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 This would make a normal fault look like it was a low angle normal fault that is no longer active. 47.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 This would make a normal fault look like it was a low angle normal fault that is no longer active. 49.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