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哈密盆地北线活动断裂带走向北西西，断续长180km。8条剖面的GPS测量结果显示，断坎坡度为15°～18°及31°～33°．单个断崖高3～10m。由年代学资料计算出该断裂带中全新世垂直活动速率为0．65±0．08mm／a，比晚更新世晚期垂直活动速率有所增大。
The active fault zone along the northern line of the Hami basin extends to the northwest and west, intermittently 180 km long. The GPS surveys of eight sections showed that the slope of the broken ridge was 15 ° ~ 18 ° and 31 ° ~ 33 °. A single cliff high 3 ~ 10m. Based on the geochronology data, the vertical rate of the Holocene activity in this fault zone is 0.65 ± 0.08mm / a, which is higher than that of late Late Pleistocene.