Canal de Lalinde

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Canal de Lalinde
Canal de Lalinde (port de Badefols) amont (1).JPG
The canal passing through Port de Badefols
Specifications
Length15 km (9.3 mi) [1]
Locks9 [1]
StatusDisused by the 1930s
History
Principal engineerVauthier
Construction began1838
Date of first useAfter 1840 [1]
Date completed1843
Geography
DirectionWest
Start point Mauzac-et-Grand-Castang
End point Tuiliéres
Beginning coordinates 44°51′50″N0°48′00″E / 44.86402°N 0.79994°E / 44.86402; 0.79994
Ending coordinates 44°50′49″N0°37′48″E / 44.84691°N 0.62989°E / 44.84691; 0.62989

The Canal de Lalinde is a canal in south western France lateral to the Dordogne River. Its purpose was to bypass the rapids of the river. [1]

Dordogne (river) river in Southwestern France

The Dordogne is a river in south-central and southwest France. The Dordogne and its watershed were designated Biosphere Reserve by UNESCO on July 11 2012.

Contents

Locks

The canal begins with its first lock at the village of Mauzac, just below the cingle of Tremolat. Two more locks are found where the canal passes through Lalinde and Borie-Basse. The canal rejoins the Dordogne with two sets of three locks in Tuilières.

Mauzac-et-Grand-Castang Commune in Nouvelle-Aquitaine, France

Mauzac-et-Grand-Castang is a commune in the Dordogne department in Nouvelle-Aquitaine in southwestern France.

Meander A sinuous bend in a series in the channel of a river

A meander is one of a series of regular sinuous curves, bends, loops, turns, or windings in the channel of a river, stream, or other watercourse. It is produced by a stream or river swinging from side to side as it flows across its floodplain or shifts its channel within a valley. A meander is produced by a stream or river as it erodes the sediments comprising an outer, concave bank and deposits this and other sediment downstream on an inner, convex bank which is typically a point bar. The result of sediments being eroded from the outside concave bank and their deposition on an inside convex bank is the formation of a sinuous course as a channel migrates back and forth across the down-valley axis of a floodplain. The zone within which a meandering stream shifts its channel across either its floodplain or valley floor from time to time is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering problems for local municipalities attempting to maintain stable roads and bridges.

Lalinde Commune in Nouvelle-Aquitaine, France

Lalinde is a commune in the Dordogne department in Nouvelle-Aquitaine in southwestern France. It lies on the Dordogne River and was enclosed within fortified walls of which little remains today.

See also

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References

  1. 1 2 3 4 McKnight, Hugh (2005). Cruising French Waterways, 4th Edition . Sheridan House. ISBN   978-1-57409-087-1.

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