1.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
2.
Gibraltar
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Gibraltar is a British Overseas Territory located on the southern end of the Iberian Peninsula. It has an area of 6.7 km2 and shares its border with Spain. The Rock of Gibraltar is the landmark of the region. At its foot is a populated city area, home to over 30,000 Gibraltarians. An Anglo-Dutch force captured Gibraltar from Spain in 1704 during the War of the Spanish Succession on behalf of the Habsburg claim to the Spanish throne, the territory was subsequently ceded to Great Britain in perpetuity under the Treaty of Utrecht in 1713. Today Gibraltars economy is based largely on tourism, online gambling, financial services, the sovereignty of Gibraltar is a major point of contention in Anglo-Spanish relations as Spain asserts a claim to the territory. Gibraltarians overwhelmingly rejected proposals for Spanish sovereignty in a 1967 referendum, under the Gibraltar constitution of 2006, Gibraltar governs its own affairs, though some powers, such as defence and foreign relations, remain the responsibility of the British government. The name Gibraltar is the Spanish derivation of the Arabic name Jabal Ṭāriq, earlier, it was known as Mons Calpe, a name of Phoenician origin and one of the Pillars of Hercules. The pronunciation of the name in modern Spanish is, evidence of Neanderthal habitation in Gibraltar between 28,000 and 24,000 BP has been discovered at Gorhams Cave, making Gibraltar possibly the last known holdout of the Neanderthals. Within recorded history, the first inhabitants were the Phoenicians, around 950 BC, subsequently, Gibraltar became known as one of the Pillars of Hercules, after the Greek legend of the creation of the Strait of Gibraltar by Heracles. The Carthaginians and Romans also established semi-permanent settlements, after the collapse of the Roman Empire, Gibraltar came briefly under the control of the Vandals. The area later formed part of the Visigothic Kingdom of Hispania from 414 AD until the Islamic conquest of Iberia in 711 AD, in 1160, the Almohad Sultan Abd al-Mumin ordered that a permanent settlement, including a castle, be built. It received the name of Medinat al-Fath, on completion of the works in the town, the Sultan crossed the Strait to look at the works and stayed in Gibraltar for two months. The Tower of Homage of the Moorish Castle remains standing today, from 1274 onwards, the town was fought over and captured by the Nasrids of Granada, the Marinids of Morocco and the kings of Castile. In 1462, Gibraltar was finally captured by Juan Alonso de Guzmán, after the conquest, King Henry IV of Castile assumed the additional title of King of Gibraltar, establishing it as part of the comarca of the Campo Llano de Gibraltar. In 1501, Gibraltar passed back to the Spanish Crown, the occupation of the town by Alliance forces caused the exodus of the population to the surrounding area of the Campo de Gibraltar. As the Alliances campaign faltered, the 1713 Treaty of Utrecht was negotiated and ceded control of Gibraltar to Britain to secure Britains withdrawal from the war. Unsuccessful attempts by Spanish monarchs to regain Gibraltar were made with the siege of 1727 and again with the Great Siege of Gibraltar, during the American War of Independence
3.
United Kingdom
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The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom or Britain, is a sovereign country in western Europe. Lying off the north-western coast of the European mainland, the United Kingdom includes the island of Great Britain, Northern Ireland is the only part of the United Kingdom that shares a land border with another sovereign state—the Republic of Ireland. The Irish Sea lies between Great Britain and Ireland, with an area of 242,500 square kilometres, the United Kingdom is the 78th-largest sovereign state in the world and the 11th-largest in Europe. It is also the 21st-most populous country, with an estimated 65.1 million inhabitants, together, this makes it the fourth-most densely populated country in the European Union. The United Kingdom is a monarchy with a parliamentary system of governance. The monarch is Queen Elizabeth II, who has reigned since 6 February 1952, other major urban areas in the United Kingdom include the regions of Birmingham, Leeds, Glasgow, Liverpool and Manchester. The United Kingdom consists of four countries—England, Scotland, Wales, the last three have devolved administrations, each with varying powers, based in their capitals, Edinburgh, Cardiff and Belfast, respectively. The relationships among the countries of the UK have changed over time, Wales was annexed by the Kingdom of England under the Laws in Wales Acts 1535 and 1542. A treaty between England and Scotland resulted in 1707 in a unified Kingdom of Great Britain, which merged in 1801 with the Kingdom of Ireland to form the United Kingdom of Great Britain and Ireland. Five-sixths of Ireland seceded from the UK in 1922, leaving the present formulation of the United Kingdom of Great Britain, there are fourteen British Overseas Territories. These are the remnants of the British Empire which, at its height in the 1920s, British influence can be observed in the language, culture and legal systems of many of its former colonies. The United Kingdom is a country and has the worlds fifth-largest economy by nominal GDP. The UK is considered to have an economy and is categorised as very high in the Human Development Index. It was the worlds first industrialised country and the worlds foremost power during the 19th, the UK remains a great power with considerable economic, cultural, military, scientific and political influence internationally. It is a nuclear weapons state and its military expenditure ranks fourth or fifth in the world. The UK has been a permanent member of the United Nations Security Council since its first session in 1946 and it has been a leading member state of the EU and its predecessor, the European Economic Community, since 1973. However, on 23 June 2016, a referendum on the UKs membership of the EU resulted in a decision to leave. The Acts of Union 1800 united the Kingdom of Great Britain, Scotland, Wales and Northern Ireland have devolved self-government
4.
