The volcano threw new showers of magma and ash into the air.
这座火山向空气中喷发了新的岩浆和火山灰。
Are there any plates or magma lakes related to these earthquakes?
是否有某些板块或岩浆湖与这些地震有关呢？
The classic cone shapes of a Fuji or Kilimanjaro are created when erupting magma piles up.
富士山或乞力马扎罗山经典的圆锥形是由喷发的岩浆堆积而成的。
Under the water, volcanoes continued to erupt, sending up magma and forming mountains of basalt.
在水下，火山依旧持续喷发，向上喷射岩浆并形成了一座座玄武岩山峰。
Shield volcanoes formed when magma comes out of the ground in the same spot over and over again.
当岩浆一次又一次地在同一地点从地下涌出时，就形成了盾状火山。
Remember, magma is hot molten rock that's underground, and it is called lava when it reaches the surface.
记住，岩浆是地下炽热的熔化了的岩石，当它到达地表时就被称为熔岩。
As the magma smashes through layers of rock, it rips out debris, creating a mix of liquid and solid material.
当岩浆撞击岩层时，会出现岩屑，形成液态和固态物质的混合物。
A few hundred degrees separates this pool of fiery orange magma in Italy's Mount Etna from its hardened, gray crust.
在意大利的埃特纳火山，几百度的高温将这一池炽热的橙色岩浆与坚硬的灰色地壳分开。
There are those which sit over isolated 'hotspots' of upwelling magma from deep in the earth, like the volcanoes of Hawaii.
有那些座落于有不断从地底深处上涌岩浆的单独“热点” 之上的火山，就像夏威夷的火山一样。
He reasoned that iron took on more or less oxygen in response to conditions in the kimberlitic magma itself—mainly in response to heat and the available oxygen.
他推断，铁吸收或多或少的氧气是由于金伯利岩浆本身的条件——主要是由于热量和可用的氧气。
Hess suggested that the presence of water, probably released from minerals decomposing in the Earth's mantle, might have meant that a high-magnesium magma could have existed at a lower temperature.
赫斯认为，水的存在可能是由地幔中分解的矿物质释放出来的，这可能意味着含镁高的岩浆可能在较低的温度下存在。
The origination of the magma is related with the dehydration of the subducting plate of the Paleozoic Tethys Sea.
岩浆的起源与古生代特提斯海俯冲板块的脱水有关。
The magma-depth discovery may settle a longstanding debate.
岩浆深度的发现或能平息久悬未决的争论。
A million years ago, molten magma explosively burst above the waves.
一百万年前，熔化的岩浆在海波之上爆发性喷发出来。
If the magma breaks through to the surface, the result is a volcano.
如果岩浆冲出地面火山就爆发了。
Last major eruption: 1945, expelled a quarter cubic kilometer of magma.
最近一次大规模喷发：1945年，喷涌出0.25立方千米岩浆。
As it cooled, an ocean of magma covering its surface began to crystallize.
当星球冷却后，覆盖其表面的岩浆海洋开始定形。
These rocks formed around 3 billion years ago from the magma ejected by lunar volcanoes.
这些岩石是在约30亿年前由月球火山喷发的岩浆所形成。
Scientists had long known that magma Chambers must lie in the vicinity of the drill site.
科学家们了解到岩浆房一定就在钻探地的附近。
Never mind that magma made from subducted seafloorshas a habit of welling up in volcanoes.
来自潜没海床的岩浆会从火山涌出，这也是一个不得不考虑的因素。
So if hydrogen were present, more chlorine-37 would escape the magma along with chlorine-35.
所以，如果存在氢元素，更多的氯37就会与氯35一起自岩浆中散逸。
The best explanation, Sharp says, is that there was hardly any hydrogen in the moon's magma ocean.
夏普认为最好的解释就是：月球的岩浆海洋中几乎不存在氢元素。
But under the water, volcanoes continued to erupt, sending up magma and forming mountains of basalt.
但是在水下，火山依旧喷发，滚滚岩浆形成了玄武岩的山脉。
They added that there was no or very little hydrogen in the magma ocean during the Moon's formation.
他们补充说月球构造的熔岩层中几乎没有或仅存在极少量的氢元素。
Then there are those which sit over isolated "hotspots" of upwelling magma from deep in the earth, like the volcanoes of Hawaii.
然后就是那些座落于有不断从地底深处上涌岩浆的单独“热点”之上的火山，就像夏威夷的火山一样。
Volcanism at Sabancaya is fueled by magma generated at the subduction zone between the Nazca and South American tectonic plates.
补充到萨班·卡亚火山的岩浆生成于纳斯卡板块与南美洲板块之间的俯冲区域中。
Before it cooled, there was a so-called magma ocean on the Moon's surface - molten rocks, capable of retaining high quantities of water.
在月球冷却之前，它的表面有一个所谓的岩浆海洋-熔融岩，有保持大量水的能力。
Beneath the sediment, along the accretionary front, the sinking Arabian plate heats up under extreme pressure and rock melts into magma.
阿拉伯板块在高压的作用下升温，沉积物下方的岩石熔为岩浆。
Beneath the sediment, along the accretionary front, the sinking Arabian plate heats up under extreme pressure and rock melts into magma.
阿拉伯板块在高压的作用下升温，沉积物下方的岩石熔为岩浆。
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