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Parts of the The Andes range has many active volcanoes distributed in four volcanic zones separated by areas of inactivity. Láscar erupted ash and pyroclastic flows in 1993 and was still active in 2012. At glacial times, however, c. 20,000 years ago, the glaciers were over ten times longer. D'Altroy, Terence N. The Incas. This results in frequent shallow focus earthquakes that get deeperas the ocean plate descends further, defining a zone of earthquake foci known as a Benioff zone.As subduction of the Nazca Plate continues, some of the sediments that accumulated on the ocean floor (together with some of the ocean crust) are scraped off and forced (accreted) onto the South American Plate in a process called “obduction”. Continued subduction of the Nazca Plate brings sea water, locked in the ocean crust, deep into the mantle. The northern Andes are typically rainy and warm, with an average temperature of 18 °C (64 °F) in Colombia. Rundsch. The climate is known to change drastically in rather short distances. As the plate heats up the water is liberated, lowering the melting point of the mantle and causing partial melting. Part III: South America, Asia, Africa, Australia, Antarctica. Development in Quaternary Science, vol. Where the two plates meet, the denser oceanic lithosphere of the Nazca Plate is forced down and under the more buoyant continental lithosphere of the South American Plate, descending at an angle into the mantle in a process called subduction.

For other uses, see The Andes mountain range, as seen from an airplane, between Santiago de Chile and Mendoza, Argentina, in summer. A long series of cultural development culminated in the expansion of the Devastated by European diseases to which they had no In modern times, the largest cities in the Andes are The rough terrain has historically put the costs of building However, there is one railroad that connects Chile with Peru via the Andes, and there are others that make the same connection via southern Bolivia. About 250 million years ago the crustal plates constituting the Earth’s landmass were joined together into the supercontinent Pangaea. A) a continental-continental convergent B) a continental-continental divergent C) an oceanic-oceanic convergent D) an oceanic-continental convergent E) a ), 735–738. 15 (Quaternary Glaciation – Extent and Chronology, A Closer Look, Eds: Ehlers, J.; Gibbard, P.L. See railroad maps of that region. Elsevier B.V., Amsterdam, pp. Some of these were built during a For decades, Chile claimed ownership of land on the eastern side of the Andes.

The first stage in the development of an Andean type mountain belt occurs prior to the formation of the subduction zone.

Also, by early sowing, maize can be cultivated higher up in the mountains (up to 3,800 m (12,500 ft)).

The Andes mountains were formed as a result of a convergence of plate tectonics. This produces magma, which rises and may be erupted explosively as andesite at the surface.Andesitic magma is less dense than the surrounding material, and can have a temperature of 1000Andean volcanoes such as the stratovolcano Láscar, in northern Chile, are a good example of this type of activity. ), Quaternary Glaciation— Extent and Chronology. Geomorphological and geophysical investigation of a complex rock glacier system—Morenas Coloradas valley (Cordon del Plata, Mendoza, Argentina)Kuhle, M. (2011): The High-Glacial (Last Glacial Maximum) Glacier Cover of the Aconcagua Group and Adjacent Massifs in the Mendoza Andes (South America) with a Closer Look at Further Empirical Evidence.

59) The Andes Mountains are an example of _____ plate boundary. On the east side of this section of the Mendozina Andes, they flowed down to 2,060 m (6,760 ft) and on the west side to about 1,220 m (4,000 ft) above sea level.The Andes are rich in fauna: With almost 1,000 species, of which roughly 2/3 are The Andes Mountains form a north–south axis of cultural influences. The largest glaciers, as e.g.

The highest peak is Aconcagua of Argentina (see below). The mountains have erupted at some distance from the contact-zone where the ‘down-rafting’ (subduction) of the Nazca plate heats, and starts to remelt, and where partial-melting, and expansion occur. (Eds. Along their length, the Andes are split into several ranges, separated by intermediate The Andes Mountains are the highest mountain range outside Asia. This is where two tectonic plates are moving toward each... See full answer below. The Andes are the result of tectonic plate processes, caused by the subduction of oceanic crust beneath the South American Plate. The effect of the collision of the two plates deforms the leading edge of the South American Plate by folding the rocks.