Major geological units (left) in Bolivia coincide with topography (right) Geological units:
Quaternary deposits
Quaternary volcanics
Tertiary deposits
Cretaceous-Tertiary volcanics
Cretaceous age rocks
Devonian age rocks
Silurian age rocks
Ordovician-Silurian age rocks
Precambrian undifferentiated
The geology of Bolivia comprises a variety of different lithologies as well as tectonic and sedimentary environments. On a synoptic scale, geological units coincide with topographical units. The country is divided into a mountainous western area affected by the subduction processes in the Pacific and an eastern lowlands of stable platforms and shields. The Bolivian Andes is divided into three main ranges; these are from west to east: the Cordillera Occidental that makes up the border to Chile and host several active volcanoes and geothermal areas, Cordillera Central (in some contexts also called Cordillera Oriental) once extensively mined for silver and tin and the relatively low Cordillera Oriental that rather than being a range by its own is the eastern continuation of the Central Cordillera as a fold and thrust belt. Between the Occidental and Central Cordillera the approximately 3,750-meter-high Altiplano high plateau extends.[1] This basin hosts several freshwater lakes, including Lake Titicaca as well as salt-covered dry lakes that bring testimony of past climate changes and lake cycles. The eastern lowlands and sub-Andean zone in Santa Cruz, Chuquisaca, and Tarija Departments was once an old Paleozoic sedimentary basin that hosts valuable hydrocarbon reserves. Further east close to the border with Brazil lies the Guaporé Shield, made up of stable Precambrian crystalline rock.
^"The Use of Solar Energy for Improving the Living Conditions in Altiplano/Argentina" (PDF). Archived from the original (PDF) on 2011-07-19. Retrieved 2010-05-25.
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The geologyofBolivia comprises a variety of different lithologies as well as tectonic and sedimentary environments. On a synoptic scale, geological units...
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American Plate. Geological research suggests that the South American Plate is moving west away from the Mid-Atlantic Ridge: "Parts of the plate boundaries...
foreland basin development and the history of Andean crustal shortening in Bolivia". Geological Society of America Bulletin. 115 (1): 58–77. Bibcode:2003GSAB...
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back-arc basin during the Ordovician. This basin went from Peru, through Bolivia to northwestern Argentina. The basin collected sediments from the Famatinian...
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