Difference between continental glaciation and alpine glaciation?

- Ice sheets cover large land masses, such as Antarctica and Greenland.

- Ice is typically thousands of meters thick.

- Glaciers flow outward from a central ice dome.

- Continental glaciers can erode and transport vast amounts of sediment.

- Continental glaciation can have a profound impact on climate, sea level, and ecosystems.

Alpine Glaciation

- Glaciers are confined to mountainous areas.

- Ice is typically hundreds of meters thick.

- Glaciers flow from high elevations to lower elevations.

- Alpine glaciers can erode and transport large amounts of sediment.

- Alpine glaciation can have a significant impact on local climate, water resources, and ecosystems.

Comparison Table

| Feature | Continental Glaciation | Alpine Glaciation |

|---|---|---|

| Location | Large land masses | Mountainous areas |

| Thickness of ice | Thousands of meters | Hundreds of meters |

| Flow of ice | Outward from a central ice dome | From high elevations to lower elevations |

| Erosional power | High | Moderate |

| Impact on climate | Profound | Significant |