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浆室内。

Deep below a volcano, beneath the Earth's mantle, is a magma chamber waiting to blow skyward.

在火山的深处，在地幔之下，是一个正等待着喷向天空的岩浆库。

Somewhere between 8,000 and 30,000 metric tons of carbon dioxide boil out of the magma chamber each day.

每天大约8000到30000吨的二氧化碳在岩浆中生成。

It was being warmed by radioactive elements in the granite that formed in the solidified magma chamber below.

在下面凝固的岩浆腔中形成的花岗岩中的放射性元素正在给它加热。

They'd pump cold water down into the wells, which over time, would cool a ring of rock around the magma chamber.

科学家们将冷水输送进这些井道，随着时间流逝，这些井道将冷却岩浆室内的一圈岩石。

It would involve drilling a series of wells around the perimeter of the volcano to send ice-cold water down to the magma chamber.

这将涉及在火山周围进行一系列钻井工程，以将冰冷的水送至岩浆室。

When too much gas accumulates within the magma chamber the pressure grows and grows.

当过多的气体在岩浆室内积聚时 ，压力就会越来越大。

Landslides can remove massive quantities of rock from atop a magma chamber, dropping the lithostatic pressure and instantly triggering an eruption.

山体滑坡可以从岩浆房顶部移除大量岩石，降低岩石静压力并立即引发喷发。

Even worse, cooling the rock could create fractures near the magma chamber, which might trigger a supereruption, the very thing we're trying to avoid in the first place.

更糟糕的是，冷却岩石将令岩浆室周围产生碎裂，而这可能会引起超级火山喷发，而这恰恰正是我们当初想避免的。

The shape, in turn, can be used to calculate the length of time the crystals sat in the magma chamber before erupting.

反过来，该形状可用于计算晶体在喷发前在岩浆库中停留的时间长度。

It's hard to say how big Everest's magma chamber might be, but it would have to be pretty large to send magma high enough to reach the surface.

很难说珠峰的岩浆库可能有多大，但它必须足够大，才能将岩浆喷发到足以到达地表的高度。

This magma, laden with dissolved gases like water vapor, carbon dioxide, and sulfur dioxide, is stored in a magma chamber beneath the volcano.

这种岩浆充满了水蒸气、二氧化碳和二氧化硫等溶解气体，储存在火山下方的岩浆室中。

While scientists can roughly determine the strength and weight of the Earth's crust, the depth and heat of magma chambers makes measuring changes in magmastatic pressure very difficult.

虽然科学家可以粗略地确定地壳的强度和重量，但岩浆房的深度和热量使得测量岩浆静压力的变化非常困难。

Both are clues that the volcanoes are connected by one big caldera, a massive crater that forms when a very large magma chamber in a volcano explodes and empties.

两者都是火山由一个大火山口连接的线索，一个巨大的火山口是在火山中一个非常大的岩浆室爆炸并排空时形成的。