Earth's crust is dominated by just two elements—oxygen and silicon—which together make up approximately 75% of its mass; oxygen bonds within minerals while silicon forms the silicate framework, and this distribution pattern, first systematically studied by Frank Wigglesworth Clarke in the early 1900s, explains why some elements like iron and aluminum are abundant and economically accessible while precious metals like gold and platinum are rare and costly due to their affinity for iron and sinking into Earth's core during planetary differentiation.
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Earth's Crustal Abundance | Distribution Of ElementsAdded:
Two elements dominate Earth's crust.
What if I told you two elements make up 75% of it?
Earth's crustal abundance means the relative concentration of chemical elements in the outermost solid layer.
Oxygen and silicon together are about 75%.
Oxygen bonds in minerals. [music] Silicon builds the silicate framework.
In the early 1900s, Frank Wigglesworth Clarke, the father of geochemistry, compiled the first systematic estimate.
>> [music] >> Later, A.P. Vinogradov and others refined them by studying rocks from granite to basalt.
They found iron and aluminum are also common, fueling large-scale mining.
But precious metals like gold and platinum are rare.
During planetary differentiation, many sank into Earth's iron core.
This is why some materials are abundant and cheap, others scarce and costly.
>> [music] >> Like and subscribe for more free science learning videos.
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