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  • The Earth is a gigantic ball of semi-molten rockwith a heart of iron as hot as the surface of the  

    地球是個巨大的半熔化石球,其中心有個如太陽表面般炙熱的

  • Sun. Titanic amounts of heat left over from its  birth and the radioactive decay of trillions of  

    鐵塊。海量的地球誕生餘熱以及數萬億噸的放射性元素

  • tons of radioactive elements find no escape  but up. Currents of rock spanning thousands  

    除了向上以外沒有其他的逃脫方向。好幾千公里長的岩石流

  • of kilometers carry this energy to the surfaceEarth’s crust is the only thing in their way.  

    把這些能量帶到地球表面。唯一擋著它們去路的只有地殼

  • It feels solid to us, but it is only a fragile  barrier, an apple skin around a flaming behemoth.  

    我們覺得地殼很堅固,但它只是個脆弱的屏障,如包裹著燃燒中的龐然大物的蘋果皮

  • True apocalypses can break through  and unleash eruptions tens of times  

    真正的末日劫難可以突破地殼,釋放出比我們所有

  • more powerful than all of our nuclear weapons  combined, subjecting the climate to centuries  

    核武加起來強數十倍的噴發,使氣候在一年內經歷

  • worth of change in a single year, while  drowning continents in toxic ash and gases:  

    數百年的變化,並將各大陸淹沒於劇毒的火山灰和火山氣體之中

  • supervolcanoes. How big can they getAnd will they put an end to humanity?

    此劫難名為超級火山。它們能有多大?會造成人類滅絕嗎?

  • Volcanoes

    火山

  • There are many types of volcanosfrom towering mountains to lava domes,  

    從高聳的山到熔岩穹丘,火山的種類繁多

  • but they have two main sources:

    但它們有兩種主要成因

  • The first is at the boundaries between tectonic  plates, the pieces of the crust that cover the  

    第一種是在構造板塊邊緣。構造板塊是像拼圖一樣覆蓋地球的

  • Earth like a giant jigsaw puzzle. There are seven  major tectonic plates and dozens of smaller ones,  

    地殼碎片。有七個主要的構造板塊和數十個較小的板塊

  • drifting against each other at up  to 15 cm per year. This sounds slow,  

    它們以每年高達十五厘米的速度相互漂移。這聽起來很慢

  • but on geological timescales it istitanic struggle over who gets to stay  

    但在地質時間尺度上,這是場巨大的鬥爭,決定著

  • on the surface. The winning plate crumples  into a new mountain range while the loser  

    誰能留在地表上。獲勝的板塊坍塌成一個新的山脈,而失敗者

  • is shoved underneath, into an ocean of  hot rock at1300°Ct: The asthenosphere.

    被推到下方,進入一千三百攝氏度的熱岩海洋之中:軟流圈

  • The temperature here is enough  to melt rock into a liquid,  

    這裡的溫度足以將岩石熔化

  • but the insane pressures of all that  mass keep it a superheated solid.

    但那些質量所造成的瘋狂壓力使其保持於過熱固態

  • Tectonic plates are usually in contact  with water for thousands of years and  

    構造板塊通常與水接觸上千年並吸收

  • absorb some of it. When they are  submerged into the hot underworld,  

    其一小部分。當它們被隱沒在炙熱的地下世界時

  • this water triggers chemical transformations  that allow tiny portions to melt into magma.  

    這些水觸發化學變化,使小部分岩石熔成岩漿

  • Liquid magma is less dense than solid rockso it rises to the surface in furious bubbles  

    因為岩漿的密度比岩石小,它們像劇烈的泡泡般浮到表面

  • that accumulate in sponge-like reservoirs right  under the crust. If enough magma accumulates,  

    並在地殼下囤積成一個海綿狀的岩漿庫。如果有足夠的岩漿累積

  • it becomes powerful enough to pierce through the  crustwhich we experience as volcanoes. This  

    壓力強大到能突破地殼,這就是形成了我們所看到的火山

  • happens under the winning plate, like a revenge  attack by the loser before it is erased forever.

