|
Montsec
The Montsec Range ( ca, Serra del Montsec ; es, Sierra del Montsec) is a mountain system of the Pre-Pyrenees. Description The Serra del Montsec consists of a series of calcareous mountain ranges running roughly from east to west. The range system is about 40 km long and 186.96 square kilometres in area. The Montsec is located in the Catalan province of Lleida and the Aragonese province of Huesca in Spain. Geography The name Montsec derives from the Latin ''Montus sectus'', which makes reference to its characteristic rock formations. It marks the southern limit of the Pallars region and is divided into three main massifs by 3 of the most important rivers in Catalonia: * Montsec de Rúbies, the eastern massif, is separated by the river Segre in the east and the Noguera Pallaresa in the middle, *Montsec d'Ares, the central massif. * Montsec d'Estall, in Aragon, located to the west, separated by the Noguera Ribagorçana from the central massif. Two gorges ''(con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montsec De Rúbies
The Montsec Range ( ca, Serra del Montsec ; es, Sierra del Montsec) is a mountain system of the Pre-Pyrenees. Description The Serra del Montsec consists of a series of calcareous mountain ranges running roughly from east to west. The range system is about 40 km long and 186.96 square kilometres in area. The Montsec is located in the Catalan province of Lleida and the Aragonese province of Huesca in Spain. Geography The name Montsec derives from the Latin ''Montus sectus'', which makes reference to its characteristic rock formations. It marks the southern limit of the Pallars region and is divided into three main massifs by 3 of the most important rivers in Catalonia: * Montsec de Rúbies, the eastern massif, is separated by the river Segre in the east and the Noguera Pallaresa in the middle, *Montsec d'Ares, the central massif. * Montsec d'Estall, in Aragon, located to the west, separated by the Noguera Ribagorçana from the central massif. Two gorges ''(congos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montsec D'Estall
The Montsec Range ( ca, Serra del Montsec ; es, Sierra del Montsec) is a mountain system of the Pre-Pyrenees. Description The Serra del Montsec consists of a series of calcareous mountain ranges running roughly from east to west. The range system is about 40 km long and 186.96 square kilometres in area. The Montsec is located in the Catalan province of Lleida and the Aragonese province of Huesca in Spain. Geography The name Montsec derives from the Latin ''Montus sectus'', which makes reference to its characteristic rock formations. It marks the southern limit of the Pallars region and is divided into three main massifs by 3 of the most important rivers in Catalonia: *Montsec de Rúbies, the eastern massif, is separated by the river Segre in the east and the Noguera Pallaresa in the middle, *Montsec d'Ares, the central massif. * Montsec d'Estall, in Aragon, located to the west, separated by the Noguera Ribagorçana from the central massif. Two gorges ''(congost ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montsec D'Ares
Montsec d'Ares is the central part of the Montsec mountain range, stretching between the cliffs of Montrebei in the West and Terradets in the East. Location La Serra del Montsec is located in the Catalan province of Lleida and in the Aragonese province of Huesca in Spain , image_flag = Bandera de España.svg , image_coat = Escudo de España (mazonado).svg , national_motto = ''Plus ultra'' (Latin)(English: "Further Beyond") , national_anthem = (English: "Royal March") , i .... The mountain "Montsec d'Ares" is perfectly oriented West - East. The highest point is "Santalis." Several villages are located in Montsec d'Ares, including as L'Ametlla del Montsec and Ager in the South side and Sant Esteve de la Sarga in the North. Mountain ranges of Aragon Mountain ranges of Catalonia {{Aragon-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pre-Pyrenees
The Pre-Pyrenees are the foothills of the Pyrenees. Description As a mountainous system the Pre-Pyrenees are part of the Pyrenees. They run parallel to the main mountain range in a west to east direction. On the French side the Pyrenees's slopes descend rather abruptly, thus on the northern side, the Pre-Pyrenees are confined to the Corbières Massif, towards the eastern end of the mountain system. The Massif de Plantaurel further west deserves mention as well, although not as clearly a foothill. On the Iberian side, however, the picture is very different: a large and complex system of foothill ranges stretches from Navarre, across northern Aragon, reaching the Mediterranean coast on the Catalan end of the Pyrenees. At the eastern end on the southern side lies a distinct area known as the Sub-Pyrenees. Main ranges Although the highest peaks in the Pre-Pyrenees are not as high as those in the Pyrenees proper, some of the ranges are quite massive, with summits reaching up to . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Pyrenees
The Pyrenees are a 430-kilometre-long, roughly east–west striking, intracontinental mountain chain that divide France, Spain, and Andorra. The belt has an extended, polycyclic geological evolution dating back to the Precambrian. The chain's present configuration is due to the collision between the microcontinent Iberia and the southwestern promontory of the European Plate (i.e. Southern France). The two continents were approaching each other since the onset of the Upper Cretaceous (Albian/ Cenomanian) about 100 million years ago and were consequently colliding during the Paleogene (Eocene/ Oligocene) 55 to 25 million years ago. After its uplift, the chain experienced intense erosion and isostatic readjustments. A cross-section through the chain shows an asymmetric flower-like structure with steeper dips on the French side. The Pyrenees are not solely the result of compressional forces, but also show an important sinistral shearing. Geographic arrangement The Pyrenees ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sant Alís
