Pancake ice consists of approximately disk-shaped young ice floes, often with raised edges formed by collisions. Wave-driven collisions and motion in the surrounding frazil ice can dissipate energy.
Consolidated pancake ice forms when pancake ice packs, rafts and freezes together with interstitial frazil ice. Its heterogeneous granular structure can retain stacked layers and acquire later columnar basal growth.
// Target: geophysics.bigb
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Pancake ice refers to a type of ice formation found on the surface of water bodies, typically in cold regions. It consists of rounded, flat pieces of ice that resemble pancakes, hence the name. This phenomenon usually occurs in the early stages of ice formation, where ice crystals break and then re-freeze into these disc-like shapes as wind and water movement cause them to bump into each other.