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Sub-Pyrenees
The Sub-Pyrenees ( ca, Subpirineu) are a mountainous region in Catalonia, Spain, forming a section of the southern foothills of the Pyrenees. They are located at the eastern end of the Pre-Pyrenees, west of the Catalan Transversal Range, between the lower Ripollès and an area of the high Garrotxa. Description The Sub-Pyrenees consist of a series of parallel mountain ranges aligned in an east-west direction. Their shape is smooth and they are mostly covered with forest. They are cut transversally by the Ter River, between the Sant Amand (1,851 m) anticline and Bellmunt (Sant Pere de Torelló), Bellmunt (1,515 m), the mountain massif rising over the Plain of Vic. The term ''Subpirineu'' was first used in 1938 by Catalan geographer and geologist Lluís Solé. He justified the separateness of the Sub-Pyrenees from the Pre-Pyrenees and the Transversal Range on the basis of the material composition of the mountains, as well as the relatively more recent character of the anticline and ...
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Osona
Osona () is a comarca situated in Catalonia, Northeast Spain. Its capital is Vic. Its population in 2001 was 129,543. Osona covers roughly the same area as the historic Catalan county of Osona. The name Osona comes from ''Ausetans'', a group of Iberian people who had their capital in ''Ausa'' (today Vic); the Romans called the area ''Ausone'' or ''Ausona''. While most of the ''comarca'' is within the province of Barcelona, the municipalities of Espinelves, Vidrà and Viladrau form part of the province of Girona. The most important town of Osona is Vic, its capital and an important and ancient urban center in this natural region that lies in the midst of the Plain of Vic. Other significant towns in the plain are Manlleu and Tona. This natural depression in the center of the region was carved by river Ter and its tributaries and makes up a big part of Osona's land. It is surrounded by mountains: The Sub-Pyrenees, with Bellmunt mountain towering in the north, the Lluçanès (Pr ...
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Bellmunt (Sant Pere De Torelló)
Bellmunt (Sant Pere de Torelló) is a mountain of Catalonia, Spain. It has an elevation of 1,246 metres above sea level.. This mountain dominates the landscape of the Plain of Vic. See also *Sub-Pyrenees *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 Mountains of Catalonia Emblematic summits of Catalonia {{Barcelona-geo-stub ...
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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 . ...
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Catalan Transversal Range
The Catalan Transversal Range (''Serralada Transversal'') is a system of minor mountain ranges at the eastern end of the Pre-Pyrenees, between the Osona and Garrotxa comarques. The existence of the Catalan Transversal Range has made communications in the northern areas of Catalonia difficult in the past, especially between Northeastern Catalonia ( Catalan Coastal Depression, with cities like Girona, Figueres and La Jonquera) and Western Catalonia ( Catalan Mediterranean System; Lleida, Cervera and further west to Aragón), a problem that has been partly solved with the development of the Eix Transversal. Description The Catalan Transversal Range is made up of a series of mountains running in a NW / SE axis between the Pyrenees, the Sub-Pyrenees, the Catalan Pre-Coastal Range and the northern end of the Catalan Coastal Depression. The highest point is at Puigsacalm, 1.515 m. Its most characteristic feature is a small region of volcanic origin near Olot, Garrotxa. There are ...
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Plain Of Vic
The Plain of Vic (Catalan ''Plana de Vic'') is a 30 km long depression located at the eastern end of the Catalan Central Depression in the Osona comarca. It is named after the town of Vic, an important and ancient urban center in this natural region that lies in the midst of the plain. Other significant towns in the plain are Manlleu and Tona. This natural depression carved by river Ter and its tributaries is longer than it is wide and stretches in a N / S direction. It is completely surrounded by mountains: The Sub-Pyrenees, with Bellmunt mountain towering in the north, the Lluçanès ( Pre-Pyrenees) and Moianès high plateau in the West, the Montseny in the southeast and the Guilleries, located at the apex of the Catalan Transversal Range and the Pre-Coastal Range, in the east. Characteristics The Plain of Vic was the bed of an ancient sea. It is mainly formed by sedimentary rocks, like carbonatic lutite, from the eocene. The most remarkable characteristic of the la ...
