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Txindoki

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Txindoki or Larrunarri is an iconic mountain (1,346 m) located in the region of Goierri , Gipuzkoa , in the Basque Autonomous Community of Spain . Originally Larrunarri or Ñañarri ( Basque pronunciation: [ɲa'ɲari] ), the mount took on the popularized name Txindoki by extension after some shepherd huts nearby. It is sometimes referred to as the Basque Matterhorn too, because of its pyramidal shape.

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36-576: It stands out as the westernmost mountainous tip of the Aralar mountain range, with an easily recognized image that has become a symbol for all the Goierri valley. The towering mountain stands above the northern town Amezketa and its scattered farmhouses at its foot. For the most part, it is not covered in forest just like most of the Gipuzkoan side of Aralar . The steep slopes of the northern face and

72-402: A karstic lithological appearance, i.e. parts of the calcareous ( calcium carbonate , limestone) rock outcrops have been dissolved away in water. Left behind are limestone pavements—areas where the limestone has formed etched, pitted or fluted rock pinnacles and ridges between which are deep grooves, sinkholes or dolinas, caves, underground rivers, and gullies. An example, now open to

108-702: A cheerful environment, with numerous public, traditional music ( trikitixa ) enlivening the atmosphere and stalls featuring rural produce, e.g. cider and cheese, as well as crafted products. In 2008 18,000 sheep, 650 mares and 700 cows were expected to follow the seasonal migration to Aralar . On June 29, Saint Peter's day, a big and popular religious celebration is held at the hermitage (a gathering called erromeria in Basque ). 43°01′26″N 2°05′13″W  /  43.02389°N 2.08694°W  / 43.02389; -2.08694 Aralar Mendilerroa The Aralar Range ( Basque pronunciation: [aˈɾalar] )

144-427: A convenient and gentle stroll, until a winding slope is overcome some minutes before the turning of the crest (milestone Gazteraztegi, 520 m). There a broad track sets off back in the opposite direction, going up until it gets to an aerial at Urtzabal goikoa (610 m). Alternatively, a short-cut heads up cross-country straight on to the aerial from Larraitz, so gaining height in little time but with some effort. Right before

180-520: A local mythology of legends, folk beliefs and tales, which is dependent on the nature of the landscape has emerged. The ethnographer and historian, José Miguel de Barandiarán, was born in the local town, Ataun. Also called 'Aralarko San Migel Santutegia' and 'Santuario de San Miguel de Aralar' in Spanish, San Miguel is a Romanesque church located in the southern part of the range near the town of Uharte-Arakil and Mount Altxueta (1343m). Records about

216-400: A postbox for hikers. Alternatively, the hard way up can be taken at the spring Oria by heading east out of the main trail through a tough grassy slope that ends up at the col of Egurral. Another option consists of starting off from Larraitz with a view to ascending through the northern wild valley of Muitze, unknown to most hikers. This time the same track may be followed in the beginning for

252-468: A visitor centre marks the park's main entrance. It operates in the former miquelete (Gipuzkoan military police) barracks. The Aia hamlet (access via Aia road, NA120) nestles on the southern slopes of the range. The range is mountainous with large limestone massifs (formations resulting from movement of the Earth's crust into faults and flexures). This is typical of the Basque region . The range has

288-596: Is a mountain range in the Basque Mountains of the Southern Basque Country . The part of the range lying in Gipuzkoa was established as a conservation area called Aralar Natural Park in 1994. In addition to its natural features, scenery, recreational use and habitation, the range is home to a number of Basque mythology milestones and legends. The Basque word, 'Aralar' may stem from

324-604: Is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny . Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics . Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets . Mountain ranges are usually segmented by highlands or mountain passes and valleys . Individual mountains within

360-468: Is a simple fascia and no capitals. The church has three apses at the atrium, three barrel vaulted naves and a central polygonal dome. The altar front, featuring Our Lady, is enamelled. Nearby, in a grotto, there is a 12th-century shrine to San Miguel. Legend holds that in a case of mistaken identity a crusader knight, the lord Teodosio of Goni, accidentally killed his own parents. In penance, he chained himself alone on Mount Aralar. An apparition dedicated to

396-538: Is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet (3,000 m) of mostly Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to

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432-419: Is the most widely known and visited peak in the range. The peak is called "Little Cervine" and the mountain itself, the 'Basque Matterhorn'. Tower of Intza , also called “Irumugarrieta”, is the highest mountain of the range. Mountain range A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt

