Geological Heat Flow increased compared to current eon
Residual heat from planetary accretion
Formation of the metallic core
Increased decay of radioactive elements (Half-life)
Reduced plate tectonics
Increase viscosity of mantle due to removal of water
Continents only appeared at the end of the Archean period
Atmosphere begins with 0.001% free oxygen compared to modern levels
Abiogenesis (The origins of life) began,due to Reduction in the harshness on Earth allowed for the formation of life, Multiple theories: Panspermia/Primordial Soup (Miller-Urey Experiment)