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    88 Tb
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History

The company was established in 1976 by brothers' Franco and Carlo Pontiglione and by Giuseppe Priola. Lovers as they are of their own land, they did not hesitate in relaunching and making the most of the Langa's most typical product, thanks also to mother nature's generosity

 

Verduno Pelaverga: history and stories

Popular tradition has it that the Pelaverga vine was introduced in the town of Verduno in the XVII century, by., Blessed Sebastiano Valfrè, who brought some vine growing in the zone of Saluzzo. Present from time immemorial on the hills of Verduno connected with the story of Blessed in Fragrance of holiness, but also talked about as aphrodisiac, has always been considered a young adventurous knight, lively and light-hearted, a little saint and a little devil, in the court of King Barolo.

With its fragrant and spicy aroma, with a white pepper scent, it is considered a rarity by careful connoisseurs and enthusiasts in continuous search of new emotions.The impulse to grow such a vine was given to King Carlo Alberto of Savoy/Carignano(1798-1849), a great estimator of wines and in particular of Peleverga, since he possessed a country palace in this town with vineyards belonging to it.

Not even Peleverga managed to escape the scourges that swept across European wine growing between the XIX and XX centuries. Phylloxera, oidium, grape mildew made wine growing tremble and put the income of families from the Langa into great difficulty.

Once a remedy was found for these scourges, wine growing started to flourish again until new and perhaps even worse scourges hit it. The two World Wars and economical crisis following the first and pre-announced the second, put winegrowing in the Langa into difficulty once again. In the 50’s of the XX century, Peleverga was sporadically grown and used to produce grapes for eating, which were sold in the markets in Turin, or were used in other local vineyards. Slowly its diffussion diminished drastically nearly making it disappear. In the 70’s, always in the last century, thanks to the intuition of some great vine-dressers from Verduno, one being Mr. Giuseppe Priola, one of the owners of Bel Colle, saved Peleverga from extinction and was recovered. Since then, up till today, the growth of Peleverga, through physiological ups and downs, has never stopped, reaching in 1995 the sought after D.O.C. recognition.

The Verduno Pelaverga or simply Verduno wine, represents a small pearl of Langa oenology, therefore worldwide, a precious patrimony to respect and make use of to the full. The total area of the Pelaverga vineyards is only 15 hectares, but its importance for the territory which produces it is decisively relevant, more than any other wine grown.

In the 1990’s the Piedmont Region made a very close study of the two vines grown in Verduno and the Saluzzo area, and it concluded that they are two completely different vines, with just one thing in common. The name. To demonstrate such an affermation, in the National Catalogue of Vine Variety, Peleverga of Verduno has been registered as Peleverga Piccolo, a characteristic regarding the grape, to distinguish it from the other Peleverga.

 

 

 

 

 

 

 

 

 

 

Beato Sebastiano Valfrè

Born in Verduno on the 9th of March 1629 into a poor family, like many in that period, he finished his studies among many economical difficulties in Alba and Bra, moving to Turin at sixteen years of age. He managed to keep himself by being a copyist, to complete his philosophical studies. In 1650 he got a degree in Theology and ordained priest within the next year in the Congregation of the Oratory. This was founded in 1649 by Father Pier Antonio Defera with the help of priest Ottavio Cambiani and it inspired towards the teachings of San Filippo Neri “the Apostle of Rome”. The premature death of Father Pier Antonio Defera at just 34 years old on the 11th of September 1650 caused a profound crisis in the young congregation and all of the extraordinary preaching, not only in church but also and above all in every corner of the city of Turin, accompanied by feverish confessional activity, visits to prisons and hospitals seemed to be destined to fail.

In May of 1651 the young Sebastiano Valfrè presented himself to Father Ottavio Cambiani and asked to be admitted into the congregation, practically composed of only one person, without meansand near to closure. Valfrè was born poor, lived as a poor man and was not frightened by it. A little more than twenty years old, with a vitality and enthusiasm, not common, he threw himself into this new adventure to the full, without reserve and without savings, resuming the pastoral activity where Father Defera was constricted to interrupt. His tireless activity led him to have contacts with all social classes of Turin, from the most humble to His Royal Highness, the King of Piedmont, Vittorio Amadeo II. For the population, the majority illiterate and extremely poor, he became a sort of hope, but also a certainty of help in alleviating the moment’s difficulties.

