Torbole, Lake Garda - Northern Italy | 4K Scenic Drive скачать в хорошем качестве

Torbole, Lake Garda - Northern Italy | 4K Scenic Drive

Lake Garda (Italian: Lago di Garda, Italian: [ˈlaːɡo di ˈɡarda], or (Lago) Benaco, Italian: [beˈnaːko]; Eastern Lombard: Lach de Garda; Venetian: Ƚago de Garda) is the largest lake in Italy. It is a popular holiday location in northern Italy, between Brescia and Milan to the west, and Verona and Venice to the east. The lake cuts into the edge of the Italian Alps, particularly the Alpine sub-ranges of the Garda Mountains and the Brenta Group. Glaciers formed this alpine region at the end of the last ice age. The lake and its shoreline are divided between the provinces of Brescia (to the south-west), Verona (south-east) and Trentino (north). The northern part of the lake is located in a depression that insinuates itself inside the Alps, while the southern part occupies an area of the upper Pianura Padana. The shape is typical of a moraine valley, probably having been formed under the action of a Paleolithic glacier. Although traces of the glacier's actions are evident today, in more recent years it has been hypothesised that the glacier occupied a previously existing depression, created by stream erosion 5 to 6 million years ago. A characteristic of Garda is the limited size of the hydrographic basin (2,290 square kilometres or 880 square miles) compared to the lake surface: at a length of 52 kilometres (32 mi) of the lake corresponds the 95 kilometres (59 mi) of the basin, while the respective widths are 16 kilometres (9.9 mi) and 42 kilometres (26 mi). The eastern watershed of the Benacense basin has a direction parallel to the axis of the lake, while the western one has a more sinuous course. Within the basin, the major peaks are Presanella (3,556 metres or 11,667 feet) and Adamello (3,554 metres or 11,660 feet). Morphologically, the Garda hydrographic basin can be divided into four areas: the plain of about 200 square kilometres (77 sq mi), the lake surface of about 370 square kilometres (140 sq mi), the western portion of about 500 km² and the eastern one of approximately 1,040 square kilometres (400 sq mi). To the south of Lake Garda, between Brescia, Mantua and Verona, a large morainic amphitheatre develops: a succession of hilly circles with small flat areas interposed, in some cases marshy, originated thanks to the transport and storage action of the great Garda glacier. These morainic deposits were formed during the glaciations Günz, Mindel, Riss and Würm: very limited morainic deposits are attributed to the two oldest, Günz and Mindel, while the outer morainic circles are attributed to the Riss glaciation and the inner ones to the Würm glaciation. The morphology of the hills is gentle and with delicate lines; from the highest points, it is possible to perceive the relationships that link the hills to the mountains as well as the circular amphitheatre shape of the hills, which seem to embrace the southern part of the lake. The main tributary of Lake Garda is the Sarca River, others include the Ponale River (fed by Lago di Ledro), the Varone/Magnone River [de] (via the Cascate del Varone) and various streams from both mountainsides, while the only outlet is the Mincio River (79 metres or 259 feet, at Peschiera). The subdivision is created by the presence of a fault submerged between Sirmione and Punta San Vigilio which is almost a natural barrier that hampers the homogenization between the water of the two zones. If the water level of the Adige River is excessive, water is diverted to the lake through the Mori-Torbole tunnel. The lake has also numerous small islands and five main ones, the largest being Isola del Garda. Nearby to the south is San Biagio island, also known as the Isola dei Conigli ("island of the rabbits"). Both are offshore of San Felice del Benaco, on the lake's western side. The three other main islands are Isola dell'Olivo, Isola di Sogno, and Isola di Trimelone, all farther north near the east side. Ship transport is provided by Navigazione Laghi. A daily ferry service connects major towns on the eastern and western shores of Lake Garda. The service runs from Desenzano del Garda to Riva del Garda, via Peschiera del Garda, Salò and Malcesine. The region can be reached directly via the Milan-Venice railway, with Desenzano-Sirmione and Peschiera railway station. The lake is located at the centre of a crucial node between Brescia, Verona and Trento, and is therefore easily reachable via transversal infrastructures of the Po Valley and those of the Brenner-Rome axis https://en.wikipedia.org/wiki/Lake_Garda Filmed in September 2024. My Equipment - Camera - https://amzn.to/3PlgZfB Camera 2 - https://amzn.to/3Ve90os Memory Card - https://amzn.to/43eHMA8 Suction Mount - https://amzn.to/3PhHbaU Multi Charger - https://amzn.to/3Vz3T2z Power Bank - https://amzn.to/3PlBrNo Laptop - https://amzn.to/3wZTySI External Hard Drive - https://amzn.to/43iBcbL Portable Power Station - https://amzn.to/3IBe92k Please Subscribe, it helps us more than you can imagine - https://bit.ly/3GTLtQv