normal
divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.
They have the same type of force on each fault and the tension is released Whenever the vertical stress (which mostly is because of gravity) is more than horizontal stresses, normal faults can be created or activated.
Far-field stresses triggered by portions of the northern boundary stress the African plate. Intraplate stresses are the driving forces in the South American plate
Compressional Stresses
Compression, tension and shear.
Compressional stresses (reverse or thrust fault) cause a rock to shorten. Tensional stresses (normal fault) cause a rock to elongate, or pull apart. Shear stresses (strike-slip or horizontal fault) causes rocks to slip past each other.
Normal Faults
Tensional forces and compressional forces.
Shearing stress is one of three kinds of stresses. Compressional and tensional are the others. Shearing stress is associated with transform. The other two kinds of plate boundaries are convergent and divergent.
There are three main forces that drive deformation within the Earth. These forces create stress, and they act to change the shape and/or volume of a material. The following diagrams show the three main types of stress: compressional, tensional, and shear. Stress causes the build up of strain, which causes the deformation of rocks and the Earth's crust. Compressional stresses cause a rock to shorten. Tensional stresses cause a rock to elongate, or pull apart. Shearstresses causes rocks to slip past each other.
Frank John Vecchio has written: 'The response of reinforced concrete to in-plane shear and normal stresses'
Holds that a bone grows or remodels in response to the demands placed on it.
divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.
I am not sure if the term is used in cars and vehicles, but in the mechanics of materials, Mohr's circle is a graphical approach for finding solutions of stresses (or strains) of an element when the coordinate axes are rotated by a certain angle. In other words when you want to find the stresses (or strains) on a plane that is inclined to a certain angle from the plane of known stresses. When the technique is used for stresses, you draw a Mohr's circle of stresses and if it is for strains, you get the Mohr's circle of strains. When you work out the algebraic