A concept map connecting deflation, dust storms, saltation, dunes, and loess would illustrate the process of deflation, where wind erodes surface materials, leading to dust storms. Dust storms transport particles via saltation, which is the bouncing of smaller grains along the ground. As these particles accumulate, they can form dunes, while finer materials can settle and form loess deposits. Together, these elements highlight the dynamic interactions in arid and semi-arid environments.
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