UCL Mathematical & Physical Sciences



18 November 2013

Feldspar - labradorite (UCL Geology Collections)

This artifact from UCL's collections looks like it could be in outer space. But the interplay of light and chemistry that produces these shimmering colours has its feet firmly on -- or even in -- the ground. It is a close up of a polished sample of Labradorite, a type of mineral commonly found in the Earth's crust.

Feldspar - labradorite (UCL Geology Collections)

Labradorite is a type of feldspar. Feldspars are a family of common crystalline rocks, composed largely of aluminium, silicon and oxygen, with smaller quantities of sodium, potassium or calcium. Feldspars crystallise in hot magma as it cools down.

The green, shimmering quality of Labradorite (named after the region in Canada where they are commonly found) is caused by the structure of the mineral, which is made up of numerous thin sheets of transparent crystal.

Photo credit: UCL Geology Collections


High resolution image

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