[{"@context":"http:\/\/schema.org\/","@type":"BlogPosting","@id":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/valleee-du-gesso-wikipedia\/#BlogPosting","mainEntityOfPage":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/valleee-du-gesso-wikipedia\/","headline":"Valle\u00e9e du Gesso \u2014 Wikipedia","name":"Valle\u00e9e du Gesso \u2014 Wikipedia","description":"before-content-x4 The the floor valley (an Italy Gesso valley , in Occitan Choices are given ), is a valley of","datePublished":"2017-05-01","dateModified":"2017-05-01","author":{"@type":"Person","@id":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/author\/lordneo\/#Person","name":"lordneo","url":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/author\/lordneo\/","image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/44a4cee54c4c053e967fe3e7d054edd4?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/44a4cee54c4c053e967fe3e7d054edd4?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"Enzyklop\u00e4die","logo":{"@type":"ImageObject","@id":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","url":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/thumb\/2\/23\/Vallegesso.png\/220px-Vallegesso.png","url":"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/thumb\/2\/23\/Vallegesso.png\/220px-Vallegesso.png","height":"167","width":"220"},"url":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/valleee-du-gesso-wikipedia\/","wordCount":9481,"articleBody":"     (adsbygoogle = window.adsbygoogle || []).push({});before-content-x4The the floor valley (an Italy Gesso valley , in Occitan Choices are given ), is a valley of the Italian Piedmont formed by the vast gesso basin, strongly shaped by the action of the glaciers [ first ] .        (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4It is located in the province of Coni, in the portion of the Massif des Alpes Maritimes where its highest peaks are located (Mont Argentera, 3,297 m ). Geographically, it constitutes the hinge between two sections of the massif perpendicular to each other, since in the North is the Stura di Demonte valley from a north-south crest line, and in the east the Val Vermenagna from An East-West ridge line. To the south are the Tin\u00e9e, V\u00e9subie and Roya valleys, in the French department of the Alpes-Maritimes. The length of the valley is around 25 km , from the border ridge to the P\u00f4 plain which it reaches in Borgo San Dalmazzo. Its territory is divided, from upstream to downstream, between the municipalities of Entecque, Valdieri, Roaschia and Roccavione.          (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4Table of ContentsGeomorphology [ modifier | Modifier and code ] Floor dues from the valslet [ modifier | Modifier and code ] Vall\u00e9e du plaster [ modifier | Modifier and code ] Orography [ modifier | Modifier and code ] Cols [ modifier | Modifier and code ] antiquity [ modifier | Modifier and code ] Middle Ages [ modifier | Modifier and code ] Modern era [ modifier | Modifier and code ] Contemporary period [ modifier | Modifier and code ] Language [ modifier | Modifier and code ] Manifestations [ modifier | Modifier and code ] Museums [ modifier | Modifier and code ] gastronomy [ modifier | Modifier and code ] Industry [ modifier | Modifier and code ] Energy [ modifier | Modifier and code ] Tourism [ modifier | Modifier and code ] Geomorphology [ modifier | Modifier and code ]  Geomorphological diagram of the Gesso valley: Crest lines: orange Valley Fund: Blue Hall centers: black Due to its position inside the curvature of the Alps, the valley has a fairly complex configuration. The bottom of the valley has a series of successive ramifications, separated by secondary crests of considerable dimensions: for example, the crest that separates the Meris valley of Valasco valley culmine Au Monte Matta to Presque 3 100 m d’altitude. Starting from the outlet of the valley, near Borgo San Dalmazzo and the confluence with the Vermenagna torrent, the valley goes up to the southwest.        (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4To Mi-Cemin ento Borgo San Dalmazzo and Valdieri, the Roaschia valley , where the village of the same name is located, stands out towards the Southeast. The main valley exceeds Valdieri, still in the southwest, and branches off after a few kilometers: a continuous branch towards the southwest under the name of Valle Gesso della Valletta , and another south-east under the name of valley chalk of Entracque . Until this branch, the bottom of the valley is very wide. Floor dues from the valslet [ modifier | Modifier and code ] It is the valley which, since the branch, continues to the southwest. The valley shrinks a lot and, near Sant’anna di Valdieri, it takes almost a throat character. At the height of Sant’anna di Valdieri, he stands out the west the Meris valley lakes of the saddle , where is the Dante Livio Bianco refuge. The Gesso Della Valletta valley continues to the southwest, still cashed. A little upstream of Sant’anna di Valdieri, he stands out to the southeast the valley of the mine , which rises towards the top of the Asta Soprana.  The Pian del Valasco in the valley of the same name. The valley joins the Terme di Valdieri , where it widens again and has new branches. A little downstream of the thermal baths, the Vallone of Lourousa leaves south-east and climbs to Passo del Chiapous , enter the Argentine and the Soprana auction, et ouss Duquel if I Neu Negreg Mathet-Buughs. From the thermal baths, the Valasco valley Share west then the southwest, passing by the old royal hunting house (today refuge Valasco), and finally joining the lake of Valscura and the lake doors Where is the Questa refuge. The Gesso Della Valletta valley turns south from the thermal baths, taking the name of Valletta valley , and she goes up to the crest of waters’ sharing with France; At the bottom of the valley is the Regina Elena refuge. On the east side, several valleys stand out, from the general west-east direction and going back to the Cr\u00eate de l’Argentera, among which: the Valley of the Argentera Where is the Bozano refuge; the VALLONE ASSEDRAS Where is the Remondino refuge. Vall\u00e9e du plaster [ modifier | Modifier and code ] It is the valley which, since the branch a little upstream of Valdieri, goes back to the south-east, soon joining the village of Ent\u00e9cque where it branches off. The main valley turns south-southwest, exceeds the lake plate , artificial basin created by an Enel dam, and joins the locality Ponte delle Ruine where there is a new bifurcation.The Valle delle Ruine leaves southwest to lake of ruin , to the highs of 1 535 m ; From there, the bottom of the valley goes back in steep slope to the lake del particilous , artificial basin created by the Enel by means of two dams, and at Lake Brocan next to him. The Genova-Figari refuge is between the two lakes.From there goes to the north-northwest another small valley, the Chiapous valley , who goes up to Passo del Chiapous by reaching the bottom of Vallone of Lourousa . From the Ponte delle Ruine , the main valley takes the name of Valle Gesso della Barra And continues south for a few kilometers to the hamlet of San Giacomo, where there is a new bifurcation.The main valley continues to the southwest towards the sharing of waters with France and the Cime du G\u00e9las, at the foot of which is the Soria Ellena refuge, and reaches the Fenestre pass. The Vallone di Monte Colombo stands out towards the east, then takes the southern south-south-east direction and rises towards the pea of \u200b\u200bthe Mal\u00e9die; At the bottom of the valley is the Pagar\u00ec refuge. The Bousset valley continues on the other hand from Entracque to the south-east in a large valley for several kilometers, to the place called gias d’Ischietto where she has a branch:the Vallone dell’Amblto is a secondary valley that goes south, the Vallone del Sabbione Part east, soon turns south and then the south-south-east at the foot of La Roche de l’Abisse in the direction of water sharing with France, which he reached at the Sabion pass. Orography [ modifier | Modifier and code ] Due to its morphology, the valley is rich in crests and lines of internal waters, in addition to those which separate it from the surrounding valleys.  