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Sant Amand
Sant Amand or Puig de Sant Amand is a mountain of Catalonia, Spain. It has an elevation of 1,851 metres above sea level.. See also *Sub-Pyrenees *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 Mountains of Catalonia One-thousanders of Spain {{Catalonia-geo-stub ...
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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 ...
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Pyrenees
The Pyrenees (; es, Pirineos ; french: Pyrénées ; ca, Pirineu ; eu, Pirinioak ; oc, Pirenèus ; an, Pirineus) is a mountain range straddling the border of France and Spain. It extends nearly from its union with the Cantabrian Mountains to Cap de Creus on the Mediterranean Sea, Mediterranean coast. It reaches a maximum altitude of at the peak of Aneto. For the most part, the main crest forms a divide between Spain and France, with the microstate of Andorra sandwiched in between. Historically, the Crown of Aragon and the Kingdom of Navarre extended on both sides of the mountain range. Etymology In Greek mythology, Pyrene (mythology), Pyrene is a princess who eponym, gave her name to the Pyrenees. The Greek historiography, Greek historian Herodotus says Pyrene is the name of a town in Celts, Celtic Europe. According to Silius Italicus, she was the virgin daughter of Bebryx, a king in Narbonensis, Mediterranean Gaul by whom the hero Hercules was given hospitality during his ...
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Ripollès
Ripollès (; es, link=no, Ripollés) is a comarca (county) in Catalonia, Spain. It is located in the Ribes and Camprodon river valleys. In 2001, its population was 25,744, about 40% of whom lived in the capital, Ripoll. Ripollès borders the comarques of Baixa Cerdanya, Berguedà, Osona, Garrotxa, and – across the border in France – Vallespir, Conflent, and Alta Cerdanya. Municipalities See also *Sub-Pyrenees The Sub-Pyrenees ( ca, Subpirineu) are a mountainous region in Catalonia, Spain, forming a section of the southern foothills of the Pyrenees. They are located at the eastern end of the Pre-Pyrenees, west of the Catalan Transversal Range, betwe ... References External linksOfficial comarcal web site (in Catalan and Spanish) {{DEFAULTSORT:Ripolles Comarques of the Province of Girona Pyrenees ...
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Garrotxa
Garrotxa () is a comarca (county) in Girona, Catalonia, Spain. Its population in 2016 was 55,999, more than half of them in the capital city of Olot. It is roughly equivalent to the historical County of Besalú. Geography Garrotxa borders the comarques of Ripollès, Osona, Selva, Gironès, Pla de l'Estany, Alt Empordà, and Vallespir. It includes the upper basin of the River Fluvià and the headwaters of the rivers Muga, Amer and Llémena. From both the human point of view and that of physical geography, the comarca has a clear division into two subcomarques. Extending north from the valley of the Fluvià, is Alta Garrotxa (Upper Garrotxa), while the southern part is sometimes called the comarca of Olot, after the capital city. The Fluvià flows toward the Mediterranean, and has a relatively small flow of water (1.07 m³/s at Olot). The high humidity of Garrotxa contrasts with that of the neighboring comarques. Annual rainfall is over 1000 mm (about 40 inches ...
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Anticline
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used. The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper st ...
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Lluís Solé
Lluís Solé i Sabarís (May 18, 1908 - July 14, 1985) was a Spanish educator and geographer. Life Born in the city of Gavà, Solé's family moved to Lleida when he was still young. In 1926, he met Pau Vila, through whom he discovered geography, and graduated from the University of Barcelona in Natural Sciences three years later. In 1935, he helped found the Catalan Society of Geography, of which he was president from 1972 to 1981. Solé went on to study paleontology in Germany, and wrote about the subject for his doctorate in 1936. Solé devoted his life to teaching, and after the Spanish Civil War, he became chair of Physical Geography at the University of Granada. In 1943, he became a faculty member of the University of Barcelona, where he was the Professor who led the department of Geography. Carmina Virgili was one of his assistants.
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