Lebu River

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Lebu River

Lebu River an important river of the Arauco Province. It has his sources in the western slope of the Nahuelbuta Range to the east of the city and port of Lebu, capital of the province and named for the river.

The Lebu is formed from the confluence of the Riachuelos of Curanilahue and Pilpilco that meet at the base of that mountain range. From the confluence it continues to the west, widening with the flow of the Riachuelos of Quilañanco and Curihuillín, and with several streams that join it from the wooded heights on both of its banks. It goes on to empty into the Pacific Ocean at 37° 36' Lat. and 73° 41 ' Lon. after a course of about 100 kilometers until it is below the ford of Cupaño, at the salto de Gualgalén, where this strong torrent of the river that is about 20 kilometers from its mouth meets the upper reach of the tidal estuary.

At the river mouth the coast forms a port or anchorage between the Morro de Tucapel to the south, and the Punta de Millonhue to the north. Between them extends the bar of the mouth, that only opens the way by a narrow channel. Above the mouth the river estuary in front of the city is narrow and further up the river is wide and deep. In the upper part of this estuary, is the location of the old fort of Santa Margarita de Austria.

The name of the river is an alteration of the Mapudungun leufü or leuvu, “river”; and in colonial times a valley of a river, that contained habitations of Indians was called a levo. [1]

As result of the 2010 Chile earthquake a large islet emerged at the mouth of the river. This area was the part of the coast that experience the highest permanent uplift resulting from the earthquake. [2]

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Licauquén River a short river or riachuelo south of Lebu and west of Cañete. It comes from the eastern wooded heights of the Arauco Province to the coast of the Pacific Ocean, it is joined in its upper reaches by a tributary riachuelo named Pilmaiquén and it runs a few kilometers to the southwest to end on the coast at 37° 50' Lat. South, nearby Punta Molguilla.

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Fort Colcura was a small fort that was the first Spanish settlement that existed in the commune of Lota, Chile. It was on a small height on the edge of the Bay of Arauco, a little more than two kilometers to the southeast of the modern city of Lota. From its position it dominated the north slope of cerro Marihueñu and the valley of Colcura in whose extreme west is the mouth of the riachuelo Colcura that empties into the cove of Colcura.

Rele River is a river in the commune of Santa Juana. It has its origin to the south southeast of Santa Juana, from where it runs to the northeast from among the slopes of the heights of the Nahuelbuta Range and runs to the east to the Bio Bio River in which it empties a little above the confluence with the Laja River. It a river with a small volume and its course is 20 kilometers long. It has a tributary that joins it from the south, the Riachuelo Millapoa or de las Minas from the gold mines that in the sixteenth century were worked on its banks. Immediately on the north bank of the Rele River from the Millapoa was the location of the old city of Santa Cruz de Coya. At the mouth of the river was the old fort and town of Monterrey de la Frontera. A small town of Monterey now exists nearby. The Mapudungun name comes from the verb relen, “to face up”.

Quilacoya River is located in the Hualqui commune of Concepcion Province of Chile. It has course of about 40 kilometers with a small volume. It originates in the southern slopes of the series of heights of Lucay that run from east to west in the southern part of the commune of Florida. It runs to the southwest to join the Bío Bío River on the North bank nine kilometers above the town of Hualqui.

References

  1. Diccionario geográfico de la República de Chile pg. 362 Lebu. — Rio
  2. Quezada, Jorge; Jaque, Edilia; Catalán, Nicole; Belmonte, Arturo; Fernández, Alfonso; Isla, Federico (2020). "Unexpected coseismic surface uplift at Tirúa-Mocha Island area of south Chile before and during the Mw 8.8 Maule 2010 earthquake: a possible upper plate splay fault". Andean Geology . National Geology and Mining Service. 47 (2). doi: 10.5027/andgeoV47n2-3057 .

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