Mount Malinvern seen from the red earth lakes.  The most important crest due to its dimensions is the border crest that separates the Gesso valley from France. There are several remarkable altitude peaks such as, from west to east, on the water sharing line with the Tin\u00e9e: On the water sharing line with V\u00e9subie: On the water sharing line with the Gordolasque, tributary of V\u00e9subie: On the watershed with the Roya: CIMES DES LACS DE L’AGNEL – 2,852 m , Cime de Vernasque – 2 849 m , Cime Scandailli\u00e8re ( Top of the scandiniera ) – 2 705 m , SABION CIME – 2 610 m , Roche de l’Abisse – 2,755 m . The water sharing line with the Stura di Demonte valley, which delimits the Gesso valley in the northwest, starts from Mount Malinvern; there is a descendant, following the east side of the Riofreddo valley from the Stura valley: THE Peaks of Valrossa – 2 909 m For the highest, Rocca la our – 2 972 m , Rocca Pan Voud – 2 956 m ; Then on the northern crest of Meris valley : Cima Gorgia Cagna – 2 718 m , Monte Vintabren – 2 611 m , Monte Bourel – 2 468 m .  The central summit of Monte Matto . Important vertices are also present on the internal water sharing lines at the Gesso Valley. Starting from the previous water sharing line at the Rocca la our , the southern crest of Meris valley separates it from Valasco valley and the Gesso Della Valletta valley, and it is found there by going east towards the outlet of Meris valley To St. Jatherine: Rocca di Valmiana – 3 006 m , Monte Matto With its four points – 3,097 m For the highest, Cima del Latoous – 2 744 m .  Creater from Argentine du Star horn to the Cima di Nasta . In the foreground, the Mother of God .  The Star horn seen from the southeast. Further east, starting from the Guili\u00e9 peaks (2,999 m ), the ridge between the valleys of the Gesso della Valletta and the Gesso di Entracque, characterized by the highest peak of the Massif des Alpes Maritimes, will also argue, presents by following it downstream: Brocan pea – 3,054 m , Cima of the baus – 3 067 m , Cima di Nasta – 3 108 m , Cima Paganini – 3 051 m , On a secondary crest that goes west:Cessole tip – 2 915 m , Mother of God – 2 800 m , Mont will argue with its two summits – 3,297 m South pea, 3,286 m north peak, Punta Glass in Lourousa – 3 261 m ,on a secondary crest that starts from the latter to the northwest, Star horn – 3 050 m , Monte Stella – 3 262 m ; Then beyond the Colle del Chiapous : Monte Oriol – 2 943 m , and the group of Week that he forms with the secondary crest which in the northwest:Cima Mondini – 2 915 m , That soprano – 2 948 m , Sottana rod – 2 850 m , Cima della Vagliotta – 2 548 m , Cima del Lausetto – 2 687 m . A little further east, on the water sharing line between the Valle della Ruine and the Valle Gesso della Barra , which starts from the peak of Agnel (2,927 m ), we find in descend: Pointe de la Vallette – 2,848 m , Punta Fenestrelle – 2 701 m , Punta Ciambberline – 2 792 m , Punta Laura – 2 601 m , Cima della Valletta – 2 549 m . Always further east, on the watershed between the Valle Gesso della Barra and the Vallone di Monte Colombo , which starts from the Cime du G\u00e9las (3,143 m ), we find : Punta della Siula – 2 672 m . Even further east, the watershed between the Valle Gesso della Barra and the Bousset valley Part of the Cime de Vernasque (2 849 m ); There is going down: another one Cima della Valletta – 2 787 m , Monte Carbon\u00e8 – 2 873 m , Savina tip – 2 821 m , Tip of the baus – 2 779 m , Punta della Rua – 2 779 m , Mount Aiera – 2 713 m . Finally, the watershed with the Val Vermenagna, which delimits the Gesso valley to the East, starts from the Roche de l’Abisse (2,755 m ); It is found there by going downstream: Monte Colombo – 2 261 m , Monte Pianard – 2 306 m , Mount her bushesia – 2 451 m . Cols [ modifier | Modifier and code ] Nowadays, the valley does not have carriage passes. The main passes accessible on foot which connect the Gesso valley to the neighboring valleys are, from the west to the east: To the Riofreddo valley In the Stura di Demonte valley:Valscura collar – 2 520 m . Towards the Tin\u00e9e Valley:drop in druos – 2,628 m , no porters – 2,598 m , No prefouns – 2,620 m , Fr\u00e9mamorte cabbage – 2 615 m . Towards the Bor\u00e9on valley which joins the V\u00e9subie valley:cherry collar ( Colle di Ciriegia ) – 2 543 m , col de la ruins ( passage of the ruin ) – 2 724 m . Towards the V\u00e9subie valley in the Madonna of Fenestre valley:Fenester cabbage – 2 474 m . It is at the bottom of Valle Gesso della Barra south of Entracque; You can reach the pass through the M11 trail [ 2 ] . In the past, the pass played a very important communication role, on the route of the Salt Route between the Pla plain and the Ligurian Sea. On the other side is the sanctuary of the Madonna of Fenestre, attested from the WE It is century, where travelers could resume their strength, and the Madonna of Fenestre valley at the outlet of which is the village of Saint-Martin-V\u00e9subie. Towards the Vallon de Casterino which joins the Roya Valley:Col du Sabion – 2,328 m . It opens at the bottom of Vallone del Sabbione ; It can be achieved by M5 and M23 trails [ 2 ] . Via the Valmasque valley above the Vallon de Casterino, it is also an access to the Valley of Wonders. Towards the hamlet of Palanfr\u00e8 in Val Vermenagna:Passo della Mena or colle Frisson – 2 197 m , Colle della Garbella – 2 170 m . Given the orographical and morphological particularities of the valley, there are also many interior passes which put in communication the various branches of the main valley. The main ones are, overall from west to east: between the Meris valley and the Valasco valley : Colle della Dello – 2 890 m , Colle di Valmiana – 2 922 m , between the Valasco valley and the Valletta valley : Colle di Valasco – 2 429 m , enter here Valletta valley and the Valle della Ruine : not Brocan – 2,892 m , passage of debris – 3 122 m , between the Vallone of Lourousa and the valley of the mine : passage of the nodal point – 2 850 m , between the Vallone of Lourousa and the Chiapous valley : Colle del Chiapous – 2 526 m , enter here Valle della Ruine and the Valle Gesso della Barra : Colle di Fenestrelle – 2 463 m , enter here Valle Gesso della Barra and the Valley of Monte Colombo : Passage of Gel\u00e0s glaciers – 2 750 m , enter here Valley of Monte Colombo and the Vallone del Sabbione : Colle del Vei del Bouc – 2 620 m , enter here Valley of Monte Colombo and the Vallone dell’Amblto : Ste carbonary passes – 2 730 m , enter here Valle Gesso della Barra and the Bousset valley : Passo di Valle Steira – 1 515 m , between the valley chalk of Entracque and the Roaschia valley : Passo del from – 1 761 m . antiquity [ modifier | Modifier and code ] The Gesso valley was probably inhabited from the pre -Roman era by the Apuani ligues ( Liguri Montani ), defeated and subject by the Romans in 14 of. J.-C. [ 3 ] . The valley presented at the time a considerable strategic and commercial interest, due to the presence of the Way of the Fenestre Col (Salt Road), an important communication route between the coast and the P\u00f4 plain even cited by the Greek geographer Straw [ 4 ] . The Gesso valley was gathered at the municipality of Pedona (now Borgo San Dalmazzo), and it probably built Roman colonies there [ 4 ] , [ 3 ] . Christianity began to enter the valley towards the middle of III It is century, with the preaching of Saint Dalmas de Pedona. Middle Ages [ modifier | Modifier and code ] Around the year 600 arrived from the Benedictine monks which founded the Abbey of Pedona, and the latter took control of all the lands of the valley [ 3 ] , [ 4 ] . In 901, the emperor Louis III donated the abbey and the lands dependent on it to the bishop of Asti [ 3 ] , [ 4 ] . At that time, the valley was the target of Sarashic incursions [ 4 ] . At XIII It is century, after being