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Geography

Structure of Himalaya

Structure of Himalayas: Complete Guide to Mountain Formation

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The Himalayas represent one of Earth’s most complex mountain systems, formed through tectonic collision between Indian and Eurasian plates. This massive folded mountain chain spans 2,500 km and consists of three main divisions: Greater Himalayas (highest peaks), Lesser Himalayas (medium height ranges), and Outer Himalayas (Shivalik foothills). The structure includes five major tectonic zones from the Indus-Tsangpo Suture Zone in the north to the Sub-Himalayas in the south, each characterized by distinct geological formations and thrust systems.

Planets and dwarf planets of our solar system (Milky Way)

Planets of the Solar System: Definitions, Classifications & Key Facts

Planets are solid celestial bodies orbiting the Sun in elliptical orbits. They reflect sunlight but do not emit their own light. Our Solar System includes eight major planets classified as terrestrial (rocky) and Jovian (gaseous) planets, each with unique features and characteristics.