    這個過程發生在勝利板塊之下,像失敗者在被永遠消滅前展開復仇攻擊一般

  • The second main source of volcanoes are thought to  be mantle plumes. These are columns of abnormally  

    第二種主要的火山成因被認為是地幔熱柱。這些是異常熱的岩石柱

  • hot rock that rise all the way from the planet’s  core-mantle boundary to the surface. Much less is  

    從地球的核幔邊界一直上升到地表。我們對它們的了解不多

  • known about them, but in a way it is as if the  Earth’s mantle has weather patterns and mantle  

    但某程度上說,就好像地幔有天氣型態

  • plumes are a little like hot air rising to form  storm clouds. Storms hundreds of millions of  

    然後這些地幔熱柱有點像熱空氣上升形成暴風雲一樣。上百萬年

  • years old, made of rock circulating at  a rate of a few millimetres per month.  

    由石頭構成的風暴以每月數毫米的速度循環

  • They don’t care about the motion of tectonic  plates, so they can break the crust to create  

    它們不在乎構造板塊的運動,所以當地殼在它們周圍移動時

  • volcanoes in the middle of nowhere that stubbornly  stay active as the crust shifts around them.

    這些熱柱可以突破地殼在荒郊野外形成長期保持活躍的火山

  • The volcanic boom-meter

    火山爆發儀

  • Scientists love to put big booms onscale and came up with a logarithmic  

    科學家們喜歡把大爆發放在一個刻度上,並提出了一個對數刻度

  • scale that measures the volume ejected during  an eruption: The Volcanic Explosivity Index,  

    來測量火山噴發期間所噴出的體積:火山爆發指數

  • or VEI. Simply put, it starts really  small and gets very big very quickly.

    又稱VEI。簡單來說,VEI開始時非常小,然後會非常迅速地增大

  • A VEI 2 eruption would fill four hundred  full Olympic swimming pools with lava.  

    一個VEI二級的噴發能用熔岩填滿四百座奧林匹克游泳池

  • We have around 10 of these per year.

    我們每年有約十次這類的爆發

  • At VEI 3 we already see devastating effects,  

    在VEI三級我們已看到毀滅性的影響

  • like the eruption of the Semeru volcano in 2021  that destroyed thousands of homes in Indonesia.

    如在2021年的塞梅魯火山噴發,摧毀了印度尼西亞數千所房屋

  • At VEI 5, we see catastrophic amounts of  materials, cubic kilometers of debris, equivalent  

    在VEI五級,我們看到災難性數量的物質、好幾立方公里的碎片以及相當於

  • to an entire lake of molten rock blasted into  the air. Like the 2022 Hunga Tonga-Hunga Haapai  

    一座湖的熔岩噴發到空中。如在2022年的洪阿湯加-洪阿哈阿帕伊島的

  • eruption that sent a shockwave around the globe  many times and created ocean-wide tsunamis.

    海底火山爆發,多次在全球發出衝擊波並在海洋四處繼發海嘯

  • At a VEI of 6, an eruption can change the worldIn 1883, the Indonesian island volcano Krakatoa  

    在VEI六級,一個爆發能夠改變世界。在1883年,印度尼西亞的島嶼火山喀拉喀托

  • erupted nearly continuously over the course of  5 months. One of those eruptions blew it apart,  

    在五個月裡幾乎連續爆發。其中一次爆發將火山本身炸開

  • producing the loudest sound recorded in history,  

    製造出史上最巨大的聲響

  • 10 trillion times louder than a rocket  taking off, heard halfway around the world.  

    比火箭發射的聲音大十萬億倍,響徹半個世界

  • 30m high tsunamis swept away nearby populations  and so much gas and ash were released that  

    三十米高的海嘯席捲了附近的居民,其釋放出的氣體與火山灰如此之多

  • global temperatures cooled by nearly 0.5°C.  Red dusty sunsets followed for many years.

    全球溫度降低了近零點五攝氏度。塵土飛揚的紅色日落跟隨了許多年

  • At VEI 7, we get Super-Colossal  eruptions, millennium-defining  

    在VEI七級,我們見識到的是超巨大爆發。這種定義千年的

  • events that human civilization has  only encountered a handful of times.  

