十万个为什么·科学启蒙30篇(1)
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Why Do Mountains Get Taller Over Time?
为什么山脉会随着时间越来越高?
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Mountains grow taller when tectonic plates push against each other underground.当地壳板块在地下相互挤压时,山脉会逐渐增高。
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This slow collision crumples Earth's crust and lifts land upward like folded paper.这种缓慢的碰撞使地壳褶皱变形,像折叠纸张一样将陆地抬升。
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Some mountains, like the Himalayas, rise about one centimeter every year on average.有些山脉(如喜马拉雅山)平均每年升高约一厘米。
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Erosion from wind and rain tries to wear them down at the same time.与此同时,风和雨水的侵蚀作用不断削低山体。
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But in active zones, uplift often outpaces erosion over long periods.但在活跃地带,长期来看抬升速度通常超过侵蚀速度。
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Scientists measure mountain growth using GPS satellites and precise laser surveys.科学家利用GPS卫星和精密激光测量技术监测山体增长。
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Volcanic activity can also add height quickly when magma rises and hardens.火山活动也能快速增加高度——岩浆上涌并凝固后形成新山体。
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Rock layers deep underground bend and break to accommodate the rising force.地下深处的岩层在上升力作用下发生弯曲或断裂以适应形变。
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Even though growth is tiny yearly, it adds up over millions of years.尽管每年增长微小,但经数百万年累积效果显著。
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That’s why today’s tallest peaks were once flat seabeds long ago.正因如此,如今最高的山峰在远古曾是平坦的海底。