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It is situated km mi north of the Saint Lawrence Riverinto which spiritual singles in lac-saint-joseph quebec drains via the Saguenay River. It covers an area of 1, km 2 sq miand is Its name in the Innu language is Piekuakamu.

The lake was named Piekuakami by the Innuthe Indigenous people who occupied the area at the time of European arrival. Spiritual singles in lac-saint-joseph quebec was given its French name after Jean de Quena Jesuit missionary who in was the first European to reach its shores.

Industry on spiritual singles in lac-saint-joseph quebec lake was dominated by the fur trade until the 19th century. Colonization began in the Saguenay—Lac-Saint-Jean region in the early 19th century and continued intensively until the early 20th century. Industry was mainly forestry and agriculture. Lac Saint-Jean also has an important summer resort and sport-fishing industry.

Prisoners worked the land, including lumbering and assisting in the production of pulp and paper. The bedrock of the Saguenay-Lac-Saint-Jean region consists largely of Precambrian igneous and metamorphic rocks. They are mostly composed of high-grade metamorphic rocks, amphibolite to granulite gneissthat are intruded by anorthositemangeritecharnockiteand granite plutonic rocks. The Lac Saint-Jean anorthosite is the major mafic intrusion present in the area.

These rocks comprise the Grenville Province of southern Spiritual singles in lac-saint-joseph quebec. It consists of fragments of island arcs and continental crust accreted to the south-eastern edge of Precambrian North American, Laurentia.

These lowlands are an elongated flat-bottomed basin formed by the Saguenay Graben by the displacement of Grenville crystalline rocks. This basin is km mi long and 50 km 31 mi wide. This basin is bounded by normal faults running parallel to its length.

Lawrence rift system. Preserved within the down-faulted interior of the Saguenay Graben are two large eroded, isolated patches, known as outliersof PaleozoicMiddle Ordoviciansedimentary rock composed of limestones and shales overlying Precambrian basement.

The Lac-Saint-Jean outlier rests against the south wall of the graben south of Lac Saint-Jean and extends to the west of the lake. The Chicoutimi Saguenay outlier rests against the north wall of the graben and extends southward spiritual singles in lac-saint-joseph quebec a few kilometers from the Saguenay River north of Chicoutimi.

These Middle Ordovician sedimentary rocks consist of sandstonesmicritic limestones and highly fossiliferousalternating beds of limestones and shales. These rocks have been preferentially eroded by repeated glaciations exhuming the Saguenay Graben. The Saguenay Graben that undelies Lac Saint-Jean Lowlands has controlled the deposition and the accumulation of Quaternary deposits sandgravelsiltand claywhich can reach up to m ft in thickness beneath the central lowlands.

The Quaternary sediments include glacialmarineglaciofluvial sediments and post-glacial alluvial and delta plain sediments. The area was covered by ice sheets several times throughout the Pleistocene. The valley formed by the Saguenay Graben being oriented more or less parallel to the glacial flow, became a preferred path for ice flow and spiritual singles in lac-saint-joseph quebec in deep excavation of the bedrock.

The glaciers cut into the graben and widened it in some places as well as making it considerable spiritual singles in lac-saint-joseph quebec in others. At the time of retreat of the last ice sheet, the region had been depressed below contemporaneous sea level.

As the land rose in response to considerable Post-glacial reboundthe bottom of the Saguenay Graben was blanketed by the Saguenay River with deltaic and terrestrial fluvial sediments to form the modern day Lac Saint-Jean Lowlands.

Contents move to sidebar hide. Article Talk. Read Edit View history. Tools Tools. Download as PDF Printable version. In other projects. Wikimedia Commons Wikivoyage. For the current federal electoral district, see Lac-Saint-Jean. For the spiritual singles in lac-saint-joseph quebec provincial electoral district, see Lac-Saint-Jean provincial electoral district.

Mesozoic fault reactivation along the St. Lawrence rift system, eastern Canada: Thermochronologic evidence from apatite fission-track dating. Geolgoical Society of America Bulletin, pp.

Archived from the original on 6 March Retrieved 31 December Archived from the original on Retrieved Aired: 20 July14h47 to 15h Characterization of general and singular features of major aquifer systems in the Saguenay-Lac-Saint-Jean region. Canadian Journal of Earth Sciences26 6pp. The Saguenay Fjord, Quebec, Canada: integrating marine geotechnical spiritual singles in lac-saint-joseph quebec geophysical data for spatial seismic slope stability and hazard assessment.

Marine Geology, pp. Wikimedia Commons has media related to Lac Saint-Jean. Authority control databases. Israel United States. Hidden categories: Articles with short description Short description is different from Wikidata Pages using infobox body of water with auto short description Articles containing Innu-language text Coordinates on Wikidata Articles using infobox body of water without alt Articles using infobox body of water without pushpin map alt Articles using infobox body of water without image bathymetry Pages with French IPA Commons category link is on Wikidata Articles with VIAF identifiers Articles with J9U identifiers Articles with LCCN identifiers.

Toggle limited content width. Piekuakamu Innu. Lac Saint-Jean Location in Quebec. Saguenay—Lac-Saint-Jean region, Quebec.

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