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The extra heat was the result of a mix of remnant heat from planetary accretion, from the formation of the Earth's core, and produced by radioactive elements.
Most surviving Archean rocks are metamorphic or igneous.
Volcanic activity was considerably higher than today, with numerous lava eruptions, including unusual types such as komatiite.
Granitic rocks predominate throughout the crystalline remnants of the surviving Archean crust.
Like in a heterosexual set-up, trying to approach a gay guy and ask him for a date seems like a really calculated routine.
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The Cambrian marked a profound change in life on Earth; prior to the Cambrian, the majority of living organisms on the whole were small, unicellular and simple; the Precambrian Charnia being exceptional.
Complex, multicellular organisms gradually became more common in the millions of years immediately preceding the Cambrian, but it was not until this period that mineralized—hence readily fossilized—organisms became common.
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