Ukuvuselelwa kwentaba-mlilo eshisayo yezingane

Ukufanisa

Imishini esanda kwakhiwa engenamandla yokukhuphuka kwamatshe entaba-mlilo eminyakeni yakamuva. Isekelwe ezintweni ezingaqondakali, umbukwane futhi umbhoshongo volcanic imvelo njengoba ingemuva, futhi ifakwe amatshe akhuphukayo ahlanganiswe nokukhuphuka kwamatshe. Kunemibuthano yamatshe akhuphukayo ekukhuphukeni kwamatshe entaba-mlilo. Izingane zingaqala ukugibela zisuka phansi kuqala, bamba amatshe akhuphukayo ngezandla zombili futhi ukhuphuke. Lapho bekhuphukela esiqongweni sentaba, bangashelela ukusuka ku-slide phezulu kwe “intaba-mlilo” noma kusukela ebusweni be “intaba-mlilo” umthambeka. Uma wehla, umuzwa wokuslayida weslayidi ngokwaso ungavumela izingane zizwe injabulo kanye nokukhuthazwa kokushesha ukwehla ukusuka kusilayidi esiphezulu, okuyinto evumela ukuthi izingane zisebenzise ukucabanga kwazo.