Sant Alís is the highest mountain of the Serra del Montsec in Catalonia, Spain. It has an elevation of 1,675 metres above sea level.. See also *Mountains of Catalonia This is a list of mountains in Catalonia, Spain. See also *Montserrat *List of mountains in Aragon References {{DEFAULTSORT:Mountains Of Catalonia Catalonia Mountains A mountain is an elevated portion of the Earth's crust, ... References Pre-Pyrenees Mountains of Catalonia One-thousanders of Spain {{Catalonia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pallars
Pallars is a historical and natural region of Catalonia. Located in the Pre-Pyrenees and Pyrenees area, most of its territory is mountainous. The Noguera Pallaresa river is named after this region. Geography The physiography of the Pallars natural region includes the Noguera Pallaresa river basin with its tributaries. The region encompasses as well as the mountain ranges spanning the Pyrenees and Pre-Pyrenees area that surround the basin until the Serra del Montsec which forms the limit of the Pallars at its southern end. Municipalities In present times the most important town of the Pallars is Tremp. Pallars Jussà Abella de la Conca, Castell de Mur, Conca de Dalt, Gavet de la Conca, Isona i Conca Dellà, Llimiana, La Pobla de Segur, Salàs de Pallars, Sant Esteve de la Sarga, Sarroca de Bellera, Senterada, Talarn, La Torre de Cabdella and Tremp. Pallars Sobirà Alins, Alt Àneu, Baix Pallars, Espot, Esterri d'Àneu, Esterri de Cardós, Farrera, La Guingue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Lleida
The Province of Lleida (; Aranese Occitan: Lhèida ; es, Lérida ) is one of the four provinces of Catalonia. It lies in north-eastern Spain, in the western part of the autonomous community of Catalonia, and is bordered by the Provinces of Girona, Barcelona, Tarragona, Zaragoza and Huesca and the countries of France and Andorra. It is often popularly referred to as Ponent (i.e. the West). Of the population of 414,015 (2007), about 30% live in the capital, Lleida. Some other towns in the Province of Lleida are La Seu d'Urgell (see the archbishop, who is also the co-prince to Andorra), Mollerussa, Cervera, Tàrrega, and Balaguer. There are 231 municipalities in Lleida. (See ''List of municipalities in Lleida.'') Located in the Pyrenees, the Aran Valley is a special comarca with greater autonomy and with Aranese, a variety of Occitan, as its official language. The Aigüestortes i Estany de Sant Maurici National Park is located in this province. The province enjoys a thrivin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Àger
Àger is a municipality in the ''comarca'' of the Noguera in Catalonia, Spain. It is situated in the north-west of the ''comarca'', and the territory of the municipality stretches between the Noguera Ribagorçana and Noguera Pallaresa rivers. The Terradets reservoir on the Noguera Pallaresa is situated within the municipality. The village is linked to Balaguer and Tremp by the L-904 road. Villages *Àger town, 317 inhabitants. *Agulló, 45 inhabitants. *Corçà, 32 inhabitants. * Fontdepou, 16 inhabitants. * Els Masos de Millà, 17 inhabitants. * Millà, 5 inhabitants. * La Règola, 21 inhabitants. * Sant Josep de Fontdepou, 19 inhabitants. *Vilamajor, 13 inhabitants. See also *Viscounty of Àger * ''Apostles from Àger'' *Montsec The Montsec Range ( ca, Serra del Montsec ; es, Sierra del Montsec) is a mountain system of the Pre-Pyrenees. Description The Serra del Montsec consists of a series of calcareous mountain ranges running roughly from east to west. The range syste .. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barley
Barley (''Hordeum vulgare''), a member of the grass family, is a major cereal grain grown in temperate climates globally. It was one of the first cultivated grains, particularly in Eurasia as early as 10,000 years ago. Globally 70% of barley production is used as animal fodder, while 30% as a source of fermentable material for beer and certain distilled beverages, and as a component of various foods. It is used in soups and stews, and in barley bread of various cultures. Barley grains are commonly made into malt in a traditional and ancient method of preparation. In 2017, barley was ranked fourth among grains in quantity produced () behind maize, rice and wheat. Etymology The Old English word for barley was ', which traces back to Proto-Indo-European and is cognate to the Latin word ' "flour" (''see corresponding entries''). The direct ancestor of modern English ''barley'' in Old English was the derived adjective ''bærlic'', meaning "of barley". The first citation of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caliphate Of Córdoba
The Caliphate of Córdoba ( ar, خلافة قرطبة; transliterated ''Khilāfat Qurṭuba''), also known as the Cordoban Caliphate was an Islamic state ruled by the Umayyad dynasty from 929 to 1031. Its territory comprised Iberia and parts of North Africa, with its capital in Córdoba. It succeeded the Emirate of Córdoba upon the self-proclamation of Umayyad emir Abd ar-Rahman III as caliph in January 929. The period was characterized by an expansion of trade and culture, and saw the construction of masterpieces of al-Andalus architecture. The caliphate disintegrated in the early 11th century during the Fitna of al-Andalus, a civil war between the descendants of caliph Hisham II and the successors of his '' hajib'' (court official), Al-Mansur. In 1031, after years of infighting, the caliphate fractured into a number of independent Muslim '' taifa'' (kingdoms). History Umayyad Dynasty Rise Abd ar-Rahman I became emir of Córdoba in 756 after six years in exile after t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
