Lake Neuchâtel

The lake's drainage area is approximately 2,670 km2 (1,031 sq mi) and its culminating point is Le Chasseron at 1,607 metres (5,272 ft).

In the summer of 2021, Lake Neuchatel reached historically high water levels due to widespread flooding over mainland Europe.

[5] Several megalithic monuments line the lake such as the alignment of Clendy and the menhirs of Gorgier, Grandson, Saint-Aubin-Sauges, and Vauroux, as well as an imposing erratic block, the Stone of Marriage [fr].

What is now Yverdon-les-Bains was located on a barrier island on the other side of the lake, a place of smaller settlement (3 to 4 hectares) occupied from the 4th century BCE, and later fortified in 80 BCE by means of a long and solid rampart with frontal posts (like that of Vully), before this oppidum (Eburodunum) becomes a vicus in the first centuries CE.

[7] The name dominates throughout the Middle Ages, co-utilized with the current term Lake Neuchâtel, however, is frequent from the 15th century onwards.

The latter became dominant during the 19th century, in particular with the lowering of the level of the lake and the development of the Vaudois railway, which reduced the importance of the Port of Yverdon.

Cantonal participation of Lake Neuchâtel