Facets are angular crystals formed under which condition?

Prepare for the Avalanche (Avi) Exam. Study with flashcards and multiple choice questions, each with hints and explanations. Get ready for your test!

Multiple Choice

Facets are angular crystals formed under which condition?

Explanation:
Facets form when there is a strong temperature gradient within the snowpack. A large temperature difference between the surface and deeper layers drives water vapor to migrate through the snow: vapor sublimates from warmer areas and deposits on colder surfaces. This rapid, diffusion-driven metamorphism reshapes grains by removing mass from their edges and adding it to their faces, producing angular, flat-faced crystals—the faceted grains. This process is known as kinetic growth metamorphism and it creates a weak, fracture-prone layer that is important in avalanche behavior. The other descriptions don’t capture this specific metamorphic process. Round crystals result from slow, low-gradient metamorphism where grains tend to smooth out and round; dense packing relates to how tightly packed the snow is rather than crystal shape; large snow grains describe size growth that doesn’t necessarily produce the angular facets formed by a strong temperature gradient.

Facets form when there is a strong temperature gradient within the snowpack. A large temperature difference between the surface and deeper layers drives water vapor to migrate through the snow: vapor sublimates from warmer areas and deposits on colder surfaces. This rapid, diffusion-driven metamorphism reshapes grains by removing mass from their edges and adding it to their faces, producing angular, flat-faced crystals—the faceted grains. This process is known as kinetic growth metamorphism and it creates a weak, fracture-prone layer that is important in avalanche behavior.

The other descriptions don’t capture this specific metamorphic process. Round crystals result from slow, low-gradient metamorphism where grains tend to smooth out and round; dense packing relates to how tightly packed the snow is rather than crystal shape; large snow grains describe size growth that doesn’t necessarily produce the angular facets formed by a strong temperature gradient.

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