| 1. | Such cuestas may be either erosional escarpments or fault scarps .
这类单面山既可以是侵蚀山崖也可以是断层崖。 |
| 2. | Where the fault scarp is less prominent, the environments on the two sides may be almost the same .
在断崖不明显的地方，两边的环境可能总是相同的。 |
| 3. | A major vertical fault scarp formed during the earthquake was less than 1000 ft from the spillway .
地震时形成的一个主要的垂直断层崖，离溢洪道不到1000英尺。 |
| 4. | Rejuvenated fault scarp
更生断层崖 |
| 5. | Consequent fault scarp
顺向断层崖 |
| 6. | Composite fault scarp
复成断层崖 |
| 7. | Revived fault scarp
复活断层崖 |
| 8. | It is feasible to infer the specific shape of a fault scarp with the help of its average diffusion age and origin time of the scarp
无论是单一型断层崖还是复合型断层崖，通过断层崖的平均扩散年龄和初始错断时间，就能推断出它在某一时刻的具体形态。 |
| 9. | Tian shan extends east - west in central asia , the tian shan range was formed in later paleozoic , and a few intramontan basins appeared in mesozoic . it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision , so many active structures can be found in tian shan . active tectonics took actions during last ten thousands yeas , and surface traces of fault scarps , detached gullies and folds in alluvial deposit are apparent , so it is easy to distinguish them from other geological phenomema
天山位于亚洲中部，天山造山带形成于晚古生代，到中生代时，在天山内部形成了一些山间盆地，印度板块在始新世向北与欧亚板块碰撞，天山受南北向挤压力的作用再度于早中新世隆起，由于板块碰撞的持续进行，在天山山间及山前发育了许多的活动构造。 |
