Formation of the Earth
ICSE · Class 11 · Geography
Quick revision notes for Formation of the Earth — ICSE Class 11 Geography. Key concepts, formulas, and definitions for last-minute revision.
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Age of the Earth
- The Earth is generally believed to be 4 to 5 billion years old.
- Very little is known about conditions during the first one billion years before the crust consolidated.
- Modern scientific methods for estimating the Earth's age have been in use for about two centuries.
Hypotheses of Origin of the Earth
- Earth's origin is inseparable from the origin of the solar system as a whole.
- Most scholars agree that Earth, like other planets, originated from the Sun.
- Hypotheses can be broadly classified into: Nebular/Gaseous (Kant, Laplace), Catastrophist/Two-Star (Chamberlin-Moulton, Jeans-Jaffreys), and Modern (Alfven, Otto Schmidt, Big Bang).
Detailed Analysis of Each Hypothesis
- KANT'S GASEOUS HYPOTHESIS (1755): Primordial matter = evenly distributed cold particles. Gravitational pull → collision → angular velocity → rotation → gaseous mass emitting light → rings separate due
- LAPLACE'S NEBULAR HYPOTHESIS (1796): Primordial matter = intensely hot rotating gaseous mass (Nebula). Cooling → volume decreases → rotation speed increases → centrifugal force exceeds gravity → ring
- CHAMBERLIN-MOULTON PLANETESIMAL HYPOTHESIS (1904): Two bodies — proto-sun (spiral shaped) and larger companion star. Companion star's gravity + Sun's eruptive tendency → ejection of solar jets → plane
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