| 1. | Upward pressure from underlying magma domes the surface
地下岩浆的向上推力使地面成圆顶形。 |
| 2. | A volcano is simply the opening in the earth from which the magma escapes
所谓的火山简单的定义就是指能够喷发出岩浆的山。 |
| 3. | Ice is congealed by water , mountains are made by magina , love is made by terrs , love is shown by sincereness
冰是水的凝固，山是岩浆的凝固，泪是情的凝固，爱是真诚的凝固。 |
| 4. | Here are a few tips to quickly making a stream of flowing lava . i hope somebody out there can use it
这是一个关于如何快速构建一个缓慢流动的岩浆的小技巧。我希望有人能用得上它。 ） |
| 5. | Note that you will need to change the key - frame types to linear , if you want the lava ' s speed to be constant
（注意，你需要改变关键帧类型为直线，如果你希望岩浆的速度保持恒定的话。 ） |
| 6. | So when we are talking about architecture , architecture now has to cope with this enormous spread like molten lava of media , over everything
因此我们讲到建筑的时候，就必须面对这个媒体的岩浆的世界。 |
| 7. | But careful studies of microscopic , magma - filled bubbles trapped inside tiny crystals of quartz tell a different story
但是，详细研究石英的微小晶体内那些仅能在显微镜下看到、充填著岩浆的气泡，则令我们发现了不同的故事。 |
| 8. | As the magma evolved chemically , it withdrew from the chamber underneath the summit , causing the ground there to collapse and feeding eruptions on the flanks
随著岩浆的化学演进，从火山山峰下的岩浆库退去，造成地面塌陷，并促成了侧边的爆发。 |
| 9. | A look at the composition of tiny crystals trapped inside erupted lava and ash at yellowstone has suggested a partial answer , by providing new insight into how magma forms
藉由研究黄石国家公园喷发熔岩与火山灰内的微小晶体，这个疑问获得了部份解答，也使我们对于岩浆的形成机制有了新的见解。 |
| 10. | The rate at which magma leaves a chamber depends primarily on two factors : the magma ' s viscosity , or ability to flow , and the pressure difference between the chamber and the earth ' s surface
岩浆从岩浆库喷出的速度，主要取决于两个因素：岩浆的黏滞性（或是流动能力）以及岩浆库与地表的压力差。 |
