Costanza

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Leaving the rocky base and the steep relief of Portage-de-Roches, it then enters an alluvial and semi-alluvial plain up to dam de la Chute-Garneau [3] where the landscapes on both banks alternate between residences and agricultural land for a little over ten messagex. The Chute-Garneau dam is a watercourse retaining structure located on a rock base. After having bypassed Pointe du Chien, it passes under Autoroute 70 and enters the Fdom industrial park. The river then crosses the Pont-Arnaud dam and begins its increasingly rapid descent towards the Saguenay as the relief becomes increasingly steep. This retaining structure dries up the original rock bed of the river to divert it towards an underground water intake which supplies the S.

Description

Leaving the rocky base and the steep relief of Portage-de-Roches, it then enters an alluvial and semi-alluvial plain up to dam de la Chute-Garneau [3] where the landscapes on both banks alternate between residences and agricultural land for a little over ten kilometers.

The Chute-Garneau dam is a watercourse retaining structure located on a rock base. After having bypassed Pointe du Chien, it passes under Autoroute 70 and enters the Haut-Saguenay industrial park.

Saguenay messages from friends

The river then crosses the Pont-Arnaud dam and begins its increasingly rapid descent towards the Saguenay as the relief becomes increasingly steep. This retaining structure dries up the original rock bed of the river to divert it towards an underground water intake which supplies the S.

The river then re-emerges in the historic site of the Pulperie de Chicoutimi and continues to descend to the Chicoutimi dam basin. Finally, it flows into the Saguenay River.

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The Chicoutimi River flows mainly in the Saguenay grabena vast elevated valley that overlooks the lowlands surrounding the Saguenay River. The soils of this large depression are composed of Quaternary marine sediments, such as silt and claydeposited at the end of the Pleistocene and during the beginning of the Holocene by the Laflamme Sea.

The basin territory includes sections of 6 unorganized territories, the municipality in four MRCs. This river is artificially controlled over Downstream from Pont-Arnaudthe second section has a drop of The erosion of the river, barely visible upstream, becomes very apparent downstream because it has been dug, over time, in the granite of fjorda small valley up to Saguenay River.

The river is influenced sagjenay the tide only downstream of the Chicoutimi dam where it forms a basin.

Watershed[ edit ] Official deation of the basin[ edit ] First, it is important to specify that the Chicoutimi fgiends watershed includes that of Kenogami Lake since the Letellier judgment in The Chicoutimi river basin is also a sub-basin of the Saguenay Riverwhich in turn flows into the St. Lawrence River and ends up in the Atlantic Ocean which drains most of the eastern Quebec rivers.

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In terms of flow control, four entities are involved in the management of dams:.

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