Mun riga mun san yadda dutsen da aka samu a duniyarmu sakamakonsa ne magma yana tashi ta cikin alkyabbar, amma koyaushe mun kasance muna iya hango inda zasu fito.
A karo na farko a Cikakken taswirar 3D na cikin ƙasa lokacin da kake nazarin tsarin taguwar girgizar kasa. Samfurin yana nuna alkyabba, daidai daga inda dutsen mai rai yake gudana kuma cewa yana farawa tsakanin ƙasan waje da babbar rigar ko menene zai zama rashin katsewar Gutenberg don tashi zuwa saman, inda yake haɗuwa da wuraren da duwatsun ke cikin ƙasan ƙasa.
Ginshikan volcanic ba sa jagorar madaidaiciyar hanya zuwa farfajiya, a'a siffofin ban mamaki tare da karkacewar da ba zato ba tsammani. Yanzu kuma sanannen abu ne cewa yawancin duwatsun wuta na duniya, kamar sarƙoƙin tsibirin Fasifik, sun fito ne daga manya-manyan "ƙusoshin" dutse biyu masu zafi a yankin da aka ambata a sama, kamar katsewar Gutenberg.
Samfurin ba a karan kansa cikakke bane, tunda ba haka bane ɗaure wasu gashinsa zuwa wasu duwatsun wuta, kamar wanda aka samu a Filin shakatawa na Yellowstone. A kowane hali, yana aiki daidai don wakiltar shaidar waɗannan magma da kuma kasancewarta mataki na farko don manyan taswira masu ƙarfi don wanzu a nan gaba ta hanyar tauraron dan adam tare da na'urori masu auna karfin magana.
A halin yanzu an san shi kamar yadda Duniya take yadudduka kamar albasa kuma a bayanta akwai tekuna da nahiyoyi, yayin kuma daga ciki labulen alkyabba yana da kaurin kilomita 2.900. Karkashin wannan alkyabbar ita ce gindinta na waje, wanda aka hada shi da baƙin ƙarfe da baƙin ƙarfe, wanda yake lulluɓe baƙin ƙarfe na ciki a tsakiyar duniya.
Kamar yadda yake har yanzu komai wani sirri a cikin duniyar mu, Shine matakin farko da aka ɗauka don samun ingantaccen ilimin godiya ga waɗancan manyan kwamfutocin waɗanda ke taimaka mana wajen nuna hanyar da wannan magma da ke tasowa daga zurfin ke tafiya.
Idan kana da son sani don ƙarin sani game da dutsen mai fitad da wuta wuce ku don wannan shigarwar ga shubuhohi game da lokacinta.