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.=========================================The Himalayan mountain range is a vast system in Asia known for its towering peaks, including the world's highest, Mount Everest. Formed by the collision of the Indian and Eurasian tectonic plates, they extend across several countries and are divided into three main parts: the Himadri, Himachal, and Shiwaliks. The Himalayas are geologically significant, home to glaciers, and act as a major influence on regional climate and water systems.
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.Geographic extent and formation Formation: The Himalayas began forming 40 to 50 million years ago when the Indian and Eurasian tectonic plates collided, a process that continues today and is responsible for their immense height.  Extent: They stretch approximately \(2,900\text{\ km}\) (\(1,800\) miles) across northern Pakistan, northern India, Nepal, Bhutan, and northern China.  Structure: The range is typically divided into three parallel sub-ranges: the Greater Himalayas (Himadri), the Lesser Himalayas (Himachal), and the Outer Himalayas (Shiwaliks).  Key features Highest peaks: The Himalayas contain many of the world's highest mountains, including Mount Everest (the highest on Earth), Kanchenjunga, and Nanga Parbat.  Glaciers: The range is the source of major glaciers, such as the Gangotri, Khumbu, and Zemu Glaciers.  Rivers: Many of Asia's major rivers, including the Indus, Ganges, and Brahmaputra, originate in the Himalayas.  Climate and ecology Climate influence: The Himalayas block cold winds from Central Asia and force the monsoon winds to shed their moisture, which greatly impacts the climate of the Indian subcontinent.  Biodiversity: The region supports diverse plant and animal life, with ecosystems ranging from tropical rainforests in the foothills to alpine zones at higher elevations. 
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