Fundy Basin Fundy Basin The Fundy Basin is a sediment-filled rift basin on the Atlantic coast of southeastern Canada. It contains three sub-basins; the Fundy sub-basin, the Minas Basin and the Chignecto Basin. These arms meet at the Bay of Fundy, which is contained within the rift valley. From the Bay of Fundy, the Minas Basin trends northeast to Nova Scotia. Chignecto Bay runs from the Bay of Fundy northwest between New Brunswick and Nova Scotia which is separated from the waters of the Northumberland Strait by the Isthmus of Chignecto. The Fundy Basin is best known for the bay it contains.
Geography of New Brunswick and Kennebecasis River. Other water bodies within the Saint John River system are Grand Lake (which itself is fed by the Salmon River), Washademoak Lake (fed by the Canaan River), and Belleisle Bay. The high tides of the Bay of Fundy often cause the Saint John River to flow upstream, an effect most pronounced at the Reversing Falls in Saint John. The Petitcodiac River, Shepody River, Tantramar River, and Memramcook River empty into Chignecto Bay at the head of the Bay of Fundy. Like the Saint John River, the Bay of Fundy tides cause another upstream phenomenon, known as a