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Rock Glaciers : Study

Rock Glaciers : Study

A new study revealed that over 100 active permafrost structures identified in the Jhelum basin, can cause catastrophic disasters in future.

  • A rock glacier is a mass of rock, ice, snow, mud, and water that moves slowly down a mountain under the influence of gravity.
  • Unlike an ice glacier, rock glaciers usually have very little ice visible at the surface.
  • The rock glacier might consist of a mass of ice covered by rock debris, or it might consist of a mass of rock with interstitial ice.
  • Rock glaciers typically form in mountainous regions where there is a combination of permafrost, rock debris, and ice.
  • One common scenario involves a pre-existing glacier that accumulates debris and rocks as it moves.
  • Over time, if the glacier recedes or thaws, the debris-covered ice can transform into a rock glacier.
  • These are classified as ‘active’ or ‘relict’ to indicate the status of permafrost within them, identified by the appearance of the rock surfaces.
  • It increases the risk of glacial lake outburst floods (GLOFs).
  • It may also make landslides more frequent with the land on the melting ice becoming loose.