The structure of the Earth is chemically divided into layers. The Earth has an outer silicate solid crust, a highly viscousmantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. ਇੱਕ ਫੁੱਲ-ਸਾਈਜ਼ ਵਰਜ਼ਨ ਲਈ ਤਸਵੀਰ ਉੱਤੇ ਕਲਿੱਕ ਕਰੋ, ਜਿਸ ਨੂੰ ਤੁਸੀਂ ਅਜ਼ਾਦੀ ਨਾਲ ਪੁਨਰ-ਵਰਤੋਂ ਕਰ ਸਕੋ ਅਤੇ ਸੁਧਾਰ ਸਕੋ. ਇਸਦੇ ਵਰਗੀਆਂ ਹੋਰ ਤਸਵੀਰਾਂ ਪ੍ਰਾਪਤ ਕਰਨ ਵਾਸਤੇ ਹੇਠਾਂ ਵਾਲੇ ਲਿੰਕ ਤੇ ਕਲਿੱਕ ਕਰੋ
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