He dedicated all of his life to being an apostolate, so much that San Giovanni Bosco defined him “The Apostle of Turin”.An example was his assistance to the people of Turin during the seige of the French in 1706, the same Pietro Micca was looked after and confessed by Valfrè. Thanks to his assistance to the Savoyard troops during the war with the French, he was named patron of the army. He died in Turin on the 30th of January 1710 and on his death, Amedeo II of Savoy said he had lost a great friend and the poor, a great protector and father. He was the precursor and master of great Torinese Social Saints such as Giovanni Bosco, Giuseppe Benedetto Cottolengo and Giuseppe Cafasso.
He was blessed on the 15th of July 1834 by pope Gregorio XVI. He is liturgically remembered every 30th of January.

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Vineyards

The hills of the Langa surfaced for the first time about 30 million years ago, when the Thetis withdrew. The territory was formed by rocks originating from marine sedimentation during the periods of the Tertiary age starting from the most antique Eocene (55-37 million years ago) following on in the successive Oligocene (37 – 23) and Miocene (23 – 5) which produced a whole series of floor stratifications which differ for the structure and granulometry according to their distance from the coast.

Their origin and following surfacing was connected to orogenetic phenomenons responsible for the formation of the Alps. The alpine chain originated (about 40 million years ago) from that series of phenomenons of compression and folding connected to the movement of the areas of the European and African continents. In this first phase the Thetis ocean was divided in various internal seas.

The following Oligocene period was a relatively calm one of collisional movement during which the area of the Ligurian Maritime Alps and therefore the Langa endured a slow subsidence until being newly covered by a sea which was not very deep.

Successively, at the end of the Miocene the continuous movement of the African area against the European one caused the formation of mountainous chains between southern Spain and North Africa and therefore causing the closure of the Strait of Gibralta, completely isolating the first Meditteranean from the Ocean and carrying out the complete emerging of the Langa.

At the beginning of the Pliocene (about 5 million years ago) the continuous movement between Africa and Europe provoked the seperation of Spain and Africa again allowing the Ocean to flow into the Mediterranean basin again. The Langa remained on the surface but the sea covered the lower part again, that between Alessandria and Cuneo.

At the end of the Tertiary age new compression towards north brought about the slow rising of the entire Piedmontese territory and the definite withdrawal of the Po Sea and the formation of the current hilly areas in the Langa, that with time were changed by the erosion of water streams. The old geologic eras ended at the beginning of the Quaternary age (about 11,5 million years ago) the same that we find ourselves in today. The “scenery” was complete and a strange actor could enter onto the scene to start his recital on these hills: man.

During this long period of time, about 40 million years, the rocks that formed the land have changed profoundly, starting from the Pretertiary base which forms the substrate on which the sedimentation of the Piedmontese Tertiary Basin has placed itself over millions of years, which range from sandstone stratum (the most compact gave origin to the Langa’s stone), to shaley-calcareous marls (the popular Ton or Tov) to sedimentary rocks containing gypsum/sulphide, very diffused in the town of Verduno and are probably the origin of spicy fragrances of wine produced here.

 

Monvigliero vineyard

The area of Verduno named Monvigliero has always been considered the best of the municipality,but also among the best in all of the area for producing Barolo wine. It is a natural amphitheatre exposed south-westerly, to the classic afternoon sun, where the particular microclimate exhalts the production of a Barolo wine which is very fragranced and delicate with a balanced body and with soft tannins. An extremely long lasting wine which preserves these characteristics through time.

 

Borgo Castagni vineyard

Borgo Castagni is a synonym of Bel Colle, in fact the wine cellar stands in this locality which joins both Verduno and La Morra. They are household vineyards where the vegetative production is controlled and monitored daily by Belle Colle from pruning to gathering. It is exposed towards west-southwest and wines produced on calcareous-clay land with gypsum veining have an olfactory component which is unique for its intensity and persistence joined with an excellent colouring intensity.

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Winemaking

The Pelaverga Piccolo Vine, morphological characteristics

The shoot has a cotony apex, greenish white with borders that are just about pink, the apical leaves (from 1 to 3) bend in a cup shape, of a greenish white colour, with borders that are just about pink and cotony on the inside.

Base leaves (4 - ) are of a yellowish light green colour, with light copper shades, glossy on top and downy underneath.

The tendrils are very long and strong.

The bunch when ripe is medium large, conical or pyramid-shaped, winged (often with a wing of a pedunculate length) spread (above all in the proximal part), the peduncle is long lignified in the first part, of a green colour, shaded with pink.

The grape is medium, or medium-small from spheroidal to ellipsoidal short with a very pruinose skin (which gives off a bluish-grey coloration), of a violet blue colour.

The adult leaf is medium large from cuneiform to pentagonal, quinquelobate or more often trilobate. The edge is dark green in colour with a base of nervation that is principly just pink

The maturation of the grape is middle to middle-late (first ten days of October).

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