In the crust, within a few kilometers of the surface
A body of rock affected by tensile stress will likely undergo stretching. This happens during the asymmetric deformation of a rock mass.
This depends on the confining pressure, the temperature and the strain rate applied to the rock mass. In general, the lower the rate of strain, the more likely ductile or plastic deformation leading to bending or folding will occur. The higher the strain rate, the more likely brittle deformation is to occur, leading to the rock "breaking". As the confining pressure increases, a materials shear strength will increase (this usually coincides with a greater depth of burial) and due to the Earth's thermal gradient an increase in temperature. As the shear strength of the rock increases, the occurrence of brittle failure is less likely while the higher temperature means that plastic deformations are more likely to occur.
No, they're more likely to fault. Ductile rocks are more likely to fold.
Evaporation
There are two reasons. First, faulting is a form of brittle failure, which generally occurs at lower temperatures. Deep in the crust, where it is very hot, rocks tend to undergo ductile failure, deforming like taffy. Additionally, most materials resist breaking at higher overall pressure.
Igneous rock
A body of rock affected by tensile stress will likely undergo stretching. This happens during the asymmetric deformation of a rock mass.
This depends on the confining pressure, the temperature and the strain rate applied to the mineral. In general for minerals (and other materials), the lower the rate of strain, the more likely ductile or plastic creep deformation will occur. The higher the strain rate, the more likely brittle deformation is to occur. As the confining pressure increases, an objects shear strength will increase (this usually coincides with a greater depth of burial) and due to the earth's thermal gradient an increase in temperature. As the shear strength increases, brittle failure is less likely and the higher temperature means that plastic deformations or creep are more likely to occur.
This depends on the confining pressure, the temperature and the strain rate applied to the rock mass. In general, the lower the rate of strain, the more likely ductile or plastic deformation leading to bending or folding will occur. The higher the strain rate, the more likely brittle deformation is to occur, leading to the rock "breaking". As the confining pressure increases, a materials shear strength will increase (this usually coincides with a greater depth of burial) and due to the Earth's thermal gradient an increase in temperature. As the shear strength of the rock increases, the occurrence of brittle failure is less likely while the higher temperature means that plastic deformations are more likely to occur.
Hydrogen is the element that is most likely to undergo nuclear fusion.
becomes more likely
becomes more likely
Extinction
No, they're more likely to fault. Ductile rocks are more likely to fold.
Shortening
If there was a mistake during mitosis the results would most likely be a genetic deformation but it all depends on the type of cell it is.
I believe the word you are searching for is Reactivity?