have inhabited the Saguenay Fjord area for thousands of years prior to the first Europeans arriving. The first European to visit the area was Jacques Cartier, in 1535. Between 1628 and 1842, the Saguenay economy was heavily dependent on the fur trade.
In 1838, settlers began moving into the Saguenay region. Between 1840 and 1920, the region had a sizable lumber industry. By the end of the 19th, much of the forests around the Saguenay River were depleted. In addition to the depletion of the forests, difficult terrain and the decline of the lumber industry led to the Saguenay area remaining mostly undeveloped into the 20th century. Starting in 1970, the Quebec government began acquiring land around the fjord in hopes of protecting it. In 1982, the government held public on the park's design and boundaries. Saguenay National Park was officially created on June 8, 1983. In 1984, the park was twinned with France's Cévennes National Park. In 1991, facilities were added to the Baie du Moulin-à-Baude section, while in 2000, facilities were added to the Baie-Sainte-Marguerite section. On April 20, 2011, the park changed its name from Saguenay National Park to Saguenay Fjord National Park in order to emphasize the fjord's distinctiveness of being one of the most southerly fjords in the Northern Hemisphere.
Geography
Saguenay Fjord National Park lies along the shore of its namesake fjord. The Saguenay–St. Lawrence Marine Park lies to the southeast of the park. The park has lands within the following regions of Quebec: Saguenay-Lac-Saint-Jean, Charlevoix, Côte-Nord and Bas-Saint-Laurent. Saguenay Fjord National Park's Baie-Éternité visitor center is about from Saguenay, Quebec. Saguenay Fjord, the park's namesake, has a length of and a width that varies between and. The fjord has an average depth of, with the deepest point being. The cliffs along the fjord have an average height of, reaching a maximum height of. Saguenay Fjord flows into the St. Lawrence River; salt water from the river flows under a layer of freshwater originating from Lac St. Jean. Salt water takes up 93% of the water volume inside the fjord. The park contains the following three regions:
Baie-Éternité: This southwest region is reached through the village of Rivière-Éternité. The Saguenay Fjord Interpretation Centre is located here, and features exhibits about the formation of the fjord, its geology and wildlife.
Baie-Sainte-Marguerite: The north region near Sacré-Cœur includes the Beluga Interpretation Centre. In the summer, beluga whales congregate in the bay.
Baie du Moulin-à-Baude: Located around Tadoussac, this is the eastern region of the park. The Maison des Dunes Interpretation Centre features exhibits about the park's sand dunes, wildlife, marine life and ecosystems, and offers naturalist and fall bird-watching programs in conjunction with the Observatoire d'oiseaux de Tadoussac.
Geology
The geological origins of Saguenay Fjord National Park can be traced to the Grenville orogeny during the Precambrian era. This event is considered to be the beginnings to the Laurentian mountains. Around 200 million years ago, a rock basal complex between a north fault and a south fault collapsed, creating the Saguenay Graben. The graben was long and wide. During the last glacial period, the region was covered by ice sheets two to three kilometers deep. The ice sheets cut deep into the Saguenay graben, gouging the fjord in the process. The weight of the ice sheets also caused the region to sink. When the glaciers melted around 10,000 years ago, the graben was flooded by seawater. The subsequent post-glacial rebound lifted the terrain, shaping the fjord valleys in the process.
Saguenay Fjord National Park had 90,550 visitors in 2005, with 90% of those visitors coming from outside the region. Activities in the park include over of hiking trails, of skiing trails, camping, kayaking, sea kayaking, a Bateau Mouche tour of the fjord, snowshoeing and ice fishing. Accommodations at the park include cabins, huts and campgrounds.
