Rubuta ci gaba ga wannan sakin layi - Girgizar kasa ta faru ne sakamakon lalacewar turawa kusa da iyakar yankin da ke tsakanin yankin Pacific da Arewacin Amurka. Maganganun tensor na lokacin suna nuna cewa zamewa ya faru ko dai a kan tsaka-tsakin tsaka-tsakin da ke fuskantar kudu, ko kuma tsaka-tsakin tsaka-tsakin da ke fuskantar arewa maso gabas, wanda ya dace da matsewar gabas da yamma da ake tsammani a wannan yankin. A wurin wannan girgizar ƙasa, farantin Pacific yana motsawa kusan zuwa yamma dangane da farantin Arewacin Amurka a cikin saurin kowace shekara, yana nutsewa a ƙarƙashin Japan a Ramin Japan kuma yana nutsewa zuwa yamma a ƙarƙashin Japan. Cibiyar girgizar kasa tana yamma da cibiyar girgizar kasa ta Maris 2011
Ka yi haƙuri. Ya zo ne kawai kwanaki tara bayan shekaru goma na bala'in 11 ga Maris, 2011, kuma fiye da wata guda tun lokacin da girgizar kasa ta 7.3 ta faru a kudancin ranar 20 ga Maris.