The Osorno–Llanquihue Basin (Spanish: Cuenca Osorno-Llanquihue) is a sedimentary basin located in south-central Chile in the forearc region of the Andes. From north to south the basin spans and area from Catamutún to Reloncaví Sound (40–42° S). The deepest part of the basin lie to the east. The lower levels of the basin are occupied by coal-bearing Cheuquemó Formation among other units while the Miocene-aged marine Santo Domingo Formation makes up much of the upper stratigraphy. The uppermost levels are made of sediments of Quaternary age of glacial, , glaci-lacustrine and volcanic character. The thickness of Quaternary sediments is greater to the south reaching almost 1,300 m in Puerto Montt. Sediments in the western part of the basin are roughly estimated to have reached 70 °C during bur
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| - Cuenca Osorno–Llanquihue (es)
- Osorno–Llanquihue Basin (en)
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| - La cuenca Osorno–Llanquihue es una cuenca sedimentaria localizada en el sur de Chile en la región de antearco de los Andes, correspondiendo a la parte más austral de la depresión intermedia. De norte a sur, la cuenca abarca el área desde Catamutún en la provincia del Ranco al seno de Reloncaví (40–42° S). La parte más profunda de la cuenca se encuentra al este. Los niveles más bajos de la cuenca están ocupados por la carbonífera formación Cheuquemó entre otras unidades mientras que la formación Santo Domingo, que data del Mioceno, conforma la mayor parte de la estratigrafía superior. Los niveles más superiores están hechos de sedimentos de edad cuaternaria, de características glaciales, glacifluviales, glacilacustres y volcánicas. El grosor de los sedimentos cuaternarios es mayor hacia (es)
- The Osorno–Llanquihue Basin (Spanish: Cuenca Osorno-Llanquihue) is a sedimentary basin located in south-central Chile in the forearc region of the Andes. From north to south the basin spans and area from Catamutún to Reloncaví Sound (40–42° S). The deepest part of the basin lie to the east. The lower levels of the basin are occupied by coal-bearing Cheuquemó Formation among other units while the Miocene-aged marine Santo Domingo Formation makes up much of the upper stratigraphy. The uppermost levels are made of sediments of Quaternary age of glacial, , glaci-lacustrine and volcanic character. The thickness of Quaternary sediments is greater to the south reaching almost 1,300 m in Puerto Montt. Sediments in the western part of the basin are roughly estimated to have reached 70 °C during bur (en)
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| - Osorno–Llanquihue Basin (en)
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| - SRTM map of the topography of the northern part of Osorno–Llanquihue Basin. The basin does largely correspond with the topographic low of the Chilean Central Valley. (en)
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| location
| - Southwestern South America (en)
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| - Cuenca de Osorno-Llanquihue (en)
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| - La cuenca Osorno–Llanquihue es una cuenca sedimentaria localizada en el sur de Chile en la región de antearco de los Andes, correspondiendo a la parte más austral de la depresión intermedia. De norte a sur, la cuenca abarca el área desde Catamutún en la provincia del Ranco al seno de Reloncaví (40–42° S). La parte más profunda de la cuenca se encuentra al este. Los niveles más bajos de la cuenca están ocupados por la carbonífera formación Cheuquemó entre otras unidades mientras que la formación Santo Domingo, que data del Mioceno, conforma la mayor parte de la estratigrafía superior. Los niveles más superiores están hechos de sedimentos de edad cuaternaria, de características glaciales, glacifluviales, glacilacustres y volcánicas. El grosor de los sedimentos cuaternarios es mayor hacia el sur, alcanzando casi 1300 m en Puerto Montt. Los sedimentos en la parte occidental de la cuenca se estiman que alcanzaron aproximadamente unos 70 °C durante su entierro y diagénesis. (es)
- The Osorno–Llanquihue Basin (Spanish: Cuenca Osorno-Llanquihue) is a sedimentary basin located in south-central Chile in the forearc region of the Andes. From north to south the basin spans and area from Catamutún to Reloncaví Sound (40–42° S). The deepest part of the basin lie to the east. The lower levels of the basin are occupied by coal-bearing Cheuquemó Formation among other units while the Miocene-aged marine Santo Domingo Formation makes up much of the upper stratigraphy. The uppermost levels are made of sediments of Quaternary age of glacial, , glaci-lacustrine and volcanic character. The thickness of Quaternary sediments is greater to the south reaching almost 1,300 m in Puerto Montt. Sediments in the western part of the basin are roughly estimated to have reached 70 °C during burial and diagenesis. (en)
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| lakes
| - Llanquihue, Laguna Las Ortigas and the westernmost portions of Rupanco, Puyehue and Ranco (en)
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| named for
| - Osorno and Llanquihue Lake (en)
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| - Southern tip is offshore (en)
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| - POINT(-73.109214782715 -40.71212387085)
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