    事件人類文明目前只經歷過幾次

  • Mount Tambora was a 4300m high mountain  until it exploded in 1815 and released 400  

    坦博拉火山曾是高達四千三百米的高山,直到它在1815年噴發前為止,當時所釋放出的能量

  • times more energy than the Tsar Bomba.  140 billion tons of ash and dust were  

    比沙皇炸彈多四百倍。一千四百億噸的灰與塵被噴射至通往太空中途

  • shot halfway to space before smothering the  world’s skies, turning them a sickly yellow.  

    隨後掩蓋了世界的天空,將它染成病懨懨的黃色

  • There was no summer the following year, crops  died and over a hundred thousand people perished.

    之後的那一年沒有夏天。大量農作物死亡且十萬人以上喪生

  • This is the dreadful potential of volcanic  eruptions, with famines across the other  

    這是火山爆發的可怕潛力,世界另一端的飢荒

  • side of the world and even centuries-long  cold periods being attributed to them.

    甚至長達數百年的寒冷時期都歸因於它們

  • Ok. But what is a supervolcano?

    好的。那什麼是超級火山?

  • The termSuper volcanois a media invention  and not a scientific term. The main issue with  

    「超級火山」一詞是媒體發明的,並非科學術語。其最大

  • them is that not every eruption from  a supervolcano is a super eruption.

    問題在於超級火山每次爆發不一定是超級噴發

  • What makes super volcanoes special is that  they have been waiting to erupt for hundreds  

    超級火山的特別之處是,數十萬年來它們一直在等著爆發

  • of thousands of years. Pressure builds up in  colossal magma reservoirs several kilometers deep,  

    壓力在數公里深的巨大岩漿庫中積聚

  • until it becomes strong enough to lift  the rock above it by several meters.  

    直到它強到能將上方的岩石抬高數米為止

  • Rocks crack under the pressure, until they finally  give way and billions of tons of gas and ash blast  

    岩石在壓力下崩裂,直到它們最終讓路,使數十億噸的氣體與火山灰

  • out at supersonic speed. An insane explosion  of at least a thousand cubic kilometers that  

    以超音速炸出。這是一場至少涵蓋一千立方公里的

  • impacts every corner of the globe. And yet, that  is only a small portion of the magma reservoir.

    瘋狂大爆炸,衝擊著全球各個角落。然而,這只涉及到岩漿庫裡的一小部分

  • Super eruptions are like a boiling pot of water  popping its lid off and spilling a bit off the  

    超級噴發像一鍋滾水一樣,鍋蓋被掀開並從頂部溢出點水

  • top. Afterwards the ground collapses into  the void left behind, forming a hole called  

    爆發後地面陷落至剩下的虛空之中,形成一個洞

  • a caldera. Under this caldera, pressure starts  building again until the volcano gathers enough  

    名為破火山口。在這破火山口下方壓力再次開始積聚,直到火山集結足夠的

  • energy for another supereruptionbut this  could take hundreds of thousands of years.

    能量發生下一次超級爆發。但這可能需要數十萬年的時間

  • It is estimated that one of the few  volcanoes capable of supereruptions  

    我們預估地球上其中一座能超級噴發的火山

  • on Earth could cause a catastrophic eruption every  

    平均需要一萬七千年的時間

  • 17,000 years on average. That would make them far  more frequent than comparable asteroid impacts..

    才會造成災難性的爆發。這使它們比規模類似的小行星撞擊更頻繁

  • The most recent super-eruption is the Oruanui  eruption 26,500 years ago in New Zealand.  

    最近一次的超級噴發是兩萬六千五百年前在紐西蘭的Oruanui爆發

  • With the force of dozens of billions of tons of  TNT, a Mount Everest- sized pile of explosives,  

    其威力相當於數十億噸、如一座聖母峰般大的TNT炸藥堆

  • a huge portion of the landscape was  scooped out and thrown into the atmosphere.  

    有一大部分的景觀被挖出並扔到大氣層中

  • It left behind a caldera spanning 20km and  it caused the entire Southern Hemisphere  

    爆發形成的破火山口有二十公里寬,並導致整個南半球進入

  • to undergo a period of abrupt cooling. Though  among super-eruptions, it is a mere firework.

