Chilean Central Valley
The Central Valley (Spanish: Valle Central), Intermediate Depression, or Longitudinal Valley is the depression between the Chilean Coastal Range and the Andes Mountains. The Chilean Central Valley extends from the border with Peru[A] to Puerto Montt in southern Chile, with a notable interruption at Norte Chico (27°20'–33°00' S). South of Puerto Montt the valley has a continuation as a series of marine basins up to the isthmus of Ofqui. Some of Chile's most populous cities lies within the valley including Santiago, Temuco, Rancagua, Talca and Chillán.
Northern section (18°30'–27°20' S)
In northernmost Chile the central valley is made up of the Pampitas,[B] a series of small flats dissected by deep valleys. Inmediately south of the Pampitas, in Tarapacá Region and northern of Antofagasta Region, the Central Valley is known as Pampa del Tamarugal. Contrary to the Pampitas valleys descending from the Andes do not incise the plains but merge into the surface of Pampa del Tamarugal at a height of c. 1500 m. The westernmost portion of Pampa del Tamarugal has a height of 600 m. This western part contain a series of raised areas called pampas and basins containing salt flats. Interconnecting basins are important corridors for communication and transport in northern Chile.
South of Loa River the valley continues, flanked by Cordillera Domeyko to east, until it is ends at the latitude of Taltal (25°17' S). It re-appears around Chañaral (26°20' S) as an isolated basin surrounded by mountains and hills. This 250 km long and up to 70 km wide basin is called Pampa Ondulada or Pampa Austral. As the Pampa Ondulada is extinguished at Copiapó River (27°20' S) in the Norte Chico region running south of this river there is no proper Central Valley, only a few narrow north-south depressions that align with geological faults.
Central section (33°00'–41°30' S)
The main portion the Central Valley extends from Tiltil (33°05' S) near Santiago to Temuco (38°45' S). The Coast Range and the Andes almost merge in two locations: one between Santiago and Rancagua and another between San Fernando and Rengo. The result is the enclosure of the Central Valley into two smaller basins in the north: Santiago Basin and Rancagua Basin.
The valley runs an un-interrupted leght of 360 km from Angostura de Pelequén in the north to Bío Bío River (37°40' S) in the south. It broadens from 12 km at Molina (35°05' S) in the north to 74 km in the south at Laja (37°15' S) the relief being gently undulating. Conglomerate of Andean provenance cover large swathes of the Central Valley being less common to the west near the Coast Range. Occasionally the valley contains isolated hills and mountains made up of basement rocks. At the latitudes of Temuco the Coast Range is subdued to such degree the Central Valley coalesces with the coastal plains.
In the 110 km between Gorbea and Paillaco (c. 39–40° S) the Central Valley is inexistent as the region is instead crossed by a series of east-west mountainious ridges and broad fluvial valleys. South of this region the Central Valley re-appears in the south to extend into Osorno and Puerto Montt (41°30' S). This southern section is 190 km long from north to south. The Central Valley south of Bío Bío River has been influenced by volcanism and past glaciations giving origin to the ñadis and morraines that cover parts of the valley.
Southern marine basins (41°30'–46°50' S)
South of Puerto Montt the continuation of the Central Valley is made up of a series of marine basins including Reloncaví Sound, Gulf of Ancud, and the Gulf of Corcovado that separates Chiloé Island from the mainland. Further south the valley runs as the narrow Moraleda Channel. Emerged portions include numerous small islands plus the eastern coast of Chiloé Island and Taitao Peninsula east of Presidente Ríos Lake, including the Isthmus of Ofqui. (46°50' S).
- An aerial Google view of the Chilean Central Valley. Argentina lies to the east of the Andes range
- Chilean National Tourism Service (in Spanish)
- Chilean Meteorological Service (in Spanish)
- Evenstar, L.A.; Mather, A.E.; Hartley, A.J.; Stuart, F.M.; Sparks, R.S.J.; Cooper, F.J. (2018). "Geomorphology on geologic timescales: Evolution of the late Cenozoic Pacific paleosurface in Northern Chile and Southern Peru". Earth-Science Reviews. doi:10.1016/j.earscirev.2017.04.004.
- Börger, p. 40.
- Börger, p. 41.
- Brüggen, p. 6.
- Börger, p. 42.
- Börger, p. 43.
- Börger, p. 47.
- Brüggen, p. 5.
- Brüggen, p. 4.
- Brüggen, p. 2.
- Börger, p. 97.
- Börger, p. 99.
- Börger, p. 122.
- Börger, p. 123.
- Börger, p. 137.
- Börger Olivares, Reinaldo (1983). Geografía de Chile (in Spanish). Tomo II: Geomorfología. Instituto Geográfico Militar.
- Brüggen, Juan (1950). Fundamentos de la geología de Chile (in Spanish). Instituto Geográfico Militar.