Glaciers: How Ice Shapes the Land | PHY‑103 | Module Three Assignment
Introduction Think of a glacier as a slow‑moving river made of ice. Once the ice is thick enough—about 30 meters or more—its own weight makes the bottom layers creep forward. That steady flow lets glaciers carve and carry rock in ways snowfields never could (National Snow & Ice Data Center [NSIDC], 2024). How Glaciers Grow and Shrink A … Read more