briefly remained under the control of the Marquisat of Saluces, the valley passed under the lordship of the Anjou, who had created a county in Piedmont with Coni for chief town [ 4 ] , [ 3 ] . It is roughly during this period that the villages of the valley constitute themselves in free municipalities; They recognize the jurisdiction of Pedona Abbey, but enjoy wide freedom and autonomy [ 3 ] , [ 4 ] , [ 5 ] , [ 6 ] . At XIV It is century, the valley passed under the control of Am\u00e9d\u00e9e VI of Savoie, the “Count Vert”, which gave it in fief to the Marquis Carlo di Ceva in 1373 [ 4 ] , [ 3 ] . The valley returned under the direct control of the Maison de Savoie in 1424, and followed the destiny of the Duchy to the Cateau-Cambr\u00e9sis treaty in 1559 [ 4 ] , [ 5 ] . At that time, the valley enjoyed a certain tranquility. At XIV It is century, significant circulation, both civil and military, was reported on the Route du Col de Fenestre [ 3 ] . At the end of XV It is century, there is an increased presence of the Vaudoise church [ 4 ] . Modern era [ modifier | Modifier and code ] The plague of 1630-1631 made many victims in the valley. In these same years, Valdieri and Entracque were erected in new strongholds, while Roaschia will later be towards the end of XVII It is century [ 4 ] , [ 5 ] , [ 6 ] . Contemporary period [ modifier | Modifier and code ] After the French Revolution of 1789, the valley saw various military activities. In 1793, the Savoyard troops parked for a long time in the valley, and in 1798 it was the turn of the Napoleonic troops to descend from the Col de Fenestre. The valley is annexed to France [ 4 ] , [ 5 ] . French troops engage in raids and looting [ 5 ] , while the French authorities engage in particular in the fight against smuggling [ 4 ] . With the restoration of 1814, the valley returned under the control of the Maison de Savoie. The XIX It is century sees the valley struck by several natural disasters, and in particular several floods [ 5 ] . In 1855, King Victor-Emmanuel II visited the valley and was very impressed by its characteristics. In 1857, the municipalities of Entecque and Valdieri ceded to the king the hunting rights in the municipal territories: this is how the “Royal Hunting Reserve”, which over time became the current Alpes Park, maritime [ 4 ] , [ 5 ] , [ 3 ] , [ 7 ] . The presence of the royal family leads to great economic effervescence: the Terme di Valdieri are built, as well as many hunting houses, and Savoy very often come on summer vacation in the valley, providing considerable profits to the local economy. Queen H\u00e9l\u00e8ne distinguished herself in this sense, she engaged a lot in initiatives beneficial to the valley [ 3 ] . In 1928, the administrative unit of the valley was interrupted, with the incorporation of the territory of Roaschia into the municipality of Roccavione; The municipality of Roaschia will become independent in 1946 [ 6 ] . During the Second World War, the valley was concerned by the activities of the supporters and by the corresponding ratings of the troops of the axis [ 4 ] . After the Second World War, the Valley economy underwent major transformations. Traditional agricultural and pastoral activities lost importance in proportion, and he stood out a phenomenon of impoverishment which gradually led to a migratory flow, with the consequence of the depopulation of the valleys [ 6 ] . Several industrial activities settled in the territory of the Valley, including the careers of the Itacementi and Buzzi-Unicem companies; On the other hand, there was a drop in tourist flow, especially in the Roaschia valley [ 6 ] . From the end of the 1960s, the construction of the Entecque hydroelectric power station, which brought new jobs to the valley, was started. [ 4 ] . Since the 1980s, there has been a revival of tourism activity, with the creation of Parco Naturalle Dell’Argentera (then became natural park of the Alpes Maritimes) [ 4 ] , the intensification of the management of shelters, the passage of the hiking route