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The relationship between low mountain ranges and high mountain ranges can be best described in terms of geological processes and erosion. Low mountain ranges often represent older, more eroded formations, while high mountain ranges are typically younger and more tectonically active, reflecting ongoing geological uplift. Additionally, the interplay of weathering and erosion can shape their features, influencing biodiversity and climate patterns in each range. Understanding these dynamics provides insights into the Earth's geological history and landscape evolution.

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