MAUNA LOA VOLCANIC ERUPTIONS - GEOGRAPHY

News: Mauna Loa volcano in Hawaii erupts: What is the science behind volcanic eruptions?

 

What's in the news?

       Mauna Loa, the world’s largest active volcano, erupted after 38 years on Sunday (November 27), spewing ash and debris, and covering the night sky of Hawaii’s Big Island in an incandescent red hue.

 

Volcano:

       It is a rupture in the crust of a planetary-mass object (like Earth), that causes hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

       On Earth, volcanoes are generally found where tectonic plates (like Eurasian, Pacific, Somali, etc) diverge or converge. Examples- volcanoes occurring in mid-oceanic ridge and Ring of Fire.

       Eruption of volcanoes can be hazardous for humans and other lives living in its vicinity and volcanic ash may be a threat to aircrafts. Volcanoes can also cause

       Large volcanic eruptions inject water vapor (H2O), Carbon Dioxide (CO2), Sulphur Dioxide (SO2), ash, etc into the stratosphere to heights of 16-32 km.

 

Magma:

       Magma is lighter than solid rock and hence it rises, collecting in magma chambers.

       Chambers which have the potential to cause volcanic eruptions are found at a relatively shallow depth, between six to ten km under the surface.

       As magma builds up in these chambers, it forces its way up through cracks and fissures in Earth’s crust. This is what we call a volcanic eruption.

       The magma that surfaces on the Earth’s crust is referred to as lava.

 

Types of volcanoes based on frequency of eruption:

1. Active Volcano:

       Active volcanoes are volcanoes that are either erupting or on the verge of eruption.

       There are around 500 active volcanoes on Earth, excluding those submerged beneath the oceans.

       Every year, approximately 50 to 70 active volcanoes erupt, most of them being around the pacific “ring of fire”.

       Mount Etna (Italy), Hawaiian Islands (Pacific Ocean), Mauna Loa (Pacific Ocean), Mount Vesuvius (Italy), and Barren Island (India) are some examples of Active Volcanoes around the world.

2. Dormant Volcano:

       A dormant volcano is one that is not erupting at the present but has erupted in the past and is expected to erupt again.

       The distinction between active and dormant volcanoes can be hazy.

       Some volcanoes can last thousands of years without erupting, thus they are theoretically predicted to erupt in the future, but it could take many lives.

       Another of the Big Island's five volcanoes, Mauna Kea, last erupted 3,500 years ago, but it is predicted to erupt again, but no date has been set.

       People living in the neighborhood of dormant volcanoes are frequently complacent and unprepared when an eruption occurs.

       This was the case in 1980 with Mt. St. Helens.

3. Extinct Volcano:

       Extinct volcanoes are considered to be dormant and unlikely to erupt again.

       Example: Kohala, the Big Island of Hawaii's oldest volcano, hasn't erupted in 60,000 years and isn't expected to erupt again.

       However, because many Hawaiian volcanoes are in the process of rejuvenation, this classification isn't completely accurate.

       Aconcagua of the Andes is a typical example of an extinct volcano.

 

Some famous volcanoes in the world:

  1. Krakatoa - Indonesia
  2. Mount Vesuvius - Italy
  3. Mount Fuji - Japan
  4. Eyjafjallajökull - Iceland
  5. Kīlauea - Hawaii
  6. Mount St Helens - USA