EARTH
Lava Too Hot to Exist Today
~3.5 to 2.7 billion years ago
Archean · Paleoarchean
These lavas erupted so hot that they flowed like water rather than creeping like modern lava, and they crystallised into blades of olivine as long as a hand. Nothing like them has erupted since: the Earth's interior has cooled too far to produce them again.
Why it matters
These flows are a thermometer for the young Earth: they show, more directly than any other rock, how far the planet had cooled from its violent beginnings. They are also why most of the nickel we mine comes from rocks of this age.
Dating & uncertaintyDisputed
They erupted near 1,600 degrees, some three hundred degrees hotter than any lava today. Whether that requires a mantle hundreds of degrees hotter, or only wet rock melting at ordinary temperatures above a sinking plate, has been argued for fifty years. Water measured inside the crystals now favours the hot mantle.
Sources
- Grove & Parman (2004), Earth and Planetary Science Letters · Thermal evolution of the Earth as recorded by komatiites
- Sobolev et al. (2016), Nature · Komatiites reveal a hydrous Archaean deep-mantle reservoir
- Grosch & Viljoen (2023), Journal of African Earth Sciences · The discovery and petrogenetic significance of komatiites
Earth history as one day
05:29:5218 h 30 min before midnight
if Earth’s 4.54 billion years were compressed into a single day
See it on the timeline