返回

十万个为什么·科学阅读30篇(9)

23 / 30
已读 0 / 30 课
Why Glaciers Flow Like Very Slow Rivers — Not Just Slide Downhill

Why Glaciers Flow Like Very Slow Rivers — Not Just Slide Downhill

为什么冰川像极慢的河流一样流动,而不仅是沿山坡滑落?

  1. Glaciers move not just by gravity pulling ice downhill, but also by internal deformation under immense pressure.
  2. Ice crystals slowly slide past one another when temperatures rise near the melting point, even below zero degrees Celsius.
  3. Basal sliding occurs where meltwater lubricates the glacier’s base, allowing it to glide over bedrock.
  4. Scientists measure flow rates using GPS markers embedded in the ice that shift position over months.
  5. Thicker glaciers deform faster because pressure increases with depth, weakening the ice structure internally.
  6. Crevasses form where flow speeds change abruptly, revealing how stress builds and releases within the ice mass.
  7. Some glaciers surge suddenly, moving hundreds of meters in weeks due to trapped subglacial water release.
  8. Climate warming accelerates both melting and flow, altering sea level and freshwater supplies globally.
  9. Glacier movement records past climate conditions in layers of trapped air bubbles and dust.
  10. Studying this slow motion helps predict future coastal flooding and mountain water availability.
上一页
/ 30
下一页