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The tallest mountain in the world is Mount Everest, which stands at 29,032 feet (8,849 meters) tall.
The height of a mountain is typically measured from sea level to its summit using a variety of techniques, including satellite imagery, ground surveys, and trigonometric calculations.
The height of a mountain can be affected by factors such as tectonic activity, erosion, and climate. For example, tectonic forces can cause mountains to rise, while erosion can wear down their peaks over time.
Yes, it is possible for a mountain to grow taller over time. This can occur through geological processes such as volcanic eruptions or tectonic movements.
Accurate measurements of mountain heights are important for several reasons. They can help with navigation and mapping, understanding geological processes, and studying the effects of climate change on mountain ecosystems.