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Snow-capped mountains are caused by elevation and temperature variations, where temperatures are low enough for snow to accumulate and persist throughout the year. As altitude increases, the air cools, leading to precipitation falling as snow rather than rain. The permanent snow cover, or glaciers, forms due to this accumulation of snow over time, often seen in ranges like the Himalayas and the Andes. These snow-capped peaks are not only breathtaking but also play a vital role in the Earth’s climate and water cycle.
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High-altitude mountains often have snow-capped peaks because temperatures at such elevations remain consistently low, even during warmer months. The cold atmosphere prevents snow from melting, allowing it to accumulate and persist year-round. These snow-covered peaks not only create stunning landscapes but also serve as vital sources of freshwater for surrounding regions through glacial melt, so we can say that option 2 is correct.
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