構造-氣候相互作用
火山 > 結論

火山是地球上的一個強大景觀。火山的產生取決於它的位置和岩漿起源。岩漿可保持熔體狀態，直到壓力和溫度能允許結晶和排氣。當岩漿上升到地球表時，就形成火山。根據熔體物質的成分，每座火山可能含有多種氣體。火山噴發排放的大部分氣體是有溫室效應的氣體，會導致大氣變化。然後這些大氣變化迫使區域和局部的氣候造成新的大氣。這些變化可以反映為冷卻、變暖、更高的降水率等等。
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