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Sial, or the "sial" layer, refers to the lighter, less dense part of the Earth's crust primarily composed of silicate minerals. This layer is found in continental crust, which underlies landmasses and is distinct from the denser oceanic crust known as "sim." Sial is primarily located beneath continents and mountainous regions, contributing to the formation of landforms and geological structures.

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The sima layer is found beneath the sial layer because it is denser and rich in magnesium and iron minerals, making it heavier. This difference in composition and density creates the stratification of Earth's crust, with sima underlying sial.


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Sial consists of the minerals silicon and aluminium and it is the outermost lighter part of the crust. while sima consists of the minerals silicon and magnesium and it is the lower part of the crust.


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