Glacial Dams
Glacial Ice Dams Glaciers move consistently. The rate and manner in which they change depend on the elements and surrounding environment. In the warmer summer months, glaciers melt more quickly and have a shorter time period for reforming. Many of the features we observe in the summer are effects of gravity, force, and elemental shifts. During the winter, glaciers move much slower and have more time to accumulate than melt. As we observe the melting and forming stages of glacier ice, we can simultaneously explore some of the unique features created during these transition periods. What are Glacial Dams? In simplicity, glacial dams can be characterized as ice blockages in meltwater. These floating ice formations flow along with the meltwater and gravity until reaching land features that cannot be easily moved through or around. This is where we see glacial dams start to have more nuanced features that accumulate into [...]













