Santorini Volcano | UPSC

Santorini Volcano | UPSC | Why In The News ?

Greece’s Santorini volcano erupts more often when sea level drops- New Findings.
Lower sea levels over the last 360,000 years are linked with more eruptions.

Santorini Volcano | UPSC

Key Findings :

  • When the sea level dropped at least 40 meters below the present-day level, the crust above the magma chamber splintered.
  • That gives an opportunity for the magma that’s stored under the volcano to move up through these fractures and make its way to the surface.

About Santorini Volcano

  • Santorini is an island in the southern Aegean Sea, about 200 km southeast from the Greek mainland.
  • It is the largest island of a small, circular archipelago, which bears the same name and is the remnant of a volcanic caldera.
  • It is the most active volcanic centre in the South Aegean Volcanic Arc.
  • It forms the southernmost member of the Cyclades group of islands.
  • The island was the site of one of the largest volcanic eruptions in recorded history: the Minoan eruption (sometimes called the Thera eruption), which occurred about 3,600 years ago at the height of the Minoan civilization and led to its collapse.

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About Aegean Sea :

  • The Aegean Sea is an elongated embayment of the Mediterranean Sea between Europe and Asia.
  • It is located between the Balkans and Anatolia, and covers an area of some 215,000 square kilometres.
  • The Aegean is connected through the straits of the Dardanelles, the Sea of Marmara, and the Bosporus to the Black Sea, while the island of Crete can be taken as marking its boundary on the south.
  • The Aegean is subdivided into the Myrtoan Sea and the Thracian Sea.
  • The Aegean Sea experiences a Mediterranean climate.
  • The weather in the Aegean basin is mainly influenced by the Etesian wind.

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What are various types of volcanoes?

Major types of volcanoes: Volcanoes are classified on the basis of nature of eruption and the form developed at the surface.

Shield Volcanoes
  • The Shield volcanoes are the largest of all the volcanoes on the earth, which are not steep.
  • These volcanoes are mostly made up of basalt.
  • They become explosive if in some way water gets into the vent, otherwise, they are characterized by low-explosivity.
  • Eg: Hawaiian shield volcanoes
Composite Volcanoes
  • Composite Volcanoes are characterized by outbreaks of cooler and more viscous lavas than basalt.
  • They are constructed from numerous explosive eruptions.
  • The major composite volcano chains are Pacific Rim which known as the “Rim of Fire”.
  • Calderas are known as the most explosive volcanoes of Earth.
  • They are generally explosive in nature.
  • When they erupt, they incline to collapse on themselves rather than constructing any structure.
  • The collapsed depressions are known as calderas.
Flood Basalt Provinces
  • Flood Basalt Province volcanoes discharge highly fluid lava that flows for long distances.
  • Many parts of the world are covered by thick basalt lava flows.
Mid-Ocean Ridge Volcanoes
  • These volcanoes are found in the oceanic areas.
  • There exists a system of mid-ocean ridges stretching for over 70000 km all through the ocean basins.
  • The central region of this ridge gets frequent eruptions.





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