Frozen Lakes (Chapter 3): Chasing Patterns №2 – Norway Iceland and mineral content in constant

and mineral content in constant interaction

Icelandic glaciers showcase a distinctive structure characterized by crevasses

with small icebergs still floating around

The images explore how shifting light brings out textures and patterns in the sand

Frozen Lakes (Chapter 3): Chasing Patterns №2 – Norway Iceland and mineral content in constantArtwork 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