<prompt> Hlalosa hore na tsunami e thehoa joangnan  <response>: Instruction in English: Describe how a tsunami is formed . Response in English: A tsunami is a series of large waves generated in the ocean by sudden, catastrophic events such as underwater earthquakes, volcanic eruptions, landslides or meteorite impacts. Most commonly, tsunamis are triggered by earthquakes that occur at the ocean floor along tectonic plate boundaries. When two tectonic plates collide or slide against each other, the seismic energy released during the movement of the earths crust can cause a portion of the sea floor and water above it to suddenly rise or fall. The water then displaces vertically, creating a huge wave that propagates quickly across the ocean. The impact of the earthquake may also create fractures or movement in the ocean bottom that result in the release of large volumes of gas, water and sediment, which force the water upward or outward.As the wave travels across the open ocean, its height may only be a few feet and may be difficult to detect. However, once the wave approaches the shallow waters near the coast, its energy is compressed into a smaller area, causing the wave to grow in height, sometimes reaching up to 100ft. The water can also surge inland, causing flooding, destruction and loss of life.It should be noted that not all earthquakes generate tsunamis, and the factors that determine whether an earthquake will trigger a tsunami include its magnitude, depth, and the type of movement along the fault. In addition, tsunamis can also be triggered by landslides, volcanic eruptions or the impact of a large meteorite. . Response in Sesotho: Tsunami ke letoto la maqhubu a maholo a hlahisoang ka leoatleng ke liketsahalo tsa tšohanyetso, tse kotsi joalo ka litšisinyeho tsa lefatše tse ka tlasa metsi, ho foqoha ha seretse se chesang, ho khohomoha ha lefatše kapa litlamorao tsa meteorite. Hangata, li-tsunami li bakoa ke litšisinyeho tsa lefatše tse hlahang botebong ba leoatle haufi le meeli ea tectonic plate. Ha lipoleiti tse peli tsa tectonic li thula kapa li thella khahlanong le tse ling, matla a ho sisinyeha ha lefatše a tsoang nakong ea ho sisinyeha ha bokaholimo ba lefatše a ka etsa hore karolo e ngoe ea botebo ba leoatle le metsi a ka holima lona a phahame kapa a theohe ka tšohanyetso. Ka mora moo metsi a tsamaea a otlolohile, me a etsa leqhubu le leholo le namang ka potlako ho pholletsa le leoatle. Tšusumetso ea tšisinyeho ea lefatše e ka boela ea baka ho robeha kapa ho sisinyeha botebong ba leoatle hoo ho fellang ka ho ntša likhase tse ngata, metsi le matsoai, tse qobellang metsi ho ea holimo kapa ka ntle. Ha leqhubu le haola leoatleng le bulehileng, bophahamo ba lona e ka na ea e-ba limithara tse maloa feela me ho ka ba thata ho le lemoha. Leha ho le joalo, hang ha leqhubu le atamela metsing a sa tebang haufi le lebōpo, matla a lona a hatelloa sebakeng se senyenyane, ho etsa hore leqhubu le hōle ka bolelele, ka linako tse ling le fihla ho 100ft. Metsi a ka boela a kena ka hare ho naha, a baka likhohola, tšenyo le tahlehelo ea bophelo. Ho lokela ho hlokomeloa hore hase litšisinyeho tsohle tsa lefatše tse hlahisang tsunami, me lintlha tse khethollang hore na tšisinyeho ea lefatše e tla baka tsunami e kenyeletsa boholo ba eona, botebo, le mofuta oa motsamao ho ipapisitse le phoso. Ho feta moo, tsunami e ka boela ea bakoa ke ho ritsa ha lefatše, ho foqoha ha seretse se chesang kapa tšusumetso ea meteorite e kholo. 