    一段突然的降溫期。話雖如此,和其他超級噴發比起來,這只是一束煙花

  • The Lake Toba eruption of 74,000 years ago  was a much more significant turning point  

    七萬四千年前的多巴湖爆發在史上是個更顯著的

  • in history. It released a gargantuan 5300 cubic  kilometers of material, enough to blanket parts  

    轉捩點。它釋放多達五千三百立方公里的物質,足以把部分

  • of South Asia in 15 cm of ash and trigger  a rapid 4°C drop in global temperatures.  

    南亞地區覆蓋在十五公分高的火山灰之中,並導致全球氣溫迅速下降四攝氏度

  • It’s possible that the volcanic winter lasted  ten years, followed by worldwide droughts for  

    這個火山冬天可能維持了十年,隨後是數百年的

  • centuries. Earth’s climate might have  not recovered for a thousand years.

    全球乾旱。地球的氣候有可能花了一千年才得以恢復

  • The largest volcanic events we know  of were not really huge explosions,  

    我們已知的最大型火山事件與大爆炸無關

  • but floods of millions of cubic kilometers of  lava. The grand finale were the Siberian Traps  

    而是數百萬立方公里的熔岩如洪水般氾濫。最為盛大的是

  • around 250 million years ago, a continuous  release of lava for two million years.  

    約二點五億年前的西伯利亞暗色岩,當時熔岩持續湧入兩百萬年

  • They raised the ocean temperatures to over 40°C,  which caused the PermianTriassic extinction,  

    把海洋溫度提升至四十攝氏度以上,這導致了二疊紀-三疊紀滅絕事件

  • killing over 90% of all species. Earth’s surface  needed 9 million years to recover. These sorts  

    殺死了百分之九十的所有物種。地表花了九百萬年才得以復原。這類的火山爆發

  • of eruptions don’t change the climatethey are the climate. But thankfully,  

    並不改變氣候,它們就是氣候本身。但幸運的是

  • we haven’t seen anything even remotely close  to that scale in many millions of years.

    數百萬年來我們還未看到任何接近如此規模的火山爆發

  • So. Should you be scared of super-volcanoesDefinitely not. Theyve been used to frighten  

    那麼,你需要害怕超級火山嗎?當然不需要。它們常被用來嚇唬

  • many people and are overhyped as an unavoidable  apocalypse. The most famous one, Yellowstone,  

    很多人,並被過度吹噓為無可避免的末日事件。最有名的是黃石公園

  • will erupt again, but they will  be relatively small eruptions.  

    會再度噴發。但到時的爆發規模會較小

  • Natural disasters for sure, but not enough to  devastate the US or come close to ending humanity.

    是屬於天災沒錯,但不足以摧殘美國,更不會造成人類滅絕

  • The chance of a VEI 8 eruption in the  next few hundred years is less than 2%  

    接下來數百年會發生VEI八級火山噴發的機率低於百分之二

  • and more importantly, it would  not come as a sudden surprise.  

    更重要的是,這類噴發不會突如其來的發生

  • However, less powerful but more  frequent eruptions can also do  

    然而,威力較弱但更頻繁的火山爆發也能對

  • serious damage to our civilizations and  are in many ways a much greater concern.

    文明帶來重大損傷,在很多方面上是更大的擔憂

  • So we must watch for slow changes in  magma reservoirs, like ground swelling  

    所以我們必須密切關注岩漿庫的變化,如地面隆起

  • and temperature increases, to get an early  warning that can save the lives of people  

    和溫度上升等,以發掘能拯救火山鄰近居民的

  • living the closest to a volcano. And there’s time  to develop solutions that can remove sulfur and  

    前期警訊。此外我們有時間設計能從平流層移除硫磺

  • ash from the stratosphere to eliminate the root  cause of the climate disruption weve seen from  

    和火山灰的解決方案,以消滅過往火山爆發破壞

  • previous eruptions. Who knows, maybe well even  be able to turn this force of destruction into  

    氣候的根本原因。誰知道呢,也許我們甚至能通過

  • an agent for good by exploiting the geothermal  energy held in their giant magma reservoirs.

