Nothing is stopping the magma from seeping even deeper into the sandy subsoil.

没有东西可以防止岩继续向下渗透到沙质底土。

And you'd spy red magma pooling along its sides.

你会看到红色的岩在它的两侧汇聚。

The dense atmosphere and hot temperature slows the magma from cooling into solid rock.

浓密的大气和炽热的高温岩的冷却速度很慢。

The magma collects in chambers around 10 miles below the surface.

岩在地表以下约 10 英的腔室内聚集。

Lava fountain sprayed, magma flowed, ash rained down on the surrounding region.

熔岩泉出，岩流出，火山灰如雨点般在周围地区落下。

The outer rock, or magma, was completely melted producing a molten ocean.

外部岩石或者说岩完全融化，形成一片“熔海洋”。

And the ground began to deform, likely due to flows of magma.

地面开始变形，可能是因为岩流动。

And the ground began to deform, probably due to flows of magma.

地面开始变形，可能是由于熔岩流动。

And yet, that is only a small portion of the magma reservoir.

然而，这只涉及到岩的一小部分。

And that also means there is magma very close to the surface here.

有时其中的热量沸腾起来冒出像这样的泥火山。

And this is the biggest and noisiest way of seeing what magma is.

这就是岩最壮观、最喧闹的景象。

And then, these clouds fall as rains of magma, heading back to the surface.

然后，这些云层以岩雨的形式落下，返回地表。

The white-hot magma has cracked the cement slab and seeped into the empty basin.

高热岩已经将水泥板烧裂 渗入了没有水的凹地。

This magma is very hot, and under a lot of pressure.

岩温度很高，并且处于一定的压力之下。

Magma surges towards the surface and carrying diamonds.

岩裹挟着钻石，涌向地表。

But the rest stays underground, inside the supervolcano's magma chambers.

但是其余的热量蛰伏于地下，存储在超级火山的岩室内。

The magma inside the volcano was under enormous pressure and had gasses trapped within it.

火山内部的岩承受着巨大的压力，并将气体困在其中。

These strange rock clouds will then rain liquid rock or magma back onto the surface.

然后，这些奇特的岩石云会向地面下液态的岩石雨或者岩。

They say it looks like there's a lot of magma movement in the mountain.

科学家们表示当时看起来就像山上有大规模岩运动。

These are all types of magma, which becomes lava when they reach the Earth's surface.

这些都是各种类型的岩，当它们到达地球表面时就变成了熔岩。