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Surging Glaciers

Outline. What is a surging glacier?Features of surging glaciersMechanisms of movement (two hypothesis)Surging glacier distributionHazards of surging glaciers. What Is a Surging Glacier?. Rapid flow over a short time (active stage) followed by long periods of no movement (quiescent stage)Maximu

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Surging Glaciers

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    1. Surging Glaciers

    2. Outline What is a surging glacier? Features of surging glaciers Mechanisms of movement (two hypothesis) Surging glacier distribution Hazards of surging glaciers

    3. What Is a Surging Glacier? Rapid flow over a short time (active stage) followed by long periods of no movement (quiescent stage) Maximum velocities 10x more than quiescent stage During active stage ice is moved from upper area (reservoir) to the snout (ice-receiving) Active and quiescent cycles usually consistent, but every surging glacier has their own cycle length Amount of ice in accumulation zone affects surging 4% all glaciers are surging glaciers Temporate and cold glaciers both are subject to surge Glaciers of surge type appear to occur mostly on sedimentary rocks

    4. Features of a Surging Glacier Heavy crevassing Ice velocities increase and fluctuate Transfer of large volumes of ice The snout may advance (few kms in few months) Large amounts of melt water released Thrusting in the ice occurs at the surge front

    5. Ice structures formed during quiescent phases are deformed

    6. Mechanisms of Movement Rigid Bed Hypothesis Glacier lies on rigid bed of rock Water drains at base through tunnels and drains to the snout The tunnels eventually closes/collapse trapping water and building pressure Basal sliding increases and friction is less Glacier separates from its bed and cavities begin to join Joining cavities results in water discharges easily and surge stops

    7. Variegated Glacier 1982-83

    8. Deformable Bed Hypothesis Ice resting on soft unconsolidated cement Drainage through permeable sediments under the ice Permeability is reduced and ice thickens Pressure builds up and glacier begins to flow Sediments return to permeable and surging ends

    9. Trapridge Glacier

    10. Surging Glacier Distribution St Elias mountains, Alaska range, the Wrangell mountains

    11. Surging Glacier Distribution Andes, Iceland, Greenland, USSR

    12. Hazards Hubbard glacier 150km long, southern Alaska Advanced at rates of 10m/day

    13. Moved across water at mouth of Russell fiord Reached far side of mountain wall of fiord in two months, creating a lake 50kms long out of the fiord Many of the marine mammals became trapped Attempt to carry mammals around the ice barrier but many were left The lake began to rise driving birds from their nests and destroyed eggs Town of Yakutat and airport now threatened Lake broke through the ice dam (October 8, 1986)

    14. THE END QUESTIONS?

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