Bío-Bío Valley

Bío-Bío Valley is comprised within the region which is the southern boundary of the viticultural zone of the Central Valley. Its boundaries are, to the north the Maule administrative region and to the south the Araucanía administrative region.

The Bío-Bío Valley is comprised within the Bío-Bío administrative region which is the southern boundary of the viticultural zone of the Central Valley, between 36º 00′ and 38º 30’ latitude south. Its boundaries are, to the north the Maule administrative region and to the south the Araucanía administrative region.

Denomination of Origin: Bío Bío

Region: Southern Region

Sub-Region: Bío Bío

Complementary Areas: Entre-Cordilleras, Andes.

Soils

On the coast there are soils developed from marine terraces, flat or with soft slopes of reddish brown colour associated to other less developed soil types. Inland, in the highlands between Los Ángeles and Loncoche, the coastal sector, facing Moche Island, and in the heights of the Coastal Range the soils are thin and show drainage problems. In the eastern sector they are moderately deep and have high clay content.

In the inland valleys soils are alluvial and moderately developed between the cities of Los Ángeles and Malleco, next to soils formed from coarse-grained basaltic sands. These soils are highly permeable and there also are sectors with high groundwater levels. In the precordillera and the sectors of stronger relief of the Andes there are coarse-grained soils derived from volcanic accumulation. In the precordillera facing the city of Los Ángeles and down to Temuco, there are soils derived from volcanic ashes, known as “trumaos”. These are rich soils, deep, with high organic matter content and a great moisture retention capacity.

Climate

The Southern vine-growing Region is characterised, by a cold temperate climate with important differences between the coast and its inland valleys. The orographic conditions of the region do not allow winds from the ocean to enter the sunken basin; this causes a wide thermal variation between them. The rains increase as the territory continues towards the south increasing the diversity and amount of vegetation and the presence of rivers of greater volume. In the southern viticultural region the average rainfall and high humidity at some times of the year provide better soils for agriculture and stock farming. The difference between the coast and the sunken basin is still very noticeable as to humidity, thermal variation as well as increased rainfall. The southern viticultural region has two dominant river basins which form the hydrographic system of the region: the Itata and Bio Bío rivers, both born in the Andes and originating homonymous valleys. There are also lesser river basins, such as that of the Andalién River.

Two main watercourses form the Itata River: the Ñuble and Itata rivers. The Itata River is 180 km long, including its two affluents, the Cholguán and Huépil. The Itata River has a mixed flow pattern, since its main affluents are born in the mountain range and precordillera of the Andes and are fed spring thaws and winter rainfall. This River crosses the longitudinal valley and has a high waterfall due to an abrupt change of level of the land. In its lower reaches its main affluent is the Lonquén River, which drains the cordilleran sector of the coast to the north.

The Bío Bío River has one of the largest basins of the country and a mixed flow pattern with spates in winter and spring; it is 380 kilometres long. It is born from the Andes in the region of the Araucanía, draining two mountain lakes, the Icalma and the Galletué. In its middle course it receives the contribution of the Duqueco and the Bureo. Going through the longitudinal valley, the Bío Bío River changes course as it comes against the Coastal Range, and then it returns to its normal course in the confluence with the Vergara River. Near the coast the river receives the waters of the Laja River, its largest affluent. In its lower reaches, near the city of Concepción, the river again changes its course reaching the sea south of the Hualpén hills.

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