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KERALA UNIVERSITY 
COLLEGE OF TEACHER 
EDUCATION 
NEDUMANGAD
PRESENTED 
BY 
NAME PRIYANKA R 
OPTION SOCIALSCIENCE 
REG. No. 13983023
VOLCANOES ARE CAUSED WHEN MOLTEN 
ROCK (MAGMA)FLOWS OUT INTO THE 
EARTH’S SURFACE THROUGH FISSURES 
THAT ARE CAUSED DUE TO THE 
MOVEMENT OF PLATES. THE FISSURES , 
THROUGH WHICH MAGMA COMES OUT 
FROM THE AESTHENOSPHERE ON TO THE 
CRUST OF THE EARTH IS KNOWN AS THE 
VENT THE ROCKS AND OTHER MATERIAL 
WHICH COME FROM THE SURFACE OF 
THE EARTH ACCUMULATES TO DEVELOP 
VOLCANIC MOUNTAINS.
DIFFERENT TYPES OF 
VOLCANOES 
ACTIVE 
EXTINCT 
DORMANT
ACIVE VOLCANOS 
 THOSE THAT FREQUENTLY ERUPT 
EXAMPLE : MOUNT ETNA IN ITALY
EXTINCT VOLCANOES 
 ACTIVE AT A TIME . BUT IT WILL NOT ERUPT 
AGAIN 
EXAMPLE : KILIMANJARO IN AFRICA
DORMANT VOLCANOES 
 THOSE THAT HAVE ERUPTED EARLIER AND NOT 
ACTIVE IN THE RECENT PAST . BUT CAN BECOME 
ACTIVE 
EXAMPLE : VESUVIES IN ITALY
VOLCANOES

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VOLCANOES

  • 1.
  • 2. KERALA UNIVERSITY COLLEGE OF TEACHER EDUCATION NEDUMANGAD
  • 3. PRESENTED BY NAME PRIYANKA R OPTION SOCIALSCIENCE REG. No. 13983023
  • 4. VOLCANOES ARE CAUSED WHEN MOLTEN ROCK (MAGMA)FLOWS OUT INTO THE EARTH’S SURFACE THROUGH FISSURES THAT ARE CAUSED DUE TO THE MOVEMENT OF PLATES. THE FISSURES , THROUGH WHICH MAGMA COMES OUT FROM THE AESTHENOSPHERE ON TO THE CRUST OF THE EARTH IS KNOWN AS THE VENT THE ROCKS AND OTHER MATERIAL WHICH COME FROM THE SURFACE OF THE EARTH ACCUMULATES TO DEVELOP VOLCANIC MOUNTAINS.
  • 5.
  • 6. DIFFERENT TYPES OF VOLCANOES ACTIVE EXTINCT DORMANT
  • 7. ACIVE VOLCANOS  THOSE THAT FREQUENTLY ERUPT EXAMPLE : MOUNT ETNA IN ITALY
  • 8. EXTINCT VOLCANOES  ACTIVE AT A TIME . BUT IT WILL NOT ERUPT AGAIN EXAMPLE : KILIMANJARO IN AFRICA
  • 9. DORMANT VOLCANOES  THOSE THAT HAVE ERUPTED EARLIER AND NOT ACTIVE IN THE RECENT PAST . BUT CAN BECOME ACTIVE EXAMPLE : VESUVIES IN ITALY