468-865: The Alpide belt . The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera , the Aleutian Range , on through Kamchatka Peninsula , Japan , Taiwan , the Philippines , Papua New Guinea , to New Zealand . The Andes is 7,000 kilometres (4,350 mi) long and is often considered the world's longest mountain system. The Alpide belt stretches 15,000 km across southern Eurasia , from Java in Maritime Southeast Asia to

504-551: The Annamite Range . If the definition of a mountain range is stretched to include underwater mountains, then the Ocean Ridge forms the longest continuous mountain system on Earth, with a length of 65,000 kilometres (40,400 mi). The position of mountain ranges influences climate, such as rain or snow. When air masses move up and over mountains, the air cools, producing orographic precipitation (rain or snow). As

540-804: The Iberian Peninsula in Western Europe , including the ranges of the Himalayas , Karakoram , Hindu Kush , Alborz , Caucasus , and the Alps . The Himalayas contain the highest mountains in the world, including Mount Everest , which is 8,848 metres (29,029 ft) high. Mountain ranges outside these two systems include the Arctic Cordillera , Appalachians , Great Dividing Range , East Siberians , Altais , Scandinavians , Qinling , Western Ghats , Vindhyas , Byrrangas , and

576-860: The Karst geological forms, some waterways are underground . The waterways contribute to the economy of the region, for example, in the production of hydroelectric power. The Basque region, generally, has a temperate oceanic climate. The climate of the Aralar range transitions between the Eastern Cantabrian climate of Gipuzkoa and the Continental-Mediterranean climate of the Barranca corridor ( Navarre ). The mountains, however, do create their own micro-climate with more intense rainfall and greater cloud cover. Mists can make hiking in

612-475: The Muitze valley are the wild part of Txindoki. The northern and southern side are clearly delimited by a rocky limestone crest running east to west up to the summit, which is almost entirely bare rock. The steep sides of the crest are popular with amateur rock climbers. The main and most popular access point is from the neighbourhood Larraitz ( Basque pronunciation: [la'raits] ). From Alegia (N-1)

648-627: The air descends on the leeward side, it warms again (following the adiabatic lapse rate ) and is drier, having been stripped of much of its moisture. Often, a rain shadow will affect the leeward side of a range. As a consequence, large mountain ranges, such as the Andes, compartmentalize continents into distinct climate regions . Mountain ranges are constantly subjected to erosional forces which work to tear them down. The basins adjacent to an eroding mountain range are then filled with sediments that are buried and turned into sedimentary rock . Erosion

684-589: The archangel Michael appeared and released him. The apparition left an image, a figure with a glass (or crystal) head and face and a helmet adorned with a cross. The image was disfigured by the French in 1797. In the park there is also the Our Lady of Remedios Hermitage. There are a number of trails, landmarks and unique destinations in the ranges. The karst features are suitable for caving. Between May and November, livestock, especially latxa sheep which provide

720-583: The church date from the 11th century (1032) and it contributes to the history of Christianity in northern Spain—San Miguel is an iconic and one of the oldest saints of the Basques. The chapel was built by the lord of Goñi and consecrated 1098. However, there was an earlier 9th century structure on the same site in the Carolingian style. After a fire in the 10th century, the church was rebuilt with two aisles. The pillars are cruciform (one round). There

756-485: The east. This mass of rock was removed as the range was actively undergoing uplift. The removal of such a mass from the core of the range most likely caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment. Computer simulation has shown that as mountain belts change from tectonically active to inactive,

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792-539: The element of ruggedness of the range. Two examples are the Txindoki relief and the Ataun dome structure. Sandstone is found to the north and south of the range. Glaciated areas with small frontal moraines at one to two km from the cirque have been found. Many streams originate in the range. Between the peaks, there are four large basins: Agauntza , Zaldibia , Ibiur and Amezketa in which streams can form. Due to

828-403: The final slope to the aerial, a narrow path bounds south-east on the left into the tough and vertical valley carved by the stream Muitze (waterfalls on the way). The trail snakes out of the forest to the right and crosses the stream at the point where the forest landscape gives way to grassland. After overcoming the rocks, the stream must be crossed again to the right. A trail on the steep slopes on

864-433: The huts of Zirigarate are reached, which stand on a hollow. From Zirigarate, the trail heads east to the col of Egurral (1,152 m), the last milestone before the final struggle to the summit largely through karst terrain (1h45). On sunny Sundays of Summer and Spring people walk in droves to the top. Breathtaking scenery from the peak all over Gipuzkoa and Aralar on a clear day. The summit is covered with small memorials and