Andalusia
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Andalusia is an autonomous community in southern Spain. It is the most populated and the second largest in area of the communities in the country. The Andalusian autonomous community is recognised as historical nationality. The territory is divided into eight provinces, Almería, Cádiz, Córdoba, Granada, Huelva, Jaén, Málaga and its capital is the city of Seville. Andalusia is the only European region with both Mediterranean and Atlantic coastlines, the small British overseas territory of Gibraltar shares a three-quarter-mile land border with the Andalusian province of Cádiz at the eastern end of the Strait of Gibraltar. The main mountain ranges of Andalusia are the Sierra Morena and the Baetic System, consisting of the Subbaetic and Penibaetic Mountains, in the north, the Sierra Morena separates Andalusia from the plains of Extremadura and Castile–La Mancha on Spains Meseta Central. To the south the geographic subregion of Upper Andalusia lies mostly within the Baetic System, the name Andalusia is derived from the Arabic word Al-Andalus. Including an intense relationship with Naples, Italy, Andalusia has been a traditionally agricultural region, compared to the rest of Spain and the rest of Europe. However, the growth of the community especially in the sectors of industry and services was above average in Spain, the region has, however, a rich culture and a strong cultural identity. Many cultural phenomena that are seen internationally as distinctively Spanish are largely or entirely Andalusian in origin and these include flamenco and, to a lesser extent, bullfighting and Hispano-Moorish architectural styles. Andalusias hinterland is the hottest area of Europe, with cities like Córdoba, Late evening temperatures can sometimes stay around 35 °C until close to midnight, with daytime highs of over 40 °C common. Seville also has the highest average temperature in mainland Spain and mainland Europe. Its present form is derived from the Arabic name for Muslim Iberia. However, the etymology of the name Al-Andalus is disputed, the Spanish place name Andalucía was introduced into the Spanish languages in the 13th century under the form el Andalucía. This was a Castilianization of Al-Andalusiya, the form of the Arabic language al-Andalus. The etymology of al-Andalus is itself somewhat debated, but in fact it entered the Arabic language before this came under Muslim rule. Like the Arabic term al-Andalus, in historical contexts the Spanish term Andalucía or the English term Andalusia do not necessarily refer to the territory designated by these terms today. To designate the territories the Christians had regained by that time in the Guadalquivir valley and in the Kingdoms of Granada, in a document from 1253, Alfonso X styled himself Rey de Castilla, León y de toda Andalucía
5.
Murcia
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The population of the metropolitan area was 689,591 in 2010. It is located on the Segura River, in the Southeast of the Iberian Peninsula, noted by a climate with hot summers, mild winters, and relatively low precipitation. Murcia was founded by the emir of Cordoba Abd ar-Rahman II in 825 with the name Mursiyah مرسية and nowadays is mainly a services city and a university town. The city, as the capital of the comarca Huerta de Murcia is called Europes orchard due to its agricultural tradition and its fruit, vegetable. Murcia is located near the center of a fertile plain known as the huerta of Murcia. The Segura River and its tributary, the Guadalentín, run through the area. The city has an elevation of 43 metres above sea level, the best known and most dominant aspect of the municipal areas landscape is the orchard. A large regional park, the Parque Regional de Carrascoy y el Valle, the Segura River crosses an alluvial plain, part of a Mediterranean pluvial system. The river crosses the city from west to east and its volumetric flow is mostly small but the river is known to produce occasional flooding, like those that inundated the capital in 1946,1948,1973 or 1989. The Segura was recognized as one of the most polluted rivers in Europe, the Segura rivers Valley is surrounded by two mountain ranges, the hills of Guadalupe, Espinardo, Cabezo de Torres, Esparragal and Monteagudo in the north and the Cordillera Sur in the south. The municipality itself is divided into southern and northern zones by a series of mountain ranges and these two zones are known as Field of Murcia and Orchard of Murcia. Near the plains center, the hill of Monteagudo protrudes dramatically. The 881. 86-square-kilometre territory of Murcias municipality is made up of 54 pedanías and 28 barrios, the barrios make up the 12. 86-square-kilometre the main urban portion of the city. The historic city center is approximately 3 square kilometres of the downtown portion of Murcia. Murcia has a hot semi-arid climate, given its proximity to the Mediterranean Sea, it has mild winters and hot summers. It averages more than 320 days of sun per year, occasionally, Murcia has heavy rains where the precipitation for the entire year will fall over the course of a few days. In the coldest month, January, the temperature range is a high of 16.6 °C during the day. In the warmest month, August, the range goes from 34.2 °C during the day to 20.9 °C at night, temperatures almost always reach or exceed 40 °C on at least one or two days per year
6.