of the Great crossing from the Alps (Large crossing of the Alps) [ 8 ] first and via alpina [ 9 ] Then, and the recovery with tourist purposes of the old structures of the royal reserve, such as the hunting house of the Valasco valley, restored and reused as refuge (Valasco refuge). Language [ modifier | Modifier and code ] The Gesso valley is one of the Occitan valleys of Piedmont where Occitan is spoken. The local dialect has certain peculiarities [ ten ] , [ 11 ] . Manifestations [ modifier | Modifier and code ] The tradition of talk of Ent\u00e9cque has great historical and cultural interest. It is a sacred representation that stages the passion and death of Jesus Christ. This tradition has very old origins, even medieval according to certain sources [ 3 ] , while according to other sources it could go back to the time of the attempts to implant the Vaud church (end of XV It is century) or even the counter-reform ( XVI It is century) [ 4 ] . The event, which occupies the whole village for a long period, takes place every 5 years, in a similar way to the Br\u00e0ry de Sampeyre (who commemorates the expulsion of the Saracens), and will take place for the next time at Easter in 2015 in 2015 [ twelfth ] , [ 13 ] . Museums [ modifier | Modifier and code ] The town of Valdieri hosts several museums intended to preserve and recall local traditions. In the chief town of the town, there is a museum in the rye, an ethnographic museum, as well as the Museum of Ancient Trades [ 14 ] . gastronomy [ modifier | Modifier and code ] The Valley cuisine is very linked to the mountain environment. Among the typical products, there are several cheeses (Ricotta, tomino , soda , and the Castel Ariund , local cheese), honey and potatoes [ 15 ] . The typical dishes of the area are based on these ingredients, to which are added buckwheat, garden products, and other milk derivatives, such as cream [ 16 ] . Industry [ modifier | Modifier and code ] The presence of large quantities of limestone and clay shale has created an environment favorable to the installation of a few cement factories. The it is the Italcementi factory of Borgo San Dalmazzo, founded in 1941 and in activity since 1947, uses the material from two careers in the town of Valdieri: a limestone career in monte Cros near the village of Andonno, and a career as a clay shale Red earth at Our brunette [ 17 ] . The transport of the material of the career of monte Cros at the factory is done by means of a cable car, thus reducing the circulation of trucks on the territory of the valley [ 17 ] . There are also in the Roaschia valley two limestone careers of the Buzzi Unicem (formerly PRESACEMENTI) factory of Robilante, in activity since 1965. In this case, the material travels to the factory on a tape conveyor in a tunnel on duty [ 18 ] . One of the careers, now exhausted, has been the subject of an environmental rehabilitation, allowing to benefit from the area again [ 19 ] . The opening of a third career is planned, however part of the local population is opposed. Energy [ modifier | Modifier and code ]  It is in Ent\u00e9cque that the largest hydroelectric power station in Italy is located, the power station Luigi Einaudi [ 20 ] . Property of the Enel, the power station entered into office in 1982, but construction works had started in 1969 [ 21 ] . It uses water from the Torrent Gesso Di Barra, by means of three tanks [ 22 ] : lac plate , artificial basin near the village of Ent\u00e9cque, formed by the dam plate lac of ruin , natural basin in the upper Rovina valley lac del particilous , artificial basin in the Chiotas bowl, at the foot of Mont Argentera, formed by the two dams del particilous And by Colle Laura . The power station is able to provide 1,200 MW electrical power [ 20 ] , and can be visited by reservation [ 21 ] . Tourism [ modifier | Modifier and code ] The Gesso Valley offers different possibilities to the tourist. In the town of Valdieri, we find the thermal establishment of Terme di Valdieri , open during the summer period [ 23 ] . In the