900-436: The milk for Idiazabal cheese, dairy cattle and a herd of wild horses, graze in the park's public pastures. Although the ranges are generally uninhabited, some people of Aralar follow a nomadic life, tending their animals. Through the summer months, the sheep graze in the higher terrain. Pastoral huts have been built in these areas for shepherds. The animals winter near the villages. Approximately 5112 people live in villages in

936-568: The minor road GI-3670 that switches to the GI-2133 in the last stretch reaches Larraitz in about 15 minutes; alternatively, it can be reached by taking the GI-2133 starting in Ordizia (N-1 E-05 E-80), taking about the same time. Larraitz, lying at 403 m (943 m below the summit), harbours the long picnic area and car park Zamao , with a couple of café-restaurants (former farmhouses) and a hermitage (17th century) all surrounded by gentle fields. From

972-466: The park more dangerous. Megalithic monuments indicate prehistoric habitation of the range. These monuments include tumuli , stone circles and menhirs . There are 17 on the Gipuzkoan side and 44 on the Navarrese side of the range. Archaeological evidence suggests Neolithic pastoralism. For example, primary forests, now restricted to the fringes of the range have been replaced by pastures. Also,

1008-474: The public, is the cavern of Mendukillo in the village of Astitz . This cracked, permeable geologic milieu has provided the perfect grounds for a wide range of mythological accounts and characters. The materials that dominate are clay , marl , sandstone and limestone . Except for quaternary period coatings, all the materials are from the Jurassic and Cretaceous eras. The original limestone reefs create

1044-501: The range include griffons , Egyptian vultures , golden eagles , and bearded vultures , Alpine choughs , wood pigeons and black woodpeckers . The range is known for its beech forests. In times past, beech pollards have been used to make charcoal. There are also groves of rowan and hawthorne and Cantabrian holm oak. This plateau feature is created by the peaks of Jentilbaratza, Aizkoate, Aizkorrandi, Arastortz, Agautz, Leizadi, Asundi, Loibideko Mailoak and Ikarandieta. Txindoki

1080-465: The range; Abaltzisketa (290), Amezketa (1075), Ataun (1822), Zaldibia (1696) and Bedaio (229). They work in agriculture, in industries in larger towns and in tourism. Animals of the range include European mink , roe deer , wild boar and various small and medium mammals such as Pyrenean desmans and the European snow voles . There are amphibians such as the alpine newts . The varieties of birds of

1116-627: The rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System, including the Moon , are often isolated and formed mainly by processes such as impacts, though there are examples of mountain ranges (or "Montes") somewhat similar to those on Earth. Saturn 's moon Titan and Pluto , in particular, exhibit large mountain ranges in chains composed mainly of ices rather than rock. Examples include

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1152-490: The right leads to the hut Txindoki and an orchard that provided the current name to the mountain. Legend has it, close to this place the mythological character/goddess Mari dwells in a crack on the rock (Marizulo). By clinging to the steep path, the pass of Egurral is reached (1h45). Every year on 1 May, flocks of cattle are gathered in Larraitz to be herded to the highland grasslands until October. The meeting takes place in

1188-479: 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, and volcanic landforms resulting in a variety of rock types . Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or

1224-469: The southern end of the area, a broad dust track heads south-west, forking shortly afterwards with the left hand track leading to Txindoki. The broad track peters out into a beaten trail that turns east at the lower end of the crest (15 min). Next, it cuts its way straight across the southern side of the mountain along a pine tree plantation on the right till the spring Oria is reached at a sharp bend. After some zigzag and steep slopes heading south-west (1h00),

1260-523: The two provinces. Pamplona lies approximately 40 kilometres (25 mi) to the south east. The Spanish coastline at the Cantabrian Sea (the southern Bay of Biscay ) and the town of San Sebastian are approximately the same distance to the north north-east. The border between Spain and France is approximately 50 kilometres (31 mi) to the north-east. Villages located at the foot of the range include Beasain , Arbizu and Ataun. At Lizarrusti,

1296-480: The words '(h)aran', meaning 'valley' and 'larre', meaning 'graze-land'. In Spanish , the range is also called Sierra de Aralar . The range covers 20,800 hectares (208 km ). 10,971 hectares (109.71 km ) is conservation area. The range is located in the Basque Country of northern Spain, straddling the boundaries of south-eastern Gipuzkoa and north-western Navarre . The range effectively separates

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