Previous study found that blowouts will evolve into wind-accumulated landform, such as parabolic dunes or linear dunes. However, blowout in this area can evolve into other types of wind eroded landforms.

  • 前人的研究发现风蚀坑多发展为风沙堆积地貌,例如抛物线型沙丘或线性沙丘,而本区风蚀坑则可发展为其他类型的风蚀地貌。

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