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The rounded tops of mountains in the Northeast are primarily the result of erosion, which has worn down sharper peaks over time, creating smoother, rounded summits. The region's geology, shaped by glacial activity, often leads to thin, rocky soil as glaciers scoured the landscape, transporting and depositing materials. This combination of erosion and glacial processes results in the rough, rocky, and often thin soil found in many areas. Additionally, the climate and vegetation types in the Northeast contribute to soil degradation and limited soil depth.

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1w ago

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