| 41. | A number of high-angle normal faults accommodating tilting and extension within the hanging wall are easily visible as well.
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| 42. | Finally, during the Late Cenozoic tectonic uplift took place as a result of movement on high angle normal faults.
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| 43. | Thrust faults are generated by the highest, strike slip by intermediate, and normal faults by the lowest stress levels.
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| 44. | The Woodlark Basin is one of very few places on the earth to have active low angle normal faults.
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| 45. | These rifts are the result of the actions of numerous normal faults which are typical of all tectonic rift zones.
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| 46. | This would make a normal fault look like it was a low angle normal fault that is no longer active.
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| 47. | The Tongwynlais Fault is a normal fault and affects both the Carboniferous Limestone and underlying Devonian Upper Old Red Sandstone.
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| 48. | This would make a normal fault look like it was a low angle normal fault that is no longer active.
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| 49. | The long intervals between large earthquakes on the fault are consistent with other normal faults in the Intermountain Seismic Belt.
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| 50. | Finding the key bed in these situations may help determine whether the fault is a normal fault or a thrust fault.
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