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11 Geography




Different types of Volcanic Landforms
There are many different types of volcanic landforms.
Often these are caused by the different types of
eruptions that we looked at previously.
So first… what were the main types of eruptions?

Ex_________________   Magma is ___________ because it contains a lot of ___

                      Eg…r________________________________




Ef_________________   Magma is ___________ because it doesn’t contain so

                      much _________ eg b__________________________

                      UNLESS the magma meets ______________________

                      Then it may cause a __________-________________

Ex________________    ← eruption
Two main categories of landforms
• Cone = a
  hill, mound, mountain, dome, peak, cone etc – a
  new or altered landform that sticks up out of the
  ground




• Crater = a basin, hollow, depression in the ground
  that will probably get filled up with freshwater
  (eg a lake)

or saltwater
3 Main types of volcanic cones
• Scoria Cone (or cinder cone)
• Shield Volcano
• Stratovolcano (or composite cone)
Scoria Cone
• Otherwise known as a cinder cone
• Sides are quite straight with steep slopes
• Large summit crater



• The lava and tephra are usually basalt
  (or sometimes andesitic) which means it
  is quite runny
Scoria Cone continued
• The eruption type is usually Strombolian which
  means it has fire fountains
Strombolian Eruption
Scoria Cone continued
• A good example around Auckland is Maungawhau
  (Mt Eden) – steep, straight sides, crater in centre
Shield Volcano
• Very gentle slopes; convex
  upward


• Basalt lava flows - the lava
  flows easily away from the vent
  in large sheets, or follows
  existing stream valleys
• Sometimes caves or tubes form
  in the lava, other times large
  columnar basalt formations
Shield Volcano continued
• The eruption type is known as hawaiian,
• producing lava flows known as aa or pahoehoe
Shield Volcano continued


• Rangitoto is a good example of this type of volcano
• Gentle slopes




                               • “Aa” lava flow
                                 on Rangitoto
Stratovolcano or Composite Cone
• Gentle lower slopes, but steep upper slopes;
  concave upward;
• small summit crater
• Highly variable lava types; alternating basaltic
  to rhyolitic lava and tephra with an overall
  andesitic composition.
• This means that the lava often has a lot of
  trapped gas, so it is very sticky
• The cone is built up over a long period of time
  by many eruptions of various types
Stratovolcano continued
• This eruption type is known
  as Plinian or Vesuvian
• These eruptions can be
  huge, long-lasting and
  extremely dangerous
Stratovolcano continued
• When these volcanoes erupt they emit volcanic
  products that also have major impacts on the
  land and natural environment:
• Pyroclastic flows
• Lahars
• Ash showers

• In New Zealand volcanic activity has built up a
  huge volcanic plateau (area of upraised land) in
  the Central North Island.
Pyroclastic flows
• huge clouds of ash, rock and hot gas that sweep downhill at
  incredible speed, flattening anything in their way
Lahars
• A flow of liquid mud down a mountain or valley
• NZ’s most famous is the Whangehu River
  lahar, Christmas Eve 1953, causing the Tangiwai
  Disaster
Ash showers
• Thick layers of gritty, acidic volcanic ash fall in a
  thick blanket, choking the landscape
Craters
• A caldera forms when a huge
  stratovolcano collapses in on
  itself after a major eruption
  sequence, creating a massive
  crater
• Usually this fills with water to
  form a lake
• Rotorua and Taupo both
  formed in this way
Lake Taupo – a caldera
Maar
• A crater caused by a phreato-magmatic eruption
• This is when hot magma encounters groundwater
  and explodes out of the ground
• Auckland has several examples, such as Lake
  Pupuke, Tank Farm, Onepoto Basin, Panmure Basin
  and Orakei Basin
• A maar is often surrounded by a tuff ring = a ring
  around the edge of the crater made of layers of
  ash, soil and scoria
• Maars usually fill up with freshwater or seawater
3D map of Auckland volcanoes
A really useful website about volcanic eruptions

