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It is 3.322 metres
                       Etna covers an
 (10.922 ft) high,
                     area of 1,190 kmÂČ
 though the height
                     (460 sq mi) with a
varies with summit
                            basal
     eruptions.
                      circumference of
                           140 km.
The Mediterranean area is a convergent boundary where the Eurasian
 and African plates move toward one another and collide. These two
 plates form a subduction zone as the African plate dives under the
 Eurasian plate. As a result of pressure, friction, and plate material
    melting in the mantle, earthquakes and volcanoes are common.
- in the north the Aeolian
Islands’ volcanism
provocated by the melting
of continental crust of the
African plate.
- in the south Etna’s
volcanism due to the
magma that comes out
from the mantle (30 km
deepness) as the
subduction of the African
plate causes the crack of
the continental crust.
The current structure of Mount Etna is the effect of a long and complex
  eruptive history. The growth of the mountain was occasionally interrupted
 by major eruptions, leading to the collapse of the summit to form calderas.
                  We can divide Etna’s evolution in 4 phases:



First phase:
”pre-Etnean”

Second phase:
“Ancient Etna”

Third phase:
“Trifoglietto II”

Fourth phase:
“Mongibello”
Volcanic activity in the Etnean area began around 0.5 million years ago. Its
     products were mainly submarine lavas and volcaniclastics of tholeiitic
composition. The famous outcrops of Acicastello and nearby locations contain
                   pillow lavasproduced by this early activity.
This phase of volcanism took place in a vast marine gulf, extending over part
  of the area occupied by the present Etna. The gulf was filled by sediments
intermixed with a regional tectonic uplift. Then the suaerial eruptions began .
The various eruptions created a stratovolcano. Today Etna is by far
the largest of the three active volcanoes in Italy and one of the most
active volcanoes in the world. It is still in an almost constant state of
activity.
Etna’s vegetation is one of the most various in
   Sicily.
The volcanic eruptions makes fertile the territory
   and changes very often the landscape.
Under 2000 mt there are vineyards,brooms and
   hazelnut or oak woods.
Over about 2000 mt there are Beech and birch
   woods.
In the higher altitude of the mountain there isn’t
   any vegetation that can survives.
The Etna birch (Betula aetnensis) is
 very similar to the Northern Europe
             one, but during
   the millennia has evolved so that
    many naturalists consider it an
       endemic variety of Etna.
  A typical feature of the birch is the
      color pinkish-white of the
   cortex, that tends to epidermal
desquamation in horizontal bands. The
leaf has a bright green color, small in
       size and serrated edges.
      The branches are very thin
              and flexible.
     Also has strong detoxifying
        properties and is used
against somechronic rheumatic diseas
       es and against hair loss.
Logging and the pratice of hunting wild caused
the extinction of wolfs,wild boars,deer and roe
deer.Despite this,on the volcano,still live
porcupines,foxes, wild
cats, martens, rabbits, hares, and among the
smaller
animals,weasels, hedgehogs, dormice, dormouse.
Etna’s wildlife also includes snakes, as the viper
or the green lizard, and a big variety of
birds, for example the barn owl and the golden
eagle.
Since ancient times the rich volcanic soils of Mount
   Etna has allowed people to live on agriculture
   and livestock. Surprising and
   varied agricultural landscapes are set among
   forests and lava flows, forming a mosaic environment of
   rare beauty. The presence of man on the volcano
   for thousands of years has left a deep
   imprint: monumental works of terracing,
   warehouses,wineries, dot the slopes of the
   "Mountain". The most common kinds of agriculture in
   Etna’s territory are vineyards and orchards of olives,
   hazelnuts, pistacchio and citrus, expecially oranges.
2001 eruption
2004 eruption
2006 eruption
2011 eruption
Made by:
 Dario Borrometi
Alessandro Nicotra
   Luca Nicotra

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The volcano Etna

  • 1.
  • 2. It is 3.322 metres Etna covers an (10.922 ft) high, area of 1,190 kmÂČ though the height (460 sq mi) with a varies with summit basal eruptions. circumference of 140 km.
  • 3. The Mediterranean area is a convergent boundary where the Eurasian and African plates move toward one another and collide. These two plates form a subduction zone as the African plate dives under the Eurasian plate. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common.
  • 4. - in the north the Aeolian Islands’ volcanism provocated by the melting of continental crust of the African plate. - in the south Etna’s volcanism due to the magma that comes out from the mantle (30 km deepness) as the subduction of the African plate causes the crack of the continental crust.
  • 5. The current structure of Mount Etna is the effect of a long and complex eruptive history. The growth of the mountain was occasionally interrupted by major eruptions, leading to the collapse of the summit to form calderas. We can divide Etna’s evolution in 4 phases: First phase: ”pre-Etnean” Second phase: “Ancient Etna” Third phase: “Trifoglietto II” Fourth phase: “Mongibello”
  • 6. Volcanic activity in the Etnean area began around 0.5 million years ago. Its products were mainly submarine lavas and volcaniclastics of tholeiitic composition. The famous outcrops of Acicastello and nearby locations contain pillow lavasproduced by this early activity.
  • 7. This phase of volcanism took place in a vast marine gulf, extending over part of the area occupied by the present Etna. The gulf was filled by sediments intermixed with a regional tectonic uplift. Then the suaerial eruptions began .
  • 8. The various eruptions created a stratovolcano. Today Etna is by far the largest of the three active volcanoes in Italy and one of the most active volcanoes in the world. It is still in an almost constant state of activity.
  • 9. Etna’s vegetation is one of the most various in Sicily. The volcanic eruptions makes fertile the territory and changes very often the landscape. Under 2000 mt there are vineyards,brooms and hazelnut or oak woods. Over about 2000 mt there are Beech and birch woods. In the higher altitude of the mountain there isn’t any vegetation that can survives.
  • 10. The Etna birch (Betula aetnensis) is very similar to the Northern Europe one, but during the millennia has evolved so that many naturalists consider it an endemic variety of Etna. A typical feature of the birch is the color pinkish-white of the cortex, that tends to epidermal desquamation in horizontal bands. The leaf has a bright green color, small in size and serrated edges. The branches are very thin and flexible. Also has strong detoxifying properties and is used against somechronic rheumatic diseas es and against hair loss.
  • 11. Logging and the pratice of hunting wild caused the extinction of wolfs,wild boars,deer and roe deer.Despite this,on the volcano,still live porcupines,foxes, wild cats, martens, rabbits, hares, and among the smaller animals,weasels, hedgehogs, dormice, dormouse. Etna’s wildlife also includes snakes, as the viper or the green lizard, and a big variety of birds, for example the barn owl and the golden eagle.
  • 12. Since ancient times the rich volcanic soils of Mount Etna has allowed people to live on agriculture and livestock. Surprising and varied agricultural landscapes are set among forests and lava flows, forming a mosaic environment of rare beauty. The presence of man on the volcano for thousands of years has left a deep imprint: monumental works of terracing, warehouses,wineries, dot the slopes of the "Mountain". The most common kinds of agriculture in Etna’s territory are vineyards and orchards of olives, hazelnuts, pistacchio and citrus, expecially oranges.
  • 13.
  • 15.
  • 16.
  • 17.
  • 19.
  • 20.
  • 21.
  • 22.
  • 24.
  • 25.
  • 26.
  • 27.
  • 28.
  • 29.
  • 30.
  • 31.
  • 33.
  • 34.
  • 35.
  • 36.
  • 37.
  • 38. Made by: Dario Borrometi Alessandro Nicotra Luca Nicotra