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Now, there are several kinds of ice you'll find plastered on these mountains. First, we've got **glaciers**. These are massive, slow-moving rivers of ice, formed over centuries by the compression of snow. They're like frozen time capsules, and they sculpt the landscapes as they inch their way down. Then, there's **snow**. Yes, snow! But on mountains, it's often more than just a fluffy blanket. It accumulates and compresses, eventually becoming part of the glacier or perennially frozen snowfields. We also see ice caps, which are like glaciers but cover a larger area. They’re usually ilmzh737 max documentary netflix less defined in terms of flow compared to glaciers. You might encounter **permafrost**, which is ground that remains frozen for two or more years consecutively. Even lakes and streams high up can freeze, contributing to the overall ice cover. Furthermore, **avalanches** are a dramatic way ice is moved from the mountains. This ice can be incredibly diverse, ranging from clear, dense glacial ice to porous, fluffy snow. The nature of the ice depends a lot on the temperature, the rate of snowfall, the amount of wind, and the time the ice has to compact.