 • http://www.squidoo.com/volcano-glossary

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Types of volcanoes

  • 1. 11 Geography Different types of Volcanic Landforms
  • 2. There are many different types of volcanic landforms. Often these are caused by the different types of eruptions that we looked at previously. So first… what were the main types of eruptions? Ex_________________ Magma is ___________ because it contains a lot of ___ Eg…r________________________________ Ef_________________ Magma is ___________ because it doesn’t contain so much _________ eg b__________________________ UNLESS the magma meets ______________________ Then it may cause a __________-________________ Ex________________ ← eruption
  • 3. Two main categories of landforms • Cone = a hill, mound, mountain, dome, peak, cone etc – a new or altered landform that sticks up out of the ground • Crater = a basin, hollow, depression in the ground that will probably get filled up with freshwater (eg a lake) or saltwater
  • 4. 3 Main types of volcanic cones • Scoria Cone (or cinder cone) • Shield Volcano • Stratovolcano (or composite cone)
  • 5. Scoria Cone • Otherwise known as a cinder cone • Sides are quite straight with steep slopes • Large summit crater • The lava and tephra are usually basalt (or sometimes andesitic) which means it is quite runny
  • 6. Scoria Cone continued • The eruption type is usually Strombolian which means it has fire fountains
  • 8. Scoria Cone continued • A good example around Auckland is Maungawhau (Mt Eden) – steep, straight sides, crater in centre
  • 9. Shield Volcano • Very gentle slopes; convex upward • Basalt lava flows - the lava flows easily away from the vent in large sheets, or follows existing stream valleys • Sometimes caves or tubes form in the lava, other times large columnar basalt formations
  • 10. Shield Volcano continued • The eruption type is known as hawaiian, • producing lava flows known as aa or pahoehoe
  • 11.
  • 12. Shield Volcano continued • Rangitoto is a good example of this type of volcano • Gentle slopes • “Aa” lava flow on Rangitoto
  • 13. Stratovolcano or Composite Cone • Gentle lower slopes, but steep upper slopes; concave upward; • small summit crater • Highly variable lava types; alternating basaltic to rhyolitic lava and tephra with an overall andesitic composition. • This means that the lava often has a lot of trapped gas, so it is very sticky • The cone is built up over a long period of time by many eruptions of various types
  • 14. Stratovolcano continued • This eruption type is known as Plinian or Vesuvian • These eruptions can be huge, long-lasting and extremely dangerous
  • 15.
  • 16. Stratovolcano continued • When these volcanoes erupt they emit volcanic products that also have major impacts on the land and natural environment: • Pyroclastic flows • Lahars • Ash showers • In New Zealand volcanic activity has built up a huge volcanic plateau (area of upraised land) in the Central North Island.
  • 17. Pyroclastic flows • huge clouds of ash, rock and hot gas that sweep downhill at incredible speed, flattening anything in their way
  • 18. Lahars • A flow of liquid mud down a mountain or valley • NZ’s most famous is the Whangehu River lahar, Christmas Eve 1953, causing the Tangiwai Disaster
  • 19. Ash showers • Thick layers of gritty, acidic volcanic ash fall in a thick blanket, choking the landscape
  • 20. Craters • A caldera forms when a huge stratovolcano collapses in on itself after a major eruption sequence, creating a massive crater • Usually this fills with water to form a lake • Rotorua and Taupo both formed in this way
  • 21. Lake Taupo – a caldera
  • 22. Maar • A crater caused by a phreato-magmatic eruption • This is when hot magma encounters groundwater and explodes out of the ground • Auckland has several examples, such as Lake Pupuke, Tank Farm, Onepoto Basin, Panmure Basin and Orakei Basin • A maar is often surrounded by a tuff ring = a ring around the edge of the crater made of layers of ash, soil and scoria • Maars usually fill up with freshwater or seawater
  • 23.
  • 24. 3D map of Auckland volcanoes
  • 25. A really useful website about volcanic eruptions • http://www.squidoo.com/volcano-glossary