<prompt> Hlalosa hore na moeli oa poleiti o fapaneng o theha joangnan  <response>: Instruction in English: Describe how a divergent plate boundary forms . Response in English: A divergent plate boundary is a location where two tectonic plates are moving away from each other. This process occurs as a result of the upwelling of magma from the mantle, which causes the plates to move apart. The magma rises to the surface and solidifies into new crust, creating new oceanic lithosphere.This process often begins within a continent, where a weak spot or rift appears in the lithosphere due to underlying thermal or tectonic activity. A plume of hot material from the mantle rises toward the surface, causing the crust to expand and thin, resulting in a rift valley. As the process continues and the plates move further apart, this rift will eventually become flooded by the ocean, creating a new mid-ocean ridge.At a mid-ocean ridge, the separation of the plates creates a gap through which the molten material from the mantle can rise up and fill. This material cools and hardens into a solid rock, forming a new strip of ocean floor. Over time, this process will continue, with the continued upwelling of magma from the mantle causing the plates to move further and further apart.Overall, the formation of a divergent plate boundary is a dynamic process that involves the interaction of the earths lithosphere, mantle, and oceans, driven by the internal heat and convective processes within our planet. . Response in Sesotho: Moeli o fapaneng oa poleiti ke sebaka seo lipoleiti tse peli tsa tectonic li suthelang hole le tse ling. Tsebetso ena e etsahala ka lebaka la ho phahama ha magma ho tloha seaparong sa mantle, e leng se etsang hore lipoleiti li arohane. Magma e nyolohela holimo ebe e tiea ho ba bokaholimo bo bocha, e theha lithosphere e ncha ea leoatle. Hangata tsebetso ena e qala ka hara khonthinente, moo sebaka se fokolang kapa sekhahla se hlahang lithosphere ka lebaka la tsebetso ea mocheso kapa ea tectonic. Molomo oa lintho tse chesang tse tsoang seaparong sa ka holimo o nyolohela holimo, o etsa hore bokaholimo bo atolohe me bo be tšesaane, e leng se etsang hore ho be le phula ea likhohlo. Ha tsebetso e ntse e tsoela pele me lipoleiti li ntse li tsoela pele ho arohana, lekhalo lena le tla qetella le tletse metsi ke leoatle, me ho be le lekhalo le lecha la bohareng ba leoatle. Bohareng ba leoatle, karohano ea lipoleiti e baka lekhalo leo ka lona masela a qhibilihileng a tsoang seaparong sa mantle a ka phahamang me a tlala. Sesebediswa sena sea phola ebe se thatafala hore e be lefika le tiileng, ebe se etsa karolo e ntjha ya fatshe lewatleng. Ha nako e ntse e ea, tsebetso ena e tla tsoela pele, ha magma a ntse a tsoela pele ho phahama ho tloha seaparong sa mantle ho etsa hore lipoleiti li tsamaee le ho feta. Ka kakaretso, ho thehoa ha moeli oa lipoleiti tse fapaneng ke tsebetso e matla e kenyelletsang ho sebelisana ha lithosphere, mantle le maoatle a lefatse, e tsamaisoang ke mocheso o ka hare le mekhoa ea convective ka hara polanete ea rona. 