Early scientific theories regarding the Earth's formation fall into two broad philosophical schools:
A. Monistic (Single Star) Hypotheses:
- The Nebular Hypothesis (Immanuel Kant 1755, revised by Pierre-Simon Laplace in 1796): Asserted that the planets were formed out of a slowly rotating, hot, flattened primordial cloud of gas and dust (called a Nebula) associated with a youthful sun. As the nebula cooled, it contracted and spun faster, throwing off concentric rings of matter that condensed into planets.
- Modified Nebular Model (Otto Schmidt in Russia & Carl Weizsacker in Germany, 1950): Replaced the pure gas cloud with a solar nebula consisting of hydrogen, helium, and cosmic dust. Friction and collision of dust particles caused a disk-shaped cloud to form, and planets formed through accretion.
B. Dualistic (Binary / Two Star) Hypotheses:
- The Planetesimal Hypothesis (Chamberlin and Moulton, 1900): Proposed that a wandering companion star approached the proto-sun. The intense gravitational tidal pull of the passing star pulled out a cigar-shaped filament of solar matter. As the star sailed away, this separated material condensed into tiny solid bodies called Planetesimals, which accreted into planets.
- Sir James Jeans & Sir Harold Jeffreys: Refined this as the Tidal Hypothesis.