Castilla-La Mancha
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Castilla-La Mancha is a south-western European region that was part of the Kingdom of Castile. Nowadays it is established as a community of Spain. Castilla-La Mancha is bordered by Castile and León, Madrid, Aragon, Valencia, Murcia, Andalusia and it is one of the most sparsely populated of Spains autonomous communities. Albacete is the largest and most populous city and its capital city is Toledo, and its judicial capital city is Albacete. It is mostly in this region where the story of the famous Spanish novel Don Quixote by Miguel de Cervantes is situated, due to which La Mancha is internationally well-known. Although La Mancha is a windswept, battered plateau, it remains a symbol of Spanish culture with its vineyards, sunflowers, mushrooms, olive plantations, windmills, Manchego cheese, the history of Castilla-La Mancha has been significant. Its origin lay in the Muslim period between the 8th and 14th century, Castilla-La Mancha was the region of many historical battles between Christian crusaders and Muslim forces during the period from 1000 to the 13th century. It was also the region where the Crown of Castile and Aragon were unified in 1492 under Queen Isabel, Castilla-La Mancha is the successor to New Castile, which in turn traces back to the Muslim Taifa of Toledo, one of the taifas of Al Andalus. Alfonso VI conquered the region from the Muslims, taking Toledo in 1085, the Reconquista took Cuenca in 1177. That victory assured Castilian domination of the region and hastened the decline of the Almohad Dynasty, from the time of the Reconquista, Castilla-La Mancha formed part of the Kingdom of Castile. Four centuries later, in 1605, Cervantes Don Quixote gave the world a picture of La Mancha. In 1785, the organization by the reformer Floridablanca divided the region into the provinces of Cuenca, Guadalajara, Madrid, La Mancha. Albacete, Chinchilla, Almansa, Hellín and Yeste, however, Albacete, in turn, also incorporated parts of the territories of the old provinces of Cuenca and Murcia. Albacete was administered as part of the Region of Murcia until the 1978 configuration of autonomous regions, the Autonomous Community of Castilla-La Mancha dates from November 15,1978, as one of the many autonomous regions defined by the Spanish central government. The new, hyphenated name constituted an effort to two distinct regionalisms, that of the larger Castilla and that of the smaller onetime province of La Mancha. The Statute of Autonomy of Castilla–La Mancha was approved August 10,1982, Castilla-La Mancha is divided into 5 provinces named after their capital cities. 496 of these have less than 500 inhabitants,231 have between 501 and 2,000 inhabitants,157 between 2,000 and 10,000 inhabitants, and only 35 have more than 10,000 inhabitants. The municipalities in the north are small and numerous, while in the south they are larger and fewer and this reflects different histories of how these sub-regions were repopulated during the Reconquista
7.
