Isostasy
ICSE · Class 11 · Geography
Summary of Isostasy for ICSE Class 11 Geography. Key concepts, important points, and chapter overview.
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Overview
Isostasy is a fundamental concept in geology that explains how the Earth maintains gravitational equilibrium across its surface. The term comes from the German word 'Isostasios', meaning 'in equipoise' or 'state of balance'. This concept helps us understand why mountains, plateaus, plains, and ocean
Key Concepts
Isostasy refers to the state
Isostasy refers to the state of gravitational and mechanical equilibrium that exists between different parts of the Earth's crust. It is based on the
Sial refers to the lighter rocky
Sial refers to the lighter rocky material that makes up continental crust, primarily composed of silicon and aluminum compounds with a density of appr
Crustal roots are deep extensions
Crustal roots are deep extensions of lighter crustal material that project downward into the denser mantle material below mountains and other elevated
The level of compensation is
The level of compensation is an imaginary horizontal plane within the Earth below which there are no variations in density. Above this level, differen
Sir George Airy proposed in 1855
Sir George Airy proposed in 1855 that continents, made of lighter sial, float on denser sima following the principle of hydrostatic equilibrium. Accor
Learning Objectives
- Understand the concept of isostasy and its significance in explaining Earth's surface features
- Learn the historical development of isostasy theory through geodetic observations
- Compare and contrast Airy's and Pratt's models of isostatic equilibrium
- Understand the concept of crustal roots and compensation levels
- Analyze how different landforms maintain gravitational balance
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