " (which translates as 'Bread for today, hunger for tomorrow'; i.e., "short-term gain, long-term pain"). The plantation of pines has given way in the last decades to that of eucalyptus because this non-indigenous species has no natural attacker within the European ecosystem (while pines are highly vulnerable to the pine processionary ). Both in relative and absolute terms

9000-597: The shape of the continent. Only in Europe do they penetrate far inland, where they eventually transition into warm-summer humid continental climates ; in other continents, they are blocked by a large mountain range or limited by nearby oceans. The North Atlantic Gulf Stream , a tropical oceanic current that passes north of the Caribbean and up the East Coast of the United States to North Carolina , then heads east-northeast to

9100-467: The symbols that should represent the region: The flag , the coat of arms and the anthem of Cantabria . The Parliament of Cantabria is the principal self-government institution of the Autonomous Community, being the representative body of the Cantabrians. Presently it is constituted by thirty-nine deputies elected by universal, equal, free, direct and secret suffrage. The primary functions of

9200-412: The temperatures are commonly higher than 20 °C (68 °F). Fires are often helped by this type of wind: one example is the fire that destroyed part of the city of Santander in the winter of 1941 . In these specific cases in the southern part of the mountain range the dry adiabatic gradient produces different conditions to the rest of the region: the wind there is fresher and more humid, and there

9300-645: The term Cantabria referred to an expansive country bounded by the Cantabrian Sea (the Bay of Biscay ), the western side of the Sella valley in Asturias , the hillfort of Peña Amaya in Burgos , and along the Aguera River almost as far as Castro Urdiales . It thus included areas of Asturias , Santander , Biscay , and Guipuzcoa . Following the Roman conquest of Spain , however, it

9400-448: The tropics, a subtropical highland climate typically features mild weather year-round. Temperatures there remain relatively constant throughout the year and snowfall is seldom seen due to warmer winters than most oceanic climates. Areas with this climate feature monthly averages below 22 °C (72 °F) but above either 0 °C (32 °F) or −3 °C (27 °F) depending on isotherm used. At least one month's average temperature

9500-488: The use of woods for forestry has increased in Cantabria, and is now almost 70% of all woods in the region. Along with these characteristics it would also be necessary to mention peculiarities of the comarca of Liébana , which has a microclimate very similar to the Mediterranean , allowing to grow cork oaks , vines and olives , and which is still very well conserved from human activity. The other remarkable comarca

9600-401: The verdant countryside of the coastal strip and lies between the Bay of Biscay to the north and the Cantabrian Mountains to the south. The economy has traditionally been based on agriculture but now many people are employed in the tourist industry. The municipality consists of the villages, Aés, Hijas, Las Presillas, Puente Viesgo and Vargas. The population at the last census was 2,800, giving

9700-653: The villas, valleys and subscribed jurisdictions. They were, in addition to the Nine Valleys: Rivadedeva, Peñamellera, the province of Liébana, Peñarrubia, Lamasón, Rionansa, the Villa of San Vicente de la Barquera, Coto de Estrada, Valdáliga, the Villa of Santillana del Mar, Lugar de Viérnoles, the Villa of Cartes and environs, the Valley of Buelna, the Valley of Cieza, the Valley of Iguña with the Villas of San Vicente and Los Llares,

9800-414: The west coast of continents; hence another name for Cfb, "marine west coast climates". In addition to moderate temperatures year-round, one of the characteristics is the absence of a dry season. Except for Europe , this type of climate is confined to narrow bands of territory, largely in mid or high latitudes, although it can appear in elevated areas of continental terrain in low latitudes, e.g. plateaus in

9900-571: The year, similar to other oceanic climates, but unlike these climates, they have a high diurnal temperature variation and low humidity, owing to their inland location and relatively high elevation. Subtropical highland climates with monsoon influence ( Cwb ) have distinctive wet summers and dry winters . In locations outside the tropics, other than the drying trend in the winter, subtropical highland climates tend to be essentially identical to an oceanic climate, with mild summers and noticeably cooler winters, plus, in some instances, some snowfall. In

10000-703: Was restricted to the area of Santander and eastern Asturias , forming a part of Hispania Tarraconensis (" Tarragonan Spain"). The principal tribes of the area were the Pleutauri , the Varduli , the Autrigones , the Tuisi , and the Conisci or Concaui , who were known for feeding on their horses' blood . The area was well settled, with the largest city being Juliobriga , and the local mountains exploited for lead mines. Following

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