Transform faults also act as the plane of weakness allowing for the splitting in rift zones.
2.
This creates a horizontal plane of weakness called a " cold joint " between the two batches.
3.
Others have compound structure, in which large units are composed of smaller units separated by persistent planes of weakness.
4.
Because foliation planes are planes of weakness, these dipping towards a free surface, failure is likely to occur along these planes.
5.
Rapid shearing can then occur along these planes of weakness, giving rise to an earthquake in a mechanism similar to a shallow-focus earthquake.
6.
They tend to be larger than shallow landslides and form along a plane of weakness such as a scarps at the top and steep areas at the toe.
7.
The meristem itself is the least calcified portion; sometimes there is no mineralization at all, which makes it a plane of weakness where breaking often occurs.
8.
There are often oblique pre-existing faults, planes of weaknesses or striations to the fault slip, which do not belong to the conjugate fault sets.
9.
Additional benches on the margin of Whitman Bench are due to deep-seated slumping of large blocks, which also creates planes of weakness for future slippage and channels for water infiltration.
10.
Rock slides are the most dangerous form of mass-wasting due to the fact that they incorporate a sudden, incredibly fast-paced release of bedrock along a uniform plane of weakness.
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