โ ๐ Earth science ยท usually met in Std 7-12
The Earth's surface is broken into plates that move a few centimetres a year. Everything dramatic in geology happens where they meet.
The rigid outer shell is divided into plates that ride on the slowly flowing mantle beneath. Where they pull apart, new crust forms โ mid-ocean ridges. Where they collide, one may slide beneath the other, producing volcanoes and deep trenches, or neither gives way and the crust crumples upward into mountains. Where they slide past each other, the friction builds until it releases as an earthquake.
The Himalaya are the clearest example anywhere. The Indian plate broke from the ancient southern landmass, travelled north, and ran into Asia around fifty million years ago. It is still pushing, which is why the Himalaya are still rising and why the region is seismically active. Wegener proposed continental drift in 1912 and was dismissed because he had no mechanism; sea-floor spreading supplied it half a century later.
Want to see it moving? Search YouTube for โPlate tectonicsโ โ โ we send you to the search rather than to one video, because a link to one video eventually rots.
This entry was written for Star Student in our own words โ it is a summary, not a source. Here is where the people who actually hold these facts keep them. Go and check.
Your own textbook โBalbharati publishes the textbooks free to read online. Your chapter is the thing to check first โ an encyclopedia is a summary, and the syllabus is the syllabus. Geological Survey of India โRocks, earthquakes, the Himalaya and seismic zoning. India Meteorological Department โThe monsoon, rainfall and cyclone warnings, from the department that issues them.Last gone through: 1 October 2026 ยท How these entries are written