โ ๐ Earth science ยท usually met in Std 6-10
Crust, mantle, outer core and inner core โ worked out almost entirely from the way earthquake waves travel, because nobody has ever been more than a few kilometres down.
The crust is thin โ a few tens of kilometres under the continents, less under the oceans. Beneath it the mantle makes up most of the planet's volume: rock that is solid but creeps very slowly over geological time. The outer core is liquid iron and nickel, and its motion generates the Earth's magnetic field. The inner core is iron under such pressure that it stays solid despite being hotter still.
We know this because earthquake waves change speed and direction when they pass between materials, and some types cannot travel through liquid at all. Seismometers all over the world record what arrives and what does not, and the shadow that the liquid outer core casts is how its existence was discovered.
Want to see it moving? Search YouTube for โInside the Earthโ 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