Squeezed Snow: How a Glacier Is Born
A glacier begins with a snowflake. In very cold places, some of the snow that falls in winter does not melt away in summer. The next winter, more snow lands on top of it. Year after year, the layers pile up.
The weight of the upper snow squeezes the snow below. Fluffy flakes turn into small, hard grains, and the air between them is pushed out. After many years, the grains pack together and become solid ice. When a mass of ice grows thick enough, a glacier has been born.
A glacier may look still, but it moves. Its great weight makes the ice flow slowly downhill, a little like thick syrup. It moves so slowly that you cannot watch it happen. As it creeps along, the ice scrapes up rocks and carries them. Over a long time, a glacier can carve a mountain valley into a wide U shape.
When the glacier reaches warmer land, its front edge melts. The rocks it carried are dropped in piles. The meltwater runs into streams, rivers, and lakes, so a glacier also gives water to the land below.