The Andes in western South America is an example of a landform that arises from the movement of the tectonic plates.
The Andes mountain range is the mountain range that runs along South America's whole Pacific Ocean coast in the west. It is the world's longest continental mountain range, stretching 8500 km.
It was created by the convergence of the South American and Nazca plates towards the end of the Late Cretaceous, at the end of the Mesozoic era. In the relief configuration, seismic movements and consequent volcanic activity have been more significant than external erosive processes.
There are high mountain ranges in the existing morphology, as well as broad high plateaus, deep longitudinal valleys, and vast mountain ranges. Except for in the Argentine-Chilean Andes, transversal valleys are uncommon.
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Explanation:La subducción es el proceso de hundimiento de una placa litosférica bajo el borde de otra placa, formándose los llamados límites convergentes entre placas. La placa subducida, la que se hunde, suele estar formada por corteza oceánica, más delgada y densa que la continental. La subducción ocurre a lo largo de amplias zonas de subducción que en el presente se concentran especialmente en el entorno del océano Pacífico, en el llamado cinturón de fuego del Pacífico, pero también hay zonas de subducción en partes del mar Mediterráneo, las Antillas, las Antillas del Sur y la costa índica de Indonesia.
All of them Plays an equal and important role to support life on Earth..
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Explanation
When the sun, moon, and Earth are in alignment (at the time of the new or full moon), the solar tide has an additive effect on the lunar tide, creating extra-high high tides, and very low, low tides — both commonly called spring tides. ... A similar situation occurs between the Earth and the sun.