Valencian Community
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The Valencian Community, or the Valencian Country, is an autonomous community of Spain. It is the fourth most populousautonomous community after Andalusia, Catalonia and it is often homonymously identified with its capital Valencia, which is Spains third largest city. It is located along the Mediterranean coast to the east of the Iberian peninsula and it borders with Catalonia to the north, Aragon and Castile–La Mancha to the west, and Murcia to the south. The Valencian Community consists of three provinces which are Castellón, Valencia and Alicante, according to its Statute of Autonomy, the Valencian people are a nationality. Their origins date back to the Catalan-Aragonese colonization of the Moorish Taifa of Valencia, the newly founded Kingdom of Valencia was granted wide self-government under the Crown of Aragon with the promulgation of its Furs in 1261. Valencia experienced its golden age in the 15th century, becoming the economic and cultural capital of the Crown, self-government continued after the unification of the Spanish Kingdom, but was eventually suspended in 1707 by Phillip V of Spain as a result of the Spanish War of Succession. Valencian nationalism resurged towards the end of the 19th century, which led to the conception of the Valencian Country. Self-government under the Generalitat Valenciana was finally reestablished in 1982 after Spanish transition to democracy, the Valencian people speak a variety of Catalan called Valencian, accounting for a third of all Catalan speakers. Valencian is a language that has been historically repressed in favour of Spanish. Since it regained status in 1982, Valencian has been implemented in public administration. However, its use continues to be threatened by Spanish due to migration from other parts of Spain, especially in the cities of València. Furthermore, the conflict continues to be pressing, with some groups opposing the official standard based on Catalan orthography. Valencia was founded by the Romans under the name of Valentia Edetanorum, with the establishment of the Taifa of Valencia, the name developed to بلنسية, which eventually became Valencia after the expulsion of the Moors. Valencian Community is the translation of the official name in Valencian recognized by the Statute of Autonomy of 1982. This is the name most used in administration, tourism. On one hand, Valencian Country represented the modern conception of nationality that resurged in the 19th century and it became well-established during the Second Spanish Republic and later on with the works of Joan Fuster in the 1960s, implying the existence of the Catalan Countries. This nationalist subtext was opposed by anti-Catalan blaverists, who proposed Former Kingdom of Valencia instead in order to emphasize Valencian independence from Catalonia, currently, blaverists have accepted the official denomination. The autonomous community can be identified with its capital Valencia
8.
Rock of Gibraltar
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The Rock of Gibraltar is a monolithic limestone promontory located in the British overseas territory of Gibraltar, near the southwestern tip of Europe on the Iberian Peninsula. The Rock is Crown property of the United Kingdom, and borders Spain, most of the Rocks upper area is covered by a nature reserve, which is home to around 300 Barbary macaques. These macaques, as well as a network of tunnels. The Rock of Gibraltar was one of the Pillars of Hercules and was known to the Romans as Mons Calpe, in ancient times, the two points marked the limit to the known world, a myth originally fostered by the Greeks and the Phoenicians. Gibraltar is surrounded by the Mediterranean Sea and has no contact with the Atlantic Ocean, the Rock of Gibraltar is a monolithic promontory. The Main Ridge has a sharp crest with peaks over 400 m above sea level and it is a deeply eroded and highly faulted limb of an overturned fold. The sedimentary strata composing the Rock of Gibraltar are overturned, with the oldest strata overlying the youngest strata and these strata are the Catalan Bay Shale Formation, Gibraltar Limestone, Little Bay Shale Formation, and Dockyard Shale Formation. These strata are noticeably faulted and deformed, the Catalan Bay Shale Formation contains unidentifiable echinoid spines and belemnite fragments and infrequent Early Jurassic ammonites. The Gibraltar Limestone consists of greyish-white or pale-gray compact, and sometime finely crystalline and this formation comprises about three quarters of the Rock of Gibraltar. Geologists have found various poorly preserved and badly eroded and rolled marine fossils within it, the fossils found in the Gibraltar Limestone include various brachiopods, corals, echinoid fragments, gastropods, pelecypods, and stromatolites. These fossils indicate an Early Jurassic age for the deposition of the Gibraltar Limestone, the Little Bay and Dockyard shale formations form a very minor part of the Rock of Gibraltar. The Little Bay Shale Formation consists of dark bluish-gray, unfossiliferous shale, which is interbedded with layers of grit, mudstone. The Dockyard Shale Formation is an undescribed variegated shale of unknown age that lies buried beneath the Gibraltars dockyard and coastal protection structures. When the African tectonic plate collided tightly with the Eurasian plate, the Atlantic Ocean then broke through the Strait of Gibraltar, and the resultant flooding created the Mediterranean Sea. The Rock forms part of the Betic Cordillera, a range that dominates south-eastern Iberia. Today, the Rock of Gibraltar forms a peninsula jutting out into the Strait of Gibraltar from the southern coast of Spain, the promontory is linked to the continent by means of a sandy tombolo with a maximum elevation of 3 m. To the north, the Rock rises vertically from sea level up to 411.5 m at Rock Gun Battery, the Rocks highest point stands 426 m near the south end above the strait at OHaras Battery. The Rocks central peak, Signal Hill and the top station of the Gibraltar Cable Car, the western face, where the City of Gibraltar is located, is comparatively less steep
9.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
10.
