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.
This picture is part of the full library
Every lesson is open to everyone for 7 days after it is published. This one came out on September 13, 2026: its text stays readable here, and its picture opens with a subscription.
The app is free. A subscription opens every lesson, in every school year.
Age 13: open this week
Browse Age 13In the picture
- Dense white slab at the top of the snow cutaway.
- A cup-shaped faceted grain in the magnified inset.
- A star-shaped crystal in the lower snow layer.
- 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.
Key takeaways
- Temperature differences inside snow can change crystal shapes.
- Cup-shaped grains are loose and weak, so a slab above them may slide.
Carry on in the app
Three questions on this lesson. It has left the free week, so its quiz is for subscribers.
At least one new illustrated lesson every weekday for your child’s year, with its quiz and a reminder at 6:15 pm.
Get the app
Free app, optional subscription
App Store Google Play