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Mass screening is based on all of the following except:
Glaciers
Large masses of ice on land that move slowly over time, formed by the accumulation and compaction of snow, significantly influencing landscapes through erosion and deposition.
Glaciers
Large, slow-moving masses of ice formed from compacted layers of snow, which move under their weight and shape the land beneath.
Cirque
A bowl-shaped, steep-walled mountain basin carved by glaciation, often containing a small lake.
Continental Ice Sheet
A large mass of ice covering extensive parts of continents and flowing outward from central, thicker areas, altering landscapes through erosion and deposition.
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