<prompt> Bapisa le ho bapisa likarolo tse nè tsa Lefatše.nan  <response>: Instruction in English: Compare and contrast the Earths four layers. . Response in English: The Earth is made up of four primary layers that each have their own distinct properties and characteristics: the crust, mantle, outer core, and inner core. The first layer is the crust, which is the thin outermost layer that we live on. It is on average 30km thick and is composed mostly of lightweight elements such as oxygen, silicon, and aluminum. The crust can be divided into two types- the continental crust, which is thicker and less dense, and the oceanic crust, which is thinner and denser.The next layer is the mantle, which is the thickest layer of the Earth. It is about 2,900 km thick and consists primarily of iron and magnesium. The mantle can be further divided into the upper and lower mantle, with the upper mantle being made up of rigid material and the lower mantle being more fluid. Below the mantle is the outer core, which is the Earths only fully liquid layer. It is composed primarily of iron and nickel and is about 2200 km thick. This layer is responsible for generating the Earths magnetic field through the movement of molten iron.Finally, the inner core is the Earths central layer and is the hottest and most dense part of the planet. It is a solid sphere with a radius of 1,250 km, and is made up of iron and nickel. Despite the heat, the inner core is able to remain solid due to the intense pressure at the Earths center.In summary, the Earths layers can be distinguished by their composition, thickness, state of matter and other properties. The layers become denser, hotter and under higher pressure as one moves from the crust to the inner core. . Response in Sesotho: Lefatše le entsoe ka mekhahlelo e mene ea mantlha eo e ngoe le e ngoe e nang le thepa le litšobotsi tse ikhethang: bokaholimo, seaparo sa ka holimo, bokahare ba bokantle le bokahare bo ka hare. Lera la pele ke lekhapetla, e leng karolo e ka ntle e tšesaane eo re phelang ho eona. E ka ba bolelele ba 30km mme e entsoe haholo ka lintho tse bobebe tse kang oksijene, silicon le aluminium. Lekhapetla le ka aroloa ka mefuta e meli- bokaholimo ba continental, bo botenya ebile bo fokola haholo, le bokaholimo ba leoatle, le lesesaane ebile le le lesesaane. Lera le latelang ke seaparo sa ka holimo, e leng karolo e teteaneng ka ho fetisisa ea Lefatše. E ka ba bolelele ba likhilomithara tse 2,900 me e na le tšepe le magnesium. Seaparo sa ka holimo se ka aroloa hape ka seaparo sa ka holimo le se ka tlaase, me seaparo se ka holimo se entsoe ka thepa e thata me seaparo se tlaase se na le metsi a mangata. Ka tlasa seaparo sa ka holimo ho na le mokokotlo o ka ntle, e leng sebaka se le seng sa metsi se feletseng sa Lefatše. E entsoe haholo-holo ka tšepe le nickel me e ka ba bolelele ba likhilomithara tse 2200. Lera lena le na le boikarabello ba ho hlahisa matla a lefatše a khoheli ka ho tsamaea ha tšepe e qhibilihisitsoeng. Qetellong, bokahare bo ka hare ke karolo e bohareng ea Lefatše me ke karolo e chesang ka ho fetisisa le e teteaneng ka ho fetisisa ea polanete. Ke selikalikoe se tiileng se nang le radius ea likhilomithara tse 1,250, me se entsoe ka tšepe le nickel. Ho sa tsotellehe mocheso, mokokotlo o ka hare o khona ho lula o tiile ka lebaka la khatello e matla setsing sa Lefatše. Ka kakaretso, likarolo tsa Lefatše li ka khetholloa ka sebopeho sa tsona, botenya, boemo ba taba le lintho tse ling. Likarolo li fetoha tse teteaneng, ho chesa haholo le tlasa khatello e phahameng ha motho a tloha bokahare ho ea bohareng ba ka hare. 