Glacial ice is a different color than regular ice. It is so blue because the dense ice of the glacier absorbs every other color of the spectrum except blue--so blue is what we see!
It's Not Frozen Water!
Sometimes the glacial ice appears almost turquoise. Its crystalline structure strongly scatters blue light. The ice on a glacier has been there for a really long time and has been compacted down so that its structure is pretty different than the ice you normally see. Glacial ice is a lot different than the frozen water you get out of the freezer.
It's Not Frozen Snow!
Glacial ice is not just frozen compacted snow. There are other things in the ice that make it much different than the ice in your home. Glaciers move through rock and soil as they carve their way down a slope. This means the ice is going to have a lot more ingredients than just water.

Wow! Just Imagine...
What would happen if you broke off a big chunk of ice from a glacier and put it in your glass of water? Would it be any different than the ice in your freezer at home? What would happen to all those air bubbles that have been trapped under pressure?
* If your chunk of glacial ice melted in your glass of water, then you would have dirt, gravel, and even organic matter [living stuff] in your water.
* All those pressurized air bubbles would rush out so fast, they might explode your glass!
absorb
reflect
spectrum
organic matter
(some of the answers may come from the vocabulary list)
Glacier ice is highly pressurized. Bubbles in glacier ice get squeezed and pushed around. Sometimes, you can see round bubbles that have been squeezed into long rods or flat plains. Coarse-bubbly ice looks whiter than most other ice because it is filled with small bubbles. This kind is usually found near ablation areas of a glacier. Coarse-clear ice is free of bubbles and is the bluest ice of all. This kind is usually found near the margins and terminus of a glacier.
Look at ice cubes grown in your freezer. These ice cubes first froze on their outsides and trapped air bubbles toward the center. As a result, the exterior is bubble-free while the interior has bubbles. Bubbles in between the outside and the inside of the cube are probably longer and more extended. Can you see the differences?
(Courtesy Glaciers of North America, By S. Ferguson)