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Snow Layers and Cup Crystals

Inside snow, some layers are warmer than others. That difference slowly changes star-shaped crystals into loose, cup-shaped grains that can let a hard slab slide.

In the picture

  1. Dense white slab at the top of the snow cutaway.
  2. A cup-shaped faceted grain in the magnified inset.
  3. A star-shaped crystal in the lower snow layer.
  4. The dark ground at the bottom of the cutaway.

Examples

  • A hard crust on a ski slope can slide when a weak cup-crystal layer lies under it.
  • Sugar-like snow on a sidewalk can collapse under your boots.

Quiz: Snow Layers and Cup Crystals (Age 13)

  1. What causes star-shaped snow crystals to change into cup-shaped grains?

    • Temperature differences between layers inside the snowpack
    • The weight of the snow above pressing them flat
    • Wind blowing across the surface of the snow
  2. What can happen when weak, cup-shaped grains form in a snow layer?

    • The snowpack becomes stronger and less likely to slide
    • A hard slab above them can slide more easily
    • The snow turns into solid ice that cannot move
  3. Why are cup-shaped grains described as weak?

    • They hold the slab firmly in place
    • They are heavier than star-shaped crystals
    • They are loose and do not lock together well

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Physics, Age 13