Chilean Lake District in the context of Toltén River


Chilean Lake District in the context of Toltén River

⭐ Core Definition: Chilean Lake District

The Chilean Lake District is a zone in Southern Chile defined by its many lakes in the Andean foothills. The term is primarily used in tourism literature and advertising, in Chile Zona Sur is preferred as a geographical concept. The Chilean Lake District includes the cities of Temuco, Villarrica, Pucón, Valdivia, Osorno, Entre Lagos (Puyehue), Puerto Octay, Frutillar, Puerto Varas and Puerto Montt.

All lakes drain ultimately to the Pacific Ocean. In the north to Toltén River collects the water of Villarrica, Caburgua and Colico. South of these lakes lie the Seven Lakes whose waters reach the Pacific through Valdivia River. Bueno River drains the water of Ranco, Maihue, Puyehue and Rupanco lakes. Llanquihue Lake is drained to the Pacific by Maullín River and Petrohué River does the same for Todos los Santos Lake.

↓ Menu
HINT:

In this Dossier

Chilean Lake District in the context of Southern Chile

Southern Chile is an informal geographic term for any place south of the capital city, Santiago, or south of Biobío River, the mouth of which is Concepción, about 300 kilometres (200 mi) south of Santiago. Generally cities like Temuco are considered to be located in the south despite being relatively close to the geographical center of Chile. This is mainly because mainland Chile ended in La Frontera until the occupation of Araucanía (1861–1883). Similarly, the Southern Chile wine region is close to the geographic center of the country, encompassing wine-growing areas in the Bío Bío Region and Araucanía Region.

Southern Chile may also refer to the Zona Sur region between Biobío and Chacao Channel, which is often also called the Chilean Lake District. It may also refer to the Zona Austral, also called the Extreme South.

View the full Wikipedia page for Southern Chile
↑ Return to Menu

Chilean Lake District in the context of Llanquihue glaciation

The last glacial period and its associated glaciation is known in southern Chile as the Llanquihue glaciation (Spanish: Glaciación de Llanquihue). Its type area lies west of Llanquihue Lake where various drifts or end moraine systems belonging to the last glacial period have been identified. The glaciation is the last episode of existence of the Patagonian Ice Sheet. Around Nahuel Huapi Lake the equivalent glaciation is known as the Nahuel Huapi Drift.

The preceding interglacial is known as the Valdivia interglacial after its type locality of Valdivia.

View the full Wikipedia page for Llanquihue glaciation
↑ Return to Menu