Quick clay is a type of soil that is particularly unstable and can behave like a liquid when it is disturbed. It is primarily composed of fine-grained particles, including clay minerals, and is often found in glaciated regions, especially in areas where sediment has been deposited by glaciers. The unique characteristic of quick clay arises from its structure; it typically has a high water content and when subjected to stress, such as vibration or disturbance, it can lose its strength and become flow-like.
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