    利用這些巨大岩漿庫的地熱能來駕馭這股破壞力行善

  • Weve done this work for so many other disasters  and we are already doing things we could only  

    我們已為其他許多天災付出這類心力,而且我們已經能做

  • have dreamed about decades ago, like sendingprobe to perform our first asteroid redirection  

    在幾十年前只能想像的事情,如第一次試驗發射飛行器改變

  • test. With determination, humanity really  can solve anything. So while deep below us  

    小行星軌道。只要有決心,人類真的可以排除萬難。所以雖然在我們地下深處

  • an angry hell is churning and waiting for  its moment, you can sleep well tonight.

    有個憤怒的地獄在翻騰,等待著它的時機,你今晚能安穩的睡個好覺

  • Learning how we can get ahead of catastrophes like  climate change and supervolcanoes is interesting,  

    學習我們如何能提前應對如氣候變化和超級火山等災難雖然有趣

  • but can also be challenging. Maybe you still  feel like you don’t really understand how  

    但也可能是件困難的事情。或許你覺得自己尚未了解

  • most of the science behind it works. And on  your own it seems too hard to dig deeper.

    這些現象背後的科學原理。光靠自己深入研究好像又太難了

  • To solve this, weve collaborated with our  friends from Brilliant to create a series of  

    為了解決這道難題,我們和在Brilliant的朋友們合力製作一系列課程

  • lessons to build your understanding of fundamental  scienceby exploring fascinating insights from  

    透過探索我們熱門視頻中的有趣見解,如黑洞、生命大小

  • our most popular videos, on topics like black  holes, the size of life, and climate change.

    氣候變化等,來建立你對基礎科學的理解

  • Brilliant is an interactive learning  tool that makes science accessible with  

    Brilliant是個通過動手的方法使科學變得容易的

  • a hands-on approach. Because we know that  to really learn something, youve got to do  

    互動學習平台。因為我們知道要真正學習某事物,你必須

  • it. Think of each lesson as a one-on-one  deep-dive version of a Kurzgesagt video.

    自己動手做。把每個課程當作是一對一的深入版Kurzgesagt視頻

  • In our latest lessons, youll discover the  mechanisms that drive climate change and  

    在我們最新的課程裡,你會發掘推動氣候變化的機制

  • use them to understand the impact of  supervolcanoes on our global climate.

    並利用它們了解超級火山對全球氣候所帶來的影響

  • Beyond new Kurzgesagt lessons regularly released,  

    除了這些定期發布的Kurzgesagt課程以外

  • Brilliant has thousands of lessons for members  to explorefrom math-based topics like algebra  

    Brilliant有上千堂課程,從數學方面的課題如代數和概率

  • and probability to the concepts behind  machine learning and quantum computing.  

    到機器學習和量子計算背後的概念,任會員探索

  • With new releases each month, youll  always find something fascinating to learn.

    隨著每個月的新發布,你總能找到一些有趣的東西來學習

  • To get hands-on with Kurzgesagt lessons now, go  to Brilliant.org/nutshell and sign up for free.  

    想動手學習Kurzgesagt的課程,現在上Brilliant.org/nutshell免費註冊

  • And with a free trial of Brilliant Premiumyou can explore everything Brilliant has to  

    通過免費試用Brilliant Premium,你能探索所有Brilliant的

  • offer. There’s even an extra perk for Kurzgesagt  viewers: the first 200 people to use the link  

    課程。Kurzgesagt觀眾更能享受特殊優惠:首兩百位使用這個連結

  • get 20% off their annual membership, which  unlocks all of Brilliant’s courses in math,  

    的人享有百分之二十的年度会員費折扣,並解鎖Brilliant所有

  • science, and computer science. We love to go down a rabbit hole  

    在數學、科學及電腦科學的課程。我們喜歡透過

  • with our researchBrilliant will take  you by the hand to come along on the ride.

    做研究進入複雜奇異且未知的世界,Brilliant將與你攜手踏上學習之旅

The Earth is a gigantic ball of semi-molten rockwith a heart of iron as hot as the surface of the  

地球是個巨大的半熔化石球,其中心有個如太陽表面般炙熱的

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