What Is The Difference Between Glacial Ice And Regular Ice? — Reading Comprehension

When you put ice cubes in a drink, you're seeing regular ice. But high up in mountains or near the Earth's poles, there's another kind of ice called glacial ice. Both are made of frozen water, but they are very different! Understanding these differences helps us learn about Earth's changing surface.

Regular ice forms when water freezes quickly, like in your freezer. This rapid freezing traps tiny air bubbles inside, making regular ice look cloudy or white. If you look closely at an ice cube, you might see these bubbles. Regular ice is less dense than glacial ice because of these trapped air pockets.

Glacial ice forms in a much slower and more powerful way. It begins as snow that falls and accumulates year after year in cold regions. As more snow piles up, the weight of the new snow presses down on the older layers below. This intense pressure causes the snow crystals to change shape and pack together very tightly. Over hundreds or even thousands of years, this compression pushes out most of the air between the snow crystals, turning them into dense, solid ice.

Because glacial ice has very few air bubbles, it looks different. It often appears blue! This blue color is because when sunlight hits the very dense ice, the ice absorbs red light and reflects blue light. This makes glaciers look incredibly beautiful. Glaciers are massive rivers of ice that slowly move, carving out valleys and shaping Earth's landscape over long periods. They are a major part of Earth's geoscience processes, constantly changing the surface.

Another key difference is density. Glacial ice is much denser than regular ice. Imagine comparing a fluffy snowball (new snow) to a hard, packed snowball (older snow, on its way to becoming glacial ice). The glacial ice is much heavier for its size. This high density allows glacial ice to resist melting for longer and makes it incredibly strong. Studying glaciers helps scientists understand past climates and predict future changes to our planet, including the impact of climate change on these vast ice formations.

Interesting Fact: Some glacial ice can be so old that it contains air bubbles from thousands of years ago, giving scientists clues about Earth's ancient atmosphere!

What makes regular ice look cloudy?

What is glacial ice made from?

Glacial ice typically appears blue because it reflects blue light.

Which type of ice forms faster?

What process causes snow to turn into glacial ice?

Why is glacial ice denser than regular ice?

If you had a block of regular ice and a block of glacial ice of the same size, which would feel heavier?

The word 'compression' means:

Which type of ice is more likely to show distinct layers from different snowfalls?

Which of these is a 'geoscience process' mentioned in the passage?