Isostasy — Concept Maps
ICSE · Class 11 · Geography
4 concept maps of Isostasy for ICSE Class 11 Geography, each also written out as a text outline. Part of the ICSE Class 11 Geography syllabus.
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Isostasy: Complete Concept Overview
The map in words
- Isostasy
- Definition
- Gravitational equilibrium
- Equal mass beneath equal areas
- State of balance
- Historical Background
- Bouguer 1735
- Everest survey 1854
- Dutton 1889 term coined
- Airy Pratt 1855
- Evidence for Theory
- Plumb line deflection
- Less than expected gravity
- Crustal root observations
- Seismic studies
- Airy Concept
- Floating blocks
- Varying depth uniform density
- Mountain roots
- Hydrostatic equilibrium
- Pratt Concept
- Varying density uniform depth
- Compensation level
- Density inversely proportional
- Mercury analogy
- Crustal Layers
- Sial light rocks
- Sima dense rocks
- Continental vs oceanic
- Mohorovicic discontinuity
- Modern Understanding
- Holmes seismic evidence
- Root confirmation
- Crustal thickness variation
- Temperature constraints
- Applications
- Isostatic rebound
- Delta subsidence
- Mountain stability
- Earthquake prediction
- Definition
Isostasy: Concept Overview and Key Components
The map in words
- Isostasy Theory
- Historical Development
- Pierre Bouguer 1735
- Andes Expedition
- Plumb line deflection
- Dutton 1889
- First used term
- American geologist
- George Everest 1854
- Indo-Gangetic survey
- Himalayan observations
- Pierre Bouguer 1735
- Core Concepts
- Gravitational Equilibrium
- Equal mass balance
- Floating landforms
- Crustal Composition
- Sial layer
- Sima layer
- Compensation Level
- Uniform density below
- Variable above
- Gravitational Equilibrium
- Two Main Models
- Airy Root Hypothesis
- Varying root depths
- Similar densities
- Mountain roots
- Pratt Density Model
- Uniform depths
- Varying densities
- Inverse relationship
- Airy Root Hypothesis
- Supporting Evidence
- Geodetic Surveys
- Plumb line anomalies
- Gravitational measurements
- Seismic Studies
- Crustal roots confirmed
- Layer thickness mapping
- Modern Technology
- GPS measurements
- Continuous monitoring
- Geodetic Surveys
- Applications
- Mountain Formation
- Crustal Subsidence
- Ocean Basin Structure
- Earthquake Understanding
- Historical Development
Isostasy – Complete Concept Overview
The map in words
- ISOSTASY
- Definition and Origin
- German word Isostasios
- Meaning Equipoise
- Coined by Dutton 1889
- Gravitational equilibrium
- Historical Evidence
- Pierre Bouguer 1735
- Andes Chimborazo
- Less deflection than expected
- Sir George Everest 1854
- Kaliana to Kalianpur
- 603 km apart
- 5.23 vs 15.885 arc seconds
- French Surveyors
- Deflection away from mountains
- Towards Bay of Biscay
- Pierre Bouguer 1735
- Airy's Concept 1855
- Sial floats on Sima
- Same density 2.67
- Varying depth roots
- Iceberg analogy
- Wooden block experiment
- Root is 8 times height
- Supported by Holmes and seismic data
- Pratt's Concept 1855
- Varying density
- Same depth uniform
- Height inversely proportional to density
- Metal pieces in mercury
- Mountains least dense
- Oceans most dense
- Holmes Views 1978
- Supported Airy
- Seismic evidence
- Mountains 50 to 60 km roots
- Coastal plains 30 km sial
- Ocean floors no sial
- Level of Compensation
- Below this no density variation
- Equal mass under equal areas
- Airy roots end here
- Pratt blocks bottom here
- Definition and Origin
Isostasy
The map in words
- Isostasy
- Meaning of the term
- Basic idea
- Dutton
- Pierre Bouguer
- Sir George Everest
- Plumb-line deflection
- Kaliana and Kalianpur
- Himalayan gravitational anomaly
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