commune of Roaschia, there are interesting karst phenomena. Several caves are easily accessible from the capital of the town; Their visit still requires adequate preparation and equipment [ 24 ] . Part of the territory of the municipalities of Entecque and Valdieri is included in the Alpes Maritimes Natural Park, heir to the former “Royal Hunting Reserve” and the previous “Argentera Natural Park” and “Forest reserve and Palanfr\u00e8 lakes \u201d. The park offers very interesting possibilities with regard to nature and landscapes [ 25 ] . Among these, a particularity is the special nature reserve Juniperus phoenicea from Rocca San Giovanni , north of the village of Valdieri. This area has a particular microclimate, similar to that of the Mediterranean coast; This, added to the soil characteristics of the soil, in fact an ideal place for the proliferation of the juniper of Phenicia, which is precisely a typical plant of the Mediterranean vegetation [ 26 ] . The presence of the park and the remarkable orographic situation make available to the visitor an excellent territory of hiking and mountaineering. These activities are favored by the numerous shelters present in the territory of the valley: by going overall from west to east, Refuge Livio Bianco – 1910 m, refuge this – 2338 m, refuge Valasco – 1750 m, refuge Regina Elena – 1850 m, refuge Remondino – 2430 m, refuge Lorenzo Bozano – 2453 m, Refuge Morelli-Buzzi – 2350m, refuge Genova-Figari – 2015 m, Refuge Soria Ellena – 1840 m, refuge Pagar\u00ec – 2627 m. \u2191 (it)  ‘ Gesso Valle: Reading the history of the earth \u00bb  \u2191 a et b (it)  [PDF]  ‘ Guide of the Alpine paths of the province of Cuneo – vol. 2: Valli Stura, Gesso, Vermenagna \u00bb  \u2191 A b c d e f g h i j and k (it)  ‘ Gesso Valley – History \u00bb , on Diocese of Cuneo  \u2191 a b c d e f g h i j k l m n o p q and r (it)  ‘ History \u00bb , on Comune of Entracque  \u2191 a b c d e f and g (it)  ‘ History \u00bb , on Municipality of Valdieri  \u2191 A B C D and E (it)  ‘ History \u00bb , on Municipality of Roaschia  \u2191 ‘ History \u00bb , on Terme di Valdieri  \u2191 (it)  ‘ GTA – Main route \u00bb , on Mountain in the province of Cuneo  \u2191 ‘ Red route \u00bb , on Via alpina  \u2191 (it)  ‘ Geography of the Occitan valleys \u00bb , on Chambra d’Oc  \u2191 (it)  ‘ Culture – The language \u00bb , on Entracque.org  \u2191 (it)  ‘ The talk \u00bb , on Entracque  \u2191 (it)  ‘ The talk \u00bb , on Valllidicune.net  \u2191 (it)  ‘ Museums \u00bb , on Municipality of Valdieri  \u2191 (it)  ‘ The art of ancient flavors \u00bb , on Entracque.org  \u2191 (it)  ‘ The corner of the greedy (recipes) \u00bb , on Entracque.org  \u2191 a et b (it)  [PDF]  ‘ Italcementi and the Cemere of Borgo San Dalmazzo \u00bb , on Italcementi , p. 12, 44-45  \u2191 (it)  ‘ In Roaschia, Robilante and Roccavione the raw material is certified environment and safety \u00bb , on Buzzi-UNICEM group  \u2191 Rehabilitation of Roaschia’s career: (it)  ‘ p. 1 \u00bb , ‘ p. 2 \u00bb , on INDIENCE  \u2191 a et b (it)  ‘ Entracque \u00bb , on Ecotourism in Marittime  \u2191 a et b (it)  ‘ Luigi Einaudi Center – Enel \u00bb  [ Archive du June 29, 2015 ] , on Comune of Entracque  \u2191 (it)  ‘ The fingers of Entracque \u00bb : visit report  \u2191 ‘ The Royal thermal baths \u00bb , on Terme di Valdieri  \u2191 (it)  ‘ The caves of Roaschia \u00bb , on Municipality of Roaschia  \u2191 (it)  ‘ Maritime Alps Natural Park \u00bb , on raida.com  \u2191 (it)  ‘ Special Natural Reserve – Juniperus Phoenicea station – Valdieri (CN) \u00bb , on Piemonte region  On other Wikimedia projects:       (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4"},{"@context":"http:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"item":{"@id":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/#breadcrumbitem","name":"Enzyklop\u00e4die"}},{"@type":"ListItem","position":2,"item":{"@id":"https:\/\/wiki.edu.vn\/all2en\/wiki32\/valleee-du-gesso-wikipedia\/#breadcrumbitem","name":"Valle\u00e9e du Gesso \u2014 Wikipedia"}}]}]