1998
DOI: 10.4067/s0716-02081998000200007
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Evolución geológico-geomorfológica cuaternaria del tramo superior del valle del río Laja

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Cited by 28 publications
(24 citation statements)
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“…This is in line with the high storage capacity observed in basins of volcanic origin located in central Chile that drain from the Andes. Moreover, it is expected given the high permeability of the predominantly granular type soils (Thiele et al 1998). (c) The parameters P Lim and D are related to the direct recharge processes of the aquifer.…”
Section: Resultsmentioning
confidence: 99%
“…This is in line with the high storage capacity observed in basins of volcanic origin located in central Chile that drain from the Andes. Moreover, it is expected given the high permeability of the predominantly granular type soils (Thiele et al 1998). (c) The parameters P Lim and D are related to the direct recharge processes of the aquifer.…”
Section: Resultsmentioning
confidence: 99%
“…The Andean zone of the river (600 to 2000 m.a.s.l.) is composed of sedimentary and plutonic rocks on which there are volcanic and volcanoclastic deposits of the Antuco-Sierra Velluda volcanic complex (Thiele et al, 1998). The central depression consists of the large Laja River black sand cone alluvial deposit (100 to 300 m.a.s.l.…”
Section: Case Studymentioning
confidence: 99%
“…(a) Laja Lake: located at the slope of the Andean mountains (860-3550 m above sea level (masl)), with soils of low permeability (Thiele et al, 1998). The Laja Lake, together with the El Toro hydropower plant, plays an important role in the flow regime.…”
Section: Study Areamentioning
confidence: 99%