Orogeny
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An Orogeny is an event that leads to a large structural deformation of the Earths lithosphere due to the interaction between tectonic plates. Orogens or orogenic belts develop when a plate is crumpled and is pushed upwards to form mountain ranges. Orogeny is the mechanism by which mountains are built on continents. The word orogeny comes from Ancient Greek, though it was used before him, the term was employed by the American geologist G. K. Gilbert in 1890 to describe the process of mountain building as distinguished from epeirogeny. Formation of an orogen is accomplished in part by the processes of subduction or convergence of two or more continents. Orogeny usually produces long arcuate structures, known as orogenic belts, generally, orogenic belts consist of long parallel strips of rock exhibiting similar characteristics along the length of the belt. Orogenic belts are associated with zones, which consume crust, produce volcanoes. Geologists attribute the arcuate structure to the rigidity of the descending plate and these island arcs may be added to a continent during an orogenic event. The processes of orogeny can take tens of millions of years, frequently, rock formations that undergo orogeny are severely deformed and undergo metamorphism. Orogenic processes may push deeply buried rocks to the surface, sea-bottom and near-shore material may cover some or all of the orogenic area. If the orogeny is due to two continents colliding, very high mountains can result, an orogenic event may be studied, as a tectonic structural event, as a geographical event, and as a chronological event. The foreland basin forms ahead of the orogen due mainly to loading and resulting flexure of the lithosphere by the mountain belt. The basin migrates with the front and early deposited foreland basin sediments become progressively involved in folding and thrusting. Sediments deposited in the basin are mainly derived from the erosion of the actively uplifting rocks of the mountain range. The fill of many such shows an change in time from deepwater marine through shallow water to continental sediments. Although orogeny involves plate tectonics, the tectonic forces result in a variety of associated phenomena, including magmatism, metamorphism, crustal melting, what exactly happens in a specific orogen depends upon the strength and rheology of the continental lithosphere, and how these properties change during orogenesis. In addition to orogeny, the orogen is subject to other processes, for example, the Caledonian Orogeny refers to the Silurian and Devonian events that resulted from the collision of Laurentia with Eastern Avalonia and other former fragments of Gondwana. The Caledonian Orogen resulted from events and various others that are part of its peculiar orogenic cycle
11.
Spain
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By population, Spain is the sixth largest in Europe and the fifth in the European Union. Spains capital and largest city is Madrid, other urban areas include Barcelona, Valencia, Seville, Bilbao. Modern humans first arrived in the Iberian Peninsula around 35,000 years ago, in the Middle Ages, the area was conquered by Germanic tribes and later by the Moors. Spain is a democracy organised in the form of a government under a constitutional monarchy. It is a power and a major developed country with the worlds fourteenth largest economy by nominal GDP. Jesús Luis Cunchillos argues that the root of the span is the Phoenician word spy. Therefore, i-spn-ya would mean the land where metals are forged, two 15th-century Spanish Jewish scholars, Don Isaac Abravanel and Solomon ibn Verga, gave an explanation now considered folkloric. Both men wrote in two different published works that the first Jews to reach Spain were brought by ship by Phiros who was confederate with the king of Babylon when he laid siege to Jerusalem. This man was a Grecian by birth, but who had given a kingdom in Spain. He became related by marriage to Espan, the nephew of king Heracles, Heracles later renounced his throne in preference for his native Greece, leaving his kingdom to his nephew, Espan, from whom the country of España took its name. Based upon their testimonies, this eponym would have already been in use in Spain by c.350 BCE, Iberia enters written records as a land populated largely by the Iberians, Basques and Celts. Early on its coastal areas were settled by Phoenicians who founded Western Europe´s most ancient cities Cadiz, Phoenician influence expanded as much of the Peninsula was eventually incorporated into the Carthaginian Empire, becoming a major theater of the Punic Wars against the expanding Roman Empire. After an arduous conquest, the peninsula came fully under Roman Rule, during the early Middle Ages it came under Germanic rule but later, much of it was conquered by Moorish invaders from North Africa. In a process took centuries, the small Christian kingdoms in the north gradually regained control of the peninsula. The last Moorish kingdom fell in the same year Columbus reached the Americas, a global empire began which saw Spain become the strongest kingdom in Europe, the leading world power for a century and a half, and the largest overseas empire for three centuries. Continued wars and other problems led to a diminished status. The Napoleonic invasions of Spain led to chaos, triggering independence movements that tore apart most of the empire, eventually democracy was peacefully restored in the form of a parliamentary constitutional monarchy. Spain joined the European Union, experiencing a renaissance and steady economic growth
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