Eruption of the Hunga Tonga-Hunga Ha’apai volcano
On 15th january 2022
On 15th january 2022
On Saturday, late afternoon local time a huge explosive volcanic eruption occurred in the western Pacific Ocean in the Tonga Islands.
References : Szabolcs Harangi Blog
According to satellite images, the volcanic ash cloud from the explosion rose to almost 20 kilometers and reached the stratosphere. The sound of the eruption was heard over 1000 kilometers away and the atmospheric pressure wave was felt all over the Earth. Following the eruption, flood alarms were triggered in the Tonga region thanks to indications from sensors built over the last decade. The tide flowed to the small islands in the region and during the day reached the west coast of Japan and even North America.
But what really happened and where is the volcano?
The Tonga region is about 1,500 kilometers north of New Zealand. The islands are of volcanic origin, as the Pacific Rock grows westward under the Australian rock. The consequence of this is that due to the high pressure and high temperature, wet solutions are released from the oceanic rock plate penetrating deeper into the rock plate. This is where the melting point of the earth’s rock is reduced, causing intense melting and core formation. When the magma surfaces, it causes volcanic activity.
However, this occurs underwater in most cases. Under the water cover of the ocean, smaller or larger volcanoes are formed, the growth of which can lead some of them to rise above the water and this is also what happened in the Tonga region. Under the water of the ocean, a huge volcano has formed, at the northern edge of which volcanic eruptions have created two smaller islands: the Hunga Ha’apai Islands and the Hongga Tonga Islands.
In 2015, an explosive volcanic eruption connected the two continents and after that they became an island. On December 20, after several years of calm, there was another huge explosive eruption in which the volcanic ash cloud rose to 15 kilometers high. With this, the size of the island increased again. Another rest followed, but not for too long! On January 14, there was an even more powerful explosion followed by another one a day later. The 21st competes in size with both. with the eruptions of the century.
Tonga subduction (diving belt in rocky plate)
How can a small island produce such a volcanic eruption?
The underwater volcano of the ocean commands the authority, which was revealed by the research of the last decade. The eruption of the volcano rises to 1800 meters above the ocean surface and its base has a diameter of 20 kilometers. During their research seven years ago, by examining the rocks from previous eruptions of the volcano, volcanologists concluded that the volcano is capable of quite large eruptions.
For an eruption that occurs on average once every thousand years. Well, it has happened nowadays! The caldera volcano is a so-called caldera volcano, which forms in a way that a huge amount of magma leaves the deep core at once. And the top of this will collapse and the surface will sink like this. In the case of this volcano, a caldera with a diameter of 6 kilometers was formed during the previous eruptions. Now there is supposed to be another caldera forming eruption.
What caused this massive explosion and why was the trench attached to it?
When the magma suddenly reaches the water-covered surface of the ocean, at the meeting surface of magma and cold water at more than 1000 degrees Celsius, a layer of steam develops, which explodes in a few seconds and the magma and water can mix. The water that enters the magma turns into steam, which causes a significant increase in volume. All this happens in a fraction of a second and the sudden increase in volume shatters the magma explosively, which breaks up at speeds of several hundred meters per second. The magma material erupts as a dark rooster-shaped cloud of volcanic ash, it is accompanied by a tiny eruption cloud rich in volcanic gases and water vapor. However, this eruption cloud has now rolled over 20 kilometers in altitude! Given the strength of the eruption, it is assumed that this was caused by the repression of a considerable amount of magma, which has already begun the extraction of gas bubbles, the mixture of magma and water gave only the final push for an explosive eruption. According to early satellite data, the eruption cloud reaching the stratosphere was not rich in sulfur dioxide, so the volcanic eruption is unlikely to have a climatic impact.
The sudden surge of huge amounts of magma during two large explosive eruptions caused the submarine volcanic surface to erupt, allowing the volcanic caldera to deepen and widen. This vertical movement of material triggered waves that caused flash floods on nearby islands and remote coasts of the Pacific Ocean.
Will there be a thousand years of calm following these two or three explosions in December?
It’s hard to say now, but volcanic analysis over the next few days will help interpret it. This volcanic activity also confirms the enormous role of satellite remote sensing devices in volcanological monitoring and eruption forecasting.
Left and right images: maps of the Shane Cronin underwater volcano
VOLCANO ACTIVE FOUNDATION RESPONSABILITY
nº 2195 authorised by the Madrid's Minister of Justice
NIF G67314625
SF Abocados Francesc Macia 7 pl17
08029 Barcelona, Spain
We may request cookies to be set on your device. We use cookies to let us know when you visit our websites, how you interact with us, to enrich your user experience, and to customize your relationship with our website.
Click on the different category headings to find out more. You can also change some of your preferences. Note that blocking some types of cookies may impact your experience on our websites and the services we are able to offer.
These cookies are strictly necessary to provide you with services available through our website and to use some of its features.
Because these cookies are strictly necessary to deliver the website, refusing them will have impact how our site functions. You always can block or delete cookies by changing your browser settings and force blocking all cookies on this website. But this will always prompt you to accept/refuse cookies when revisiting our site.
We fully respect if you want to refuse cookies but to avoid asking you again and again kindly allow us to store a cookie for that. You are free to opt out any time or opt in for other cookies to get a better experience. If you refuse cookies we will remove all set cookies in our domain.
We provide you with a list of stored cookies on your computer in our domain so you can check what we stored. Due to security reasons we are not able to show or modify cookies from other domains. You can check these in your browser security settings.
These cookies collect information that is used either in aggregate form to help us understand how our website is being used or how effective our marketing campaigns are, or to help us customize our website and application for you in order to enhance your experience.
If you do not want that we track your visit to our site you can disable tracking in your browser here:
We also use different external services like Google Webfonts, Google Maps, and external Video providers. Since these providers may collect personal data like your IP address we allow you to block them here. Please be aware that this might heavily reduce the functionality and appearance of our site. Changes will take effect once you reload the page.
Google Webfont Settings:
Google Map Settings:
Google reCaptcha Settings:
Vimeo and Youtube video embeds:
The following cookies are also needed - You can choose if you want to allow them:
You can read about our cookies and privacy settings in detail on our Privacy Policy Page.
PRIVACY POLICY