What does it look like?
What is it?
Deeper into the Earth’s interior, and with the pressure building, at 525 km under another big change in the crystal structures of the minerals there occurs. Wadsleyite transforms to ringwoodite, which is has a structure known as a ‘spinel structure’. We’ve met the spinel structure before but in a very different context, lithium titanate a potential long lasting battery material. Ringwoodite is name in honour of Ted Ringwood, an Australian experimental geophysicst who predicted the phase transitions in olivine that we’ve been describing.
Where did the structure come from?
Like the wadsleyite structure, this crystal structure of ringwoodite has come from an in situ high-pressure study, and is #9001574 in the open crystallographic database.