Central Andes
Quick Summary
The Andes Mountains are a young, formidable mountain system stretching along the western edge of South America, forming a continuous barrier from north to south. This range is the longest continental mountain range in the world, second only to the Himalayas in average elevation, with many peaks exceeding 20,000 feet (6,100 meters).1
The Andes are geologically active, formed by the collision of the South American and Nazca plates. This process, which began around 25 million years ago, has resulted in significant volcanic activity and frequent earthquakes. The mountain system is broadly divided into the Northern, Central, and Southern Andes, each with distinct geological and physiographic characteristics.23
The Central Andes, encompassing Peru and Bolivia, are known for the vast Altiplano, a high plateau situated between two major ranges. This region experiences a wide range of climates due to varying altitudes, from hot rainforests and deserts to tundralike puna and polar conditions at the highest elevations. The diverse environments support a variety of plant and animal life, with distinct altitudinal bands of vegetation and fauna.1345
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