Andes Mountains

The Andes are a mountain system along western South America, extending about 8,900 kilometres from the continent’s southern tip to the Caribbean coast. Their landscape includes parallel ranges, high plateaus and deep valleys; the highest summit is Aconcagua, at about 6,959 metres. The range formed as the oceanic Nazca Plate descended beneath the South American Plate, a process still associated with earthquakes and volcanism. Strong changes in latitude and elevation create diverse climates and ecosystems, including the Tropical Andes biodiversity hotspot, and the mountains supply the headwaters of major river systems such as the Amazon and Orinoco.

Last updated
15 October 2026
Confidence
High (95%)
Sources
6
Versions
1
This article was researched and drafted with AI assistance and checked by an automated review pass. It is not guaranteed to be accurate — verify important facts against the references below.

Extent and landforms

The Andes run for roughly 8,900 kilometres along the western edge of South America, from the southern end of the continent to its northern Caribbean coast. They are not a single ridge: the system consists of multiple parallel and transverse cordilleras, high plateaus and intervening basins. A commonly used regional division distinguishes the Southern, Central and Northern Andes, although geographers do not agree on a single set of boundaries. In the central part of the range, the Altiplano is a high interior plateau between major mountain chains. Aconcagua, on the Argentina–Chile border, is the highest summit, rising about 6,959 metres above sea level.

Geological formation and hazards

The Andes are an active example of mountain building at a convergent plate boundary. The oceanic Nazca Plate moves toward and descends beneath the continental South American Plate. Compression and deformation of the overriding crust have helped uplift the mountain chain, while melting above the descending plate feeds a volcanic arc along much of the western margin. The continuing tectonic boundary produces earthquakes as well as volcanoes; its geological behaviour varies along the length of the range. The Andes therefore form part of the active Pacific margin of South America, rather than a set of mountains shaped only by ancient, completed processes.

Climate, water and biodiversity

The Andes cross a wide range of latitudes and elevations, so climate and vegetation change markedly from one region and slope to another. High elevations include cold grasslands, snow and glaciers, while lower slopes in the tropics include forests. In the tropical Andes, steep environmental gradients and isolated habitats support unusually rich biodiversity and many species found nowhere else. Mountain catchments also feed large river systems: the Tropical Andes are an important water source for the main stems of the Amazon and Orinoco. These connections make the range significant well beyond its peaks, linking highland ecosystems to downstream communities and lowland habitats.

People and cultural landscapes

People have built communities and ways of life across the Andes’ varied elevations and climates. The Tropical Andes biodiversity hotspot alone is home to more than 40 Indigenous groups, whose communities have important roles in land use and regional life. Agriculture, settlements, transport routes and resource use all interact with steep terrain and sensitive ecosystems. The Historic Sanctuary of Machu Picchu in Peru illustrates one such relationship: UNESCO describes an Inca cultural landscape in the eastern Andes where architecture, terraces, trails and the surrounding mountain environment are closely connected. It is one landmark within a much larger and culturally diverse mountain region.

Key facts

Approximate length
About 8,900 kilometres, along the western side of South America.
Highest summit
Aconcagua, approximately 6,959 metres above sea level, on the Argentina–Chile border.
Tectonic setting
The Nazca Plate descends beneath the South American Plate, driving uplift and contributing to earthquakes and volcanism.
Regional importance
The Tropical Andes are recognized as a biodiversity hotspot and supply water to the main stems of the Amazon and Orinoco rivers.

Ask about this article

Answers use only “Andes Mountains” and its references, with citations.

References

  1. 1.
    Andes Mountains

    Encyclopaedia Britannica · other · reliability: high · retrieved 15 October 2026

    Supports: Reference overview of the Andes’ extent, relief, highest summit, regional divisions, geology and physical environment.

  2. 2.
    Seismicity of the Earth 1900-2013, seismotectonics of South America (Nazca Plate Region)

    U.S. Geological Survey · other · reliability: high · retrieved 15 October 2026

    Supports: Geological report describing Nazca–South American plate subduction, Andean uplift, the volcanic arc and seismicity along the margin.

  3. 3.
    Oceanic/Continental: The Andes

    The Geological Society of London · other · reliability: high · retrieved 15 October 2026

    Supports: Explains subduction of the Nazca Plate beneath South America and associated mountain building, earthquakes and volcanism.

  4. 4.
    Tropical Andes

    Critical Ecosystem Partnership Fund (CEPF) · other · reliability: high · retrieved 15 October 2026

    Supports: Describes the Tropical Andes biodiversity hotspot, its Indigenous communities and the mountains’ role as a source for Amazon and Orinoco waters.

  5. 5.
    Biodiversity

    Food and Agriculture Organization of the United Nations (FAO), Mountain Partnership · other · reliability: high · retrieved 15 October 2026

    Supports: Overview of mountain biodiversity and its ecological, cultural and agricultural importance, including Andean crop diversity.

  6. 6.
    Historic Sanctuary of Machu Picchu

    UNESCO World Heritage Centre · other · reliability: high · retrieved 15 October 2026

    Supports: Authoritative description of Machu Picchu’s Inca cultural landscape and its setting in the eastern Andes.

References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.

Article history

  1. Version 115 October 2026 · EditorCreated by Zapia