{"id":11463,"date":"2023-11-11T02:46:23","date_gmt":"2023-11-11T02:46:23","guid":{"rendered":"https:\/\/shareperformanceinsight.com\/index.php\/2023\/11\/11\/be-prepared-for-all-outcomes-inside-the-saga-of-a-supervolcano-thats-waking-up\/"},"modified":"2023-11-11T02:46:23","modified_gmt":"2023-11-11T02:46:23","slug":"be-prepared-for-all-outcomes-inside-the-saga-of-a-supervolcano-thats-waking-up","status":"publish","type":"post","link":"https:\/\/shareperformanceinsight.com\/index.php\/2023\/11\/11\/be-prepared-for-all-outcomes-inside-the-saga-of-a-supervolcano-thats-waking-up\/","title":{"rendered":"\u2018Be prepared for all outcomes\u2019: Inside the saga of a supervolcano that\u2019s waking up"},"content":{"rendered":"<p class=\"paragraph inline-placeholder\">      Forget Italy\u2019s most famous active volcano, Mt. Vesuvius, which destroyed Pompei in 79 AD.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The most dangerous volcanic threat in Italy right now is one<strong> <\/strong>you\u2019ve probably never heard of: Campi Flegrei, or the Phlegraean Fields.  <\/p>\n<p class=\"paragraph inline-placeholder\">      This unassuming plain, which stretches 200 kilometers (125 miles)\u00a0under\u00a0the bay of Naples and the islands of Capri and Ischia to the outskirts of the city of Naples, is a giant caldera, or depression, left by a supervolcano some 2 million years ago.  <\/p>\n<p class=\"paragraph inline-placeholder\">      It is now the site of multiple volcanoes that have been active for 39,000 years, many of which lie underwater. It\u2019s also populated with villas, small villages and shopping malls and home to 800,000 people\u00a0and a hospital under construction. More than 500,000 of the locals live in what Italy\u2019s civil protection agency has deemed a \u201cred zone,\u201d an area encompassing 18 towns that\u2019s at highest risk in the event of an eruption. An additional 3 million residents\u00a0of Naples live immediately outside the eastern edge of the caldera, according to the civil protection agency.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The last major eruption of Campi Flegrei was in 1538, and it created a new mountain in the bay. Seismic activity in the area has been intensifying since December of 2022, according to Italy\u2019s National Institute of Geophysics and Volcanology (INGV), and experts fear that the volcano could be reawakening after generations at rest.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The densely populated region, which is less than 50 kilometers (31 miles) from Vesuvius, is prone to a seismic phenomenon known as bradyseism, defined by cycles of uplift and gradual lowering of the ground. The last time the region saw such activity was 1984, when the ground rose 3.5 meters (11.5 feet) before it began a slow descent\u00a0accompanied by seismic activity similar to what is happening in the area now.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Currently in a state of positive bradyseism, when the ground moves upward, the entire volcanic zone is also experiencing a surge in earthquakes that has rattled nerves and sent residents seeking safety out into the streets. In September, the strongest earthquake in 40 years struck the region, and that 4.2 magnitude quake was followed by one of a similar strength just days later.  <\/p>\n<p class=\"paragraph inline-placeholder\">      So far in 2023 Campi Flegrei has recorded more than 3,450 earthquakes, 1,118 of which occurred in August alone. This is more than triple the previous year\u2019s total, according to INGV\u2019s data.<strong> <\/strong>More than 500 earthquakes occurred in October, the strongest of which hit 4.0 magnitude, followed by a dozen aftershocks.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Until the beginning of May, the quakes were almost all under 3.0 magnitude, according to INGV.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Many experts think the local population should be better prepared to cope with the seismic activity and the possibility of an eruption. On October 5, the country\u2019s civil protection agency laid out an updated evacuation plan, which calls for the movement of half a million people over a 72-hour period of time on roads many locals fear won\u2019t accommodate such intense traffic.<strong> <\/strong>The last time a such a plan had been studied was in 2019, and the findings showed the evacuation plan was lacking.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Carlo Doglioni, head of the INGV, gave testimony on the potential outcomes of the seismic activity before the Italian government\u2019s Environmental Commission\u2019s lower chamber on September 28.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThere are two possible scenarios relating to the evolution of the situation in the Campi Flegrei: the best is that the ongoing bradyseism crisis ends as happened in 1983 to 84; the worst is an eruption similar to that of 1538,\u201d he said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cIt is an evolution that we do not know and that we are monitoring,\u201d Doglioni said.  <\/p>\n<h3 class=\"subheader\">    What\u2019s behind the increase in activity<\/h3>\n<p class=\"paragraph inline-placeholder\">      Dr. Giuseppe De Natale, a research director at the INGV in Naples, said the current cycle of uplift is associated with pressure below the surface of the caldera. \u201cWe don\u2019t know exactly the depth of the increase of pressure, it could be between zero and 3.5 kilometers,\u201d he said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      There are two hypotheses as to what could be causing the current increase in seismic activity at Campi Flegrei, according to De Natale.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The first \u2014 and potentially most dangerous \u2014 possibility is that it could be an \u201cintrusion of magma coming from the magma chamber located about 8 kilometers deep,\u201d De Natale said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      The second, which he said is more likely, is that there is a large \u201cdegassing\u201d of gases created by the magma coming from the deep magma chamber. The degassing at the same depth as the magma chamber is what he believes has caused the ground to rumble.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThe problem is the rocks,\u201d De Natale said. \u201cThe shallow rocks cannot hold high levels of pressure, so if the pressure increases too much, there could happen complete fracturing of the rocks, which is generally the cause of the eruption of a volcano.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      Dr. Benedetto De Vivo, a retired professor of geochemistry at the University of Naples and an expert on bradyseism, agrees that the crater is degassing, and doesn\u2019t think that the rising land is due to magma alone. These gases, he believes, are caused by the magma below the caldera receding, not rising. But he said it is impossible to know exactly what is happening.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cWe can use statistics to create models, but we cannot predict the natural process because we do not know all of the variables in play,\u201d De Vivo said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      In spite of objections\u00a0by the local residents that drilling could trigger more seismic activity, De Natale won approval in 2009 to lead a team of volcano experts from 18 countries in 2012 on a mission to drill a pilot hole 501 meters (1,644 feet) deep into the caldera in an attempt to see exactly what was going on. However, Rosa Russo Iervolino, who was mayor of Naples at the time, halted the drilling project before it began, citing concerns for the population. In 2012, after she left office, the project was briefly reinstated by the new mayor, Luigi di Magistris, but by then funding had dried up and only the borehole was drilled.  <\/p>\n<h3 class=\"subheader\">    Planning around a natural enigma<\/h3>\n<p class=\"paragraph inline-placeholder\">      Supervolcanoes are among the most perplexing and least understood natural threats in the world.  <\/p>\n<p class=\"paragraph inline-placeholder\">      What distinguishes a supervolcano from an ordinary volcano is the amount of volcanic material it has ejected during past eruptions \u2014 a reflection of the volcano\u2019s explosive power.<strong><\/strong><strong><\/strong>  <\/p>\n<p class=\"paragraph inline-placeholder\">      A supervolcano is one that has ejected more than 240 cubic miles of material and reached a level 8 \u2014 the highest threat \u2014 on the Volcano Explosivity Index\u00a0or VEI, according to the US Geological Survey. The VEI index measures how much debris is ejected, at what height, and for how long the eruption lasts. Yellowstone, which erupted 2.1 million years ago, was one of the largest ever known eruptions. The most recent eruptions of other notable supervolcanoes, including Long Valley in California, Toba in Indonesia, and Campi Flegrei, were all around the same size.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Scientists have a 2,000-year record of activity on Campi Flegrei. Pillars at the Roman Temple of Serapis in the city of Pozzuoli in the middle of the caldera, which were excavated in the 18th century, show evidence of holes made by molluscs, revealing the pillars were once underwater. The base of the temple is connected to the sea by a series of underground tunnels, and the rising and falling of the ground caused by bradyseism has resulted in the water flooding and then draining out of the structure, making it possible to observe the seismic phenomenon over time.  <\/p>\n<p class=\"paragraph inline-placeholder\">      In 2016, the regional government designated the Campi Flegrei area \u00a0\u201cyellow\u201d \u00a0under its warning system, the second of four levels that move from green to red to indicate the danger to the population from the movement of the ground.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Italy\u2019s civil protection agency said in October it would be moving some parts of the area to next level, orange, given the intensity of the recent activity. The INGV now has to sign off on the level change, which it is expected to do since it originally petitioned the civil protection agency for the move. Upping the level to orange will allow civil protection agencies to evacuate the area most vulnerable to the effects of bradyseism and the continuing earthquakes more easily and keep the most vulnerable populations safe, officials say.  <\/p>\n<p class=\"paragraph inline-placeholder\">      During a meeting with the civil protection agency and government on November 7, the INGV also determined that 15,000 buildings, including 125 schools and other academic structures, are in the high-risk area. A directive will be released November 27 outlining a new protocol for evacuations, drills and potentially moving some institutions from the area temporarily until the current cycle of bradyseism subsides.  <\/p>\n<h3 class=\"subheader\">    The likelihood of an eruption<\/h3>\n<p class=\"paragraph inline-placeholder\">      Parts of the volcano could be weakening due to the effects of bradyseism, according to a paper published in the scientific journal Communications Earth &amp; Environment in June. But the situation remains unpredictable, experts say.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cWhat we expect depends on whether the ground keeps rising. If it carries on moving at its current rate, we expect the number of small earthquakes per day will fluctuate over weeks from just a handful to the swarms of a few hundred events, as felt in mid-August and late September,\u201d said study coauthor\u00a0Christopher Kilburn, a professor of volcanology at University College London.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cAny larger magnitude earthquakes are most likely to occur during the swarms. These are the classic signals of crust being stretched to breaking point.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      However, this does not mean an eruption is inevitable.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cIt\u2019s the same for all volcanoes that have been quiet for generations,\u201d said study coauthor Stefano Carlino, a volcanologist from the Vesuvius Observatory, in news release accompanying the paper.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cCampi Flegrei may settle into a new routine of gently rising and subsiding, as seen at similar volcanoes around the world, or simply return to rest,\u201d Carlino said. \u201cWe can\u2019t yet say for sure what will happen. The important point is to be prepared for all outcomes.\u201d  <\/p>\n<p class=\"paragraph inline-placeholder\">      A first step toward preparing<strong> <\/strong>should be avoiding population increase by prohibiting more construction\u00a0in Campi Flegrei, which is one of the most developed areas in Italy, said Dr. Benedetto De Vivo, a retired professor of geochemistry at the University of Naples.  <\/p>\n<p class=\"paragraph inline-placeholder\">      He also said there should be a better evacuation route with wider roads so that people who live in the densely populated area could evacuate within 24 hours. \u201cWe cannot construct even one more home in the area,\u201d he said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Italy\u2019s volcano experts are wary about making specific predictions about volcanic eruptions for fear of being held accountable if they are wrong, according to the INGV.  <\/p>\n<p class=\"paragraph inline-placeholder\">      Seven scientists were convicted of manslaughter for telling residents of L\u2019Aquila in central Italy not to worry about an increase in seismic activity in 2009. An earthquake that struck a few days after one scientist had appeared to say it was OK to relax and have a glass of wine\u00a0killed more than 300 people. The scientists were eventually acquitted on appeal, but the experience left the scientific community in Italy shaken.  <\/p>\n<p class=\"paragraph inline-placeholder\">      One of the largest kinds of volcanic eruptions, called an \u201cignimbritic eruption\u201d \u2014 such as the one that occurred in the Campi Flegrei area around 39,000 years ago \u2014 is not what Natale believes could happen any time soon.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cIt is difficult to study these potential huge eruptions, very rare but very catastrophic, and this is one of the most important but also the most challenging areas of vulcanology,\u201d Natale said.  <\/p>\n<p class=\"paragraph inline-placeholder\">      He said the next Campi Flegrei eruption \u2014 if one were to occur in the near future \u2014 would most likely be more in line with the last significant activity in 1538, which created the 133-meter-tall (463-foot-tall)\u00a0Monte Nuovo cone visible in the sea. However, due to population growth, the impacts of a similar event could look very different in present day.  <\/p>\n<p class=\"paragraph inline-placeholder\">      \u201cThat (1538) was a very small eruption, that, if it would happen today, in a densely urbanized area, would be very destructive anyway,\u201d Natale said.  <\/p>\n\n<div>This post appeared first on cnn.com<\/div>","protected":false},"excerpt":{"rendered":"<p>Forget Italy\u2019s most famous active volcano, Mt. Vesuvius, which destroyed Pompei in 79 AD. The most dangerous volcanic threat in Italy right now is one you\u2019ve probably never heard of: Campi Flegrei, or the Phlegraean Fields. This unassuming plain, which stretches 200 kilometers (125 miles)\u00a0under\u00a0the bay of Naples and the islands of Capri and Ischia <\/p>\n","protected":false},"author":0,"featured_media":11464,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[],"class_list":{"0":"post-11463","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-world"},"_links":{"self":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts\/11463","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/types\/post"}],"replies":[{"embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/comments?post=11463"}],"version-history":[{"count":0,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/posts\/11463\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/media\/11464"}],"wp:attachment":[{"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/media?parent=11463"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/categories?post=11463"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/shareperformanceinsight.com\/index.php\/wp-json\/wp\/v2\/tags?post=11463"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}