Isostasy
ICSE · Class 11 · Geography
Quick revision notes for Isostasy — ICSE Class 11 Geography. Key concepts, formulas, and definitions for last-minute revision.
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1. Introduction and Definition of Isostasy
- Isostasy comes from the German word 'Isostasios' meaning 'in equipoise' or 'state of balance'
- The term was first used by American geologist Dutton in 1889
- Isostasy explains the gravitational equilibrium of Earth's landforms (mountains, plateaus, plains, oceans)
2. Historical Background: The Basis of Isostasy Theory
- Pierre Bouguer (1735) first observed that mountains don't pull gravity as strongly as expected—seeds of isostasy were sown here
- During the Andes Expedition, Bouguer found that the deflection of the plumb line near Chimborazo was much less than calculated
- Sir George Everest's Indo-Gangetic Plain Survey (1854) provided crucial evidence supporting the theory
3. Causes of Less Than Expected Gravitational Pull
- Airy and Pratt identified four main causes for the anomaly in gravitational pull:
- First cause (REJECTED): Lower density of mountains—assumed density was 2.67, but if lower, mountains would be 'hollow bubbles' (geologically impossible)
- Second cause (ACCEPTED): No heavy material beneath mountains; light material extends to great depth; mountains sink into heavy liquid below like floating objects
4. Airy's Concept of Isostasy
- Sir George Airy (1801-1892) was the Astronomer Royal who formulated his theory in 1855
- Airy followed the Law of Floatation—continents are composed of lighter sial floating on denser sima
- Key principle: Mountains are stable because lighter rocks extend as 'roots' deep into the denser substratum below
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