Champlain Valley southward into the Valley of Vermont. The Vermont Lowlands are primarily underlain by sedimentary rocks, especially limestone and shale, though metamorphic rocks such as marble and slate are also present. Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, drained northward by the Richelieu River into the St. Lawrence River at Sorel-Tracy, Quebec (northeast of Montreal). Major tributaries of Lake Champlain include Otter Creek and the Winooski, Missisquoi, and Lamoille rivers in Vermont, and the Ausable, Chazy, Boquet, and Saranac rivers in New York. Lake Champlain also receives
Lordship of Champlain Lordship of Champlain The Lordship of Champlain was granted in 1664, on the north side of the St. Lawrence River between Trois-Rivières and Quebec City, under the feudal system of New France. Today, the territory of the former manor of Champlain is located in the administrative region of Mauricie in Quebec, Canada. The capital was the town of Champlain. The Lordship of Champlain stretched from the north shore of the St. Lawrence River (west of the mouth of the Champlain River) up towards the north, parallel to the Lordship of Batiscan on the east side. The north-south dividing line between