Despite the obvious interpretation of the title that studying the early Earth IS cool, there is now additional evidence that the early Earth WAS much cooler than many people would have expected for newly accreted planetary body full of radioactive elements. In this new study by Trail et al., they develop a new geothermometer for the ancient zircons that have been dated into the Hadean Eon (the oldest, >3.85 billion years). With this they show that some of these oldest-discovered-zircons have crystallized from a cool melt (for rocks to be cool and molten, they need to be rich in water), thus bolstering another argument by John Valley et al., (full disclosure: JV was a former committee member for me) that the early Earth was cool enough to have liquid water on the surface and a functioning rock cycle long before people had imagined.
Both of these studies are extremely interesting because the zircons they have studied seem to indicate that there was a functioning rock cycle as far back as 4.4 billion years (only ~150 million years after formation), of which these zircons were a part of, but we have no complete rocks older than about 4 billion years (the Acasta gneiss in Canada), leaving us with a giant gap in the geological record. What happened to all these older rocks, and if they are all gone, how have tiny bits of them survived while the main bodies were lost? Verdict: early Earth still cool.

Image by A. Valley and M. Diman from here

