Hotel B&B Avellino
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The of campania Appennino, reached in the province of Avellino, is opened to the center of a formed width conca from the Picentini mounts. In this evocative scene it is spread Goes it them of the Saturday in which the city of Avellino rises, capoluogo of the Irpinia. The city is encircled to the northeast from the Montevergine (m.1493) that it is sure most famous of mounts of the Partenio, characterized com' is from omonimo the Benedictine sanctuary of XII the century, place to 1270 m. Main the water course that crosses the city is the S. Francisco (by now nearly of the all place setting) and the Rigatoreche covers fondovalle the Fenestrelle. Thanks to the exploitation of the water energy of the river, along its way in the centuries pass to you were the most active flourishing and the processes of the working of the cloth, wools, the ironworks, the flour mills and cartiere. The city of Avellino is found to being a point centers them in the important crossing communication ways combines the Adriatic to the Tyrrhenian one, beyond connecting the beneventana area and that salernitana, this last one through goes them to them of the Sarno and the Irno. And obvious that the territory enjoys a natural water resource thanks also to the next presence of the river Heat, than, feeding the aqueduct of the High Heat, it not only supplies water to extraprovincial the most numerous city but also to common of the province and. The surrounding campaign, remarkablly reorganized from the been left over one of the constructions of these last decades, is rich of vegetation with prevalence of nocelleti that they produce the valuable ' avellane ' nocciuole. The fertility of the earth, rich above all of ortaggi and yields, it must to the salubrità of the climate and to the abundance of the precipitations that happen in the course of the year. The climate of Avellino is in fact of continental type: rigid in winter, it introduces also in the warm season remarkable excursions in the daily temperature for the sensitive lowerings of the same one in the nocturnal hours. The mountains (Montevergine and Terminio) are constituted from limestone and mesozoiche cliffs. To Avellino city and in the collinari zones of the outskirtses the sottosuolo ignimbrite is constituted from the so-called tufo of campania gray (), of vulcanica origin, eroded from the two rivers that cross one valley.
Part of the information regarding the history, the art, the traditions and the events about the city of on this page is drawn from www.wikipedia.org respecting the GNU Free Documentation License. |
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