This heat source powers the convection currents, Magma here gets heated up, Hot magma rises up because it is less dense, Magma here starts to cool off, Cool magma sinks because it is more dense, Magma gets close to the heat again and the process repeats.

Convection Current Diagram

由
嵌入

排行榜

視覺風格

選項

切換範本

恢復自動保存: ?