Heat supplies the energy that causes motion. The deeper you go into toward the Earths core, the hotter it gets. At the core it is really hot. All that heat tries to rise toward the surface. In the Mantle, the rock is partially melted and is able to move. As it is heated, the material in the mantle moves toward the surface. As the mantle material rises, it cools. When it reaches the Earths crust, it is mostly stopped. A little of the material can break through the surface, but not all. Instead, it begins to move horizontally. The mantle material moves horizontally away from a mid-ocean ridge crest. Toward the surface, the mantle material starts to cool. As it cools it sinks back down into the mantle. These areas are where deep sea trench occur. The material sinks back down to the core. The system operates like a giant conveyor belt. The motion due to heating and cooling is called convection. 

Question: "Where does the heat deep in the Earth try to go?"

Response: "Even deeper"

Does the response correctly answer the question?

OPTIONS:
- no
- yes
no
Värme ger den energi som orsakar rörelse. Ju djupare man går in mot Jordens kärna, desto hetare blir den. I kärnan är det riktigt varmt. All värme försöker stiga upp mot ytan. I Manteln är bergarten delvis smält och kan röra sig. När den värms upp rör sig materialet i manteln mot ytan. När mantelmaterialet stiger svalnar det. När den når jordskorpan stoppas den mest. Lite av materialet kan bryta igenom ytan, men inte allt. Istället börjar den röra sig horisontellt. Mantelmaterialet rör sig horisontellt bort från ett mittoceanskt åskam. Mot ytan börjar mantelmaterialet svalna. När den svalnar sjunker den tillbaka ner i manteln. Dessa områden är där djuphavsgrav förekommer. Materialet sjunker tillbaka ner till kärnan. Systemet fungerar som ett jättelikt transportband. Rörelsen på grund av uppvärmning och kylning kallas konvektion. Fråga: Vart försöker hettan djupt inne i jorden ta vägen? Svar: "Än djupare" Svarar svaret rätt på frågan? ALTERNATIV: - nej - ja
Heat gives the energy that causes movement. The deeper you go into Earth's core, the hotter it gets. At the core, it's really hot. All the heat is trying to rise to the surface. In the Mantle, the rock is partially melted and can move. When heated, the material in the mantle moves towards the surface. As the mantle material rises, it cools. When it reaches the crust of the earth, it is stopped most. Some of the material can break through the surface, but not everything. Instead, it starts moving horizontally. The mantle material moves horizontally away from a midocean ridge crest. To the surface, the mantle material begins to cool. As it cools, it sinks back into the mantle. These areas are where deep-sea graves occur. The material sinks back down to the core. The system works like a giant conveyor belt. The movement due to heating and cooling is called convection. Question: Where does the heat in the deep soil try to go? Answer: "Even deeper" Answeres the question correctly? ALTERNATIVE: - no - yes
nt
nt