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and seasonal flooding
mist and low-hanging clouds blend with the waterfall’s spray
Icelandic glaciers showcase a distinctive structure characterized by crevasses
and mineral content in constant interaction
glacial landscape
Frozen Lakes (Chapter 3): Chasing Patterns №2 – Norway Iceland and seasonal floodingArtwork Information The formation of holes and cracks on frozen lakes is a result of a variety of factors, including temperature changes, wind, water currents, and the physical characteristics of the ice itself. Norway's cold climate and fluctuating temperatures make its frozen lakes particularly susceptible to cracking and breaking. Strong winds and water currents can also create stress on the ice, leading to cracks and the formation of ridges. The
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