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Geosciences LibreTexts

5: Glaciers

  • Page ID
    13485
    • 5.1: Introduction
    • 5.2: Classification of Glaciers
    • 5.3: Distribution of Glaciers
    • 5.4: Glacier Ice
    • 5.5: The Budget of Glaciers
    • 5.6: Movement of Glaciers
      An important consequence of the balance considerations in the previous section is the glacier tends to thicken in its upper part and thin in its lower part, thus increasing its surface slope. The glacier flows under its own weight, passing ice across the equilibrium line to maintain an equilibrium slope.
    • 5.7: Deformation of Ice
      As in many crystals, the way ice crystals are deformed or sheared when a stress is applied is by propagation of dislocations through the crystal. A dislocation is a line defect in a crystal that disrupts the otherwise ideal and regular arrangement of atoms or molecules.
    • 5.8: The Thermal Structure of Glaciers
      A glacier can gain or lose heat in several ways. It’s clear that these processes operate both at the surface of the glacier and at the base of the glacier. What are these processes, and what is their relative importance?
    • 5.9: Glacial Meltwater
      Glacial meltwater is the liquid water produced by ablation of glaciers. Meltwater is in most glaciers by far the most important product of ablation; it’s much more important than evaporation. Of course, in glaciers that terminate in the ocean, calving is more important.
    • 5.10: Glacial Erosion
      Glaciers are very effective in eroding, transporting, and depositing bedrock. How do we know that?
    • 5.11: Glacial Sediment Transport
      The term load is used for all drift that’s in transport by a glacier at a given time. As with fluvial sediment transport, keep in mind the distinction between the load and the transport rate. The transport rate of a glacier is the time rate of passage of sediment past some cross section through the glacier that’s stationary relative to the underlying bedrock.
    • 5.12: Glacial Deposits
      Here are some comments on the nature of sedimentary materials deposited by glaciers: