Kungenzeka ukubuka indlela yokuziphatha kwe- umoya futhi i amanzi esikalini esihlukile: kusuka ekubonakalisweni okuncane kakhulu, njengeqhwa leqhwa, kuye kwesiphepho esikhulu. Phakathi kwalezi zinto ezimbili ezeqisayo, kunesenzakalo se ukucindezela umkhathi, amafu, imvula, amagagasi namagagasi.
Ukuhamba nje okulula noma izindaba kungaphakamisa imibuzo eminingi. Kungani isibhakabhaka siluhlaza? Kungani kunosawoti olwandle? Yini indlela engadala ifayili le- ukuhlushwa, isiphepho noma i-tsunami ebhubhisayo? Okulandelayo ehlobo kuzoba ukushisa noma, kunalokho, kuthambile kakhulu?
Ngakho-ke, i phenomena okubonakalayo emoyeni nasemanzini, kwezinye izimo, kungasimangaza noma kusesabise, njengesiphepho ePhilippines, esabulala abantu abangaphezu kuka-5.000 XNUMX ukuwa kusuka ngonyaka odlule. Kodwa-ke, lezi zimo zingasisiza futhi ukuba siziqonde kangcono.
Umthombo we Ukungcoliswa kolwandle kungumoya, obekwe ebusweni bolwandle. Lesi ngesinye sezici eziningi zokushintshana ngomkhathi wolwandle. Imvelo ye-physico-chemical yokungcola kwasolwandle ifana ncamashi naleyo ye- ukungcola kusuka emoyeni. Uhlu lwayo olude lubandakanya zonke izinto ezikhishwe phansi noma ku- izilwandle futhi kuvame ukuxhunyaniswa nemisebenzi yabantu.
Imifula yengeza okuningi ukungcola, ngamanzi ezitshalo aqukethe umanyolo kanye izibulala-zinambuzane, namanzi angcolile avela ezindaweni ezisemadolobheni, ezolimo noma zezimboni. Ngaphezu kwalokho, izimoto ezihamba olwandle zinengxenye ebalulekile kwi ukungcola komoya wasolwandle.
wangikhonza kakhulu ngomsebenzi wami wesikole