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PHYSICAL GEOGRAPHY SAVINDRA SINGH, CH-2: SOLAR SYSTEM, CH-3: AGE OF THE…

- - - - EVOLUTION OF EARTH'S ATMOSPHERE
      - ORIGIN OF HEAT
    - - EVOLUTION OF CONTINENTS AND OCEAN BASINS
    - - EVALUATION
- - - - HAWIIN TYPE
      - STROMBOLIAN TYPE
      - VULCANIAN TYPE
      - PELEEAN TYPE
      - VISUVIUS TYPE
    - - LAVA FLOOD OR LAVA FLOW
      - MUD FLOW
      - FUMAROLES
- - - - A. ELEVATED FORMS
        
        VOLCANIC CONES
      - B. DEPRESSED FORM
        
        CRATERS AND CALDERAS
    - - A. LAVA PLATEAUX AND DOMES
      - B. LAVA PLAINS
- - - - TENSIONAL FORCES
        
        CRUSTAL FRACTURE
        
        CRACKING
        
        FAULTING (FAULTS)
        
        TYPES OF FAULT
        
        NORMAL FAULTS
        
        REVERSE FAULTS
        
        LATERAL OR STRIKE-SLIP FAULTS
        
        STEP FAULTS
      - COMPRESSIONAL FORCES
        
        CRUSTAL BENDING
        
        WARPING
        
        UPWARPING
        
        DOWNWARPING
        
        FOLDING (FOLDS)
        
        TYPES OF FOLDS
        
        SYMETRICAL FOLDS
        
        ASYMMETRICAL FOLDS
        
        MONOCLINICAL FOLDS
        
        ISOCLINAL FOLDS
        
        RECUMBENT FOLDS
        
        OVERTURNED FOLDS
        
        PLUNGE FOLDS
        
        FAN FOLDS
        
        OPEN FOLDS
        
        CLOSED FOLDS
        
        NAPPES
        
        CRUSTAL FRACTURE
    - - UPWARD MOVEMENT (EMERGENCE)
      - DOWNWARD MOVEMENT (SUBMERGENCE)
- - - - CHARACTERISTICS
      - CLASSIFIATION
        
        ON THE BASIS OF AMOUNT OF SILICA
        
        ACIDIC IGNEOUS ROCKS
        
        BASIC IGNEOUS ROCKS
        
        ITREMEDIATE IGNEOUS ROCKS
        
        ULTRA BASIC IGNEOUS ROCKS
        
        ON THE BASIS OF MINERAL COMPOSITION
        
        FELSIC IGNEOUS ROCKS
        
        MAFIC IGNEOUS ROCKS
        
        ULTRAMAFIC IGNEOUS ROCKS
        
        ON THE BASIS OF TEXTURE OF GRAINS
        
        PEGMATITIC IGNEOUS ROCKS
        
        PHANERITIC IGNEOUS ROCKS
        
        APHANITIC IGNEOUS ROCKS
        
        GLASSY IGNEOUS ROCKS
        
        PORPHYRITIC IGNEOUS ROCKS
        
        FRAGMENTAL IGNEOUS ROCKS
        
        GENERALLY
        
        COARSE GRAINED IGNEOUS ROCKS
        
        FINE -GRAINED IGNEOUS ROCKS
        
        MEDIUM GRAINED IGNEOUS ROCKS
        
        ON THE BASIS OF MODE OF OCCURENCE
        
        INTRUSIVE IGNEOUS ROCKS
        
        ON THE BASIS OF DEPTH OF PLACE OF COOLING
        
        HYPABYSSAL IGNEOUS ROCKS
        
        SHAPES
        
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        PLUTONIC IGNEOUS ROCKS
        
        GRANITES
        
        EXTRUSIVE IGNEOUS ROCKS
        
        ON THE BASIS O FNATURE OF APPEARANCE
        
        EXPLOSIVE TYPE
        
        BASALT
        
        QUIET TYPE
      - IGNEOUS ROCKS AND LANDFORMS
    - - INTRODUCTION
      - CHARACTERISTICS
      - CLASSIFICATION
        
        ON THE BASIS OF NATURE OF SEDIMENTS
        
        MECHANICALLY FORMED OR CLASTIC ROCKS
        
        SANDSTONES
        
        CONGLOMERATES
        
        CLAYROCK
        
        SHALE
        
        LOESS
        
        CHEMICALLY FORMED
        
        GYPSUM
        
        SALT ROCK
        
        ORGANICALLY FORMED
        
        LIMESTONES
        
        DOLOMITES
        
        COALS
        
        PEATS
        
        ON THE BASIS OF LIME & CARBON CONTENT
        
        CALCAREOUS ROCKS
        
        CARBONACEOUS ROCKS
        
        SILICEOUS ROCKS
        
        ON THE BASIS OF TRANSPORTING AGENT
        
        ARGILLACEOUS ROCKS
        
        ON THE BASIS OF TRANSPORTING AGENTS
        
        AGRILLACEOUS OR AQUEOUS ROCKS
        
        MARINE ROCKS
        
        LACUSTRINE ROCKS
        
        RIVERINE ROCKS
        
        AEOLIAN SEDIMENTARY ROCKS
        
        LOESS
        
        GLACIAL SEDIMENTARY ROCKS
        
        TILL
        
        MORAINES
    - - MEANING AND CHARACTERISTICS
      - METAMORPHISM
        
        METAMORPHISM
        
        2.CHEMICAL METAMORPHISM
        
        PHYSICAL METAMORPHISM
        
        AGENTS OF METAMORPHISM
        
        HEAT
        
        COMPRESSION
        
        SOLUTION
        
        TYPES OF METAMORPHISM
        
        ON THE BASIS OF NATURE OF AGENTS
        
        THERMAL METAMORPHISM (DUE TO HEAT)
        
        DYNAMIC METAMORPHISM ( DUE TO PRESSURE)
        
        HYDRO-METAMORPHISM ( DUE TO HYDRO-STATIC PRESSURE
        
        HYDROTHERMAL METAMORPHISM
        
        ON THE BASIS OF PLACE OR AREA
        
        CONTACT METAMORPHISM (LOCALIZED IN AREA)
        
        REGIONAL METAMORPHISM (INVOLVING LARGER AREA)
        
        COMPOSITE CLASSIFICATION
        
        CONTACT OR THERMAL METAMORPHISM
        
        DYNAMIC AND REGIONAL METAMORPHISM
        
        HYDRO-METAMORPHISM
        
        HYDRO-THERMAL METAMORPHISM
      - CLASSIFICATION OF METAMORPHIC ROCKS
        
        META-SEDIMENTARY OR PARA-METAMORPHIC ROCKS
        
        META-IGNEOUS OR ORTHO-METAMORPHIC ROCKS
        
        ON THE BASIS OF FOLIATION
        
        FOLIATED METAMORPHIC ROCKS
        
        SLATES
        
        GNEISSES
        
        SCHISTS
        
        NON FOLIATED METAMORPHIC ROCKS
        
        QUARTZITES
        
        MARBLES
        
        SERPENTINES