Indonesia ’s Mount Sinabung break open in a truly spectacular fashion this week – and , as footage and picture taking clearly draw , it ’s awe - inspiring and terrifying in equal measure . At present , rather unmistakably , there are n’t any reports of casualties , so hat off to the authorities on the ground for being on the ball .

Since 2013 , Sinabung has been erupting evenhandedly continuously , and as noted by volcanologist Erik Klemetti over atDiscover , it ’s primarily call for explosions that have trigger off pyroclastic flow rate .

Commencing on February 19 , a variety in the underlie magmatic system clearly activate a ( abbreviated ) period of more violent activity . This new eruption has produced a column of ash potentially 16.5 kilometers ( 10 nautical mile ) high , as well as some truly spectacular pyroclastic flow rate , so it ’s not surprising that they ’ve become the focal point of much of themedia’scoverageof the consequence .

accord to the AP , the eructation has been energetic enough toreshape the summit .

DrJanine Krippner , a volcanologist at Concord University , told IFLScience that although “ this bang is one of the large produced during this eruption period , but there have been many pyroclastic flow and frequent ash plumes since 2013 . ”

The current explosivity in this “ always changing system ” could be down to “ a change in the protrusion pace or some other magma property , ” but it ’s far too other to tell .

Getting caught up in these flow is thevery opposite of pleasant . Travelling at speeds outmatch that of a speeding gondola , these turbulent mixtures of superheated gas , debris , and blebs of lava compass temperatures as high as 1,000 ° C ( 1,830 ° F ) , and will bolt down anyone caught in them instantaneously through uttermost caloric shock or , sometimes , suffocation .

These pyroclastic flows haveformedin several ways . In crude condition , when the eruption editorial becomes cooler and ultimately denser than the surrounding air , or when it fails to keep an up impulse by head for the hills out of volatile thrust at its foundation , it begins to crock up , produce pyroclastic flows .

On other occasions , low explosions create an ephemeral plumage that quickly collapses and rolls down the wing of the vent . There ’s also a chance that the collapse of alava dome – a engine block mass of lava emerging from a volcano – has also been triggering pyroclastic flows .

Either mode , they ’re pestilent , and their emergence at Sinabung has bestow to a perpetual crisis , one thatconstantly displacestens of thousands of villagers and , occasionally , kills them .

At this percentage point , it ’s worth remember that Sinabung ’s hardly the only fiery fountain on the archipelago . Indonesia has around 130 active volcanoes , all with their own history and , of course , furious time to come .

There ’s a bunch left to understand about the land ’s volcanism . Considering that the densely populated body politic is home to 261 million people , the quicker our ken of them advances , the better .

According to the Smithsonian Institution’sGlobal Volcanism Program , significant eruptions prior to Sinabung ’s fireworks back in 2010 have yet to be confirmed . Its present bodily function is clean-cut to see – evenfrom blank space – but its past times remain decidedly enigmatic .

“ Understanding the chronicle and current activeness of a volcano takes time and resource , and like in most volcanically active countries , this has not been done at many volcanoes due to a lack of time and resource , ” Krippner added . “ Volcanic enquiry and monitoring has to be prioritized . ”