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 the state of gravitational balance between different parts of the earth's crust. High landforms such as mountains and plateaus are made of lighter material and extend deeper into the earth, while low areas such as plains and ocean basins are made of denser material. The idea explains why
Key Concepts
Isostasy means equipoise or a state
Isostasy means equipoise or a state of balance. It describes the balance between the earth's surface features and the material below them.
The term was first used by
The term was first used by Dutton in 1889 to explain gravitational equilibrium between continents, oceans, mountains, plateaus, and plains on a rotati
Pierre Bouguer noticed during the Andes
Pierre Bouguer noticed during the Andes Expedition that the plumb-line near Chimborazo was deflected much less than expected.
Sir George Everest's 1854 survey
Sir George Everest's 1854 survey of the Indo-Gangetic plain showed a difference between astronomically measured latitude and triangulation measurement
This is the level below
This is the level below the earth's surface below which density does not vary. Above it, landforms of different sizes and densities are in balance.
Learning Objectives
- Understand the meaning and origin of isostasy.
- Learn how plumb-line observations led to the idea of crustal balance.
- Compare the views of Airy and Pratt on isostasy.
- Understand the concept of level of compensation.
- Recognize why higher landforms require deeper support below the surface.
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