Lake Garda

Lake Garda (Lago di Garda ˈlaːɡo di ˈɡarda or (Lago) Benaco beˈnaːko; Lach de Garda; 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). In Roman times the lake was known as Benacus and by some it was revered as god Benacus, the personification of the lake, sometimes associated with the cult of Neptune. Today it is better known as Lake Garda, a toponym of Germanic origin attested since the Middle Ages and deriving from that of the homonymous town on the Veronese shore of the lake, which, together with another famous locality of the lake, Gardone Riviera, and others less known – such as Gàrdola, Gardoncino, Gardoni, Guàrdola and Le Garde – testifies the Germanic presence in the area that goes from the 6th to the 8th century CE, in particular, the Lombard one. The name Garda is evolved from the Germanic word warda, meaning "place of guard", "place of observation" or "place of safety". The classic toponym of the lake, or Benācus lacus (Benaco), is almost certainly of Celtic origin, therefore prior to romanization, and should derive from bennacus, comparable with the Irish bennach, which means "horned". The term may derive from the many promontories of the lake. 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.