Passage Excerpt:
Glaciers move across landscapes through two primary mechanisms: basal sliding and internal deformation. Basal sliding occurs when liquid water under immense pressure acts as a lubricant beneath the glacier, allowing the entire ice mass to melt slightly at its base and slide over bedrock. In contrast, internal deformation occurs when individual ice crystals within the glacier slip past one another under the weight of overlying ice without requiring subglacial liquid water. While basal sliding dominates in warmer temperate glaciers where basal ice reaches the melting point, internal deformation is the principal movement mechanism in cold polar glaciers, where the ice remains frozen solid to the bedrock below.
Based on the passage, what is one explicitly stated difference between basal sliding and internal deformation?
- Basal sliding requires subglacial liquid water to facilitate movement, whereas internal deformation occurs without requiring subglacial liquid water.Answer
- BBasal sliding occurs when ice crystals slip past one another under heavy weight, whereas internal deformation relies on melting ice at the bedrock surface.
- CBasal sliding serves as the primary movement mechanism in cold polar glaciers, whereas internal deformation predominates in warmer temperate glaciers.
- DBasal sliding enables glaciers to travel across bedrock, whereas internal deformation causes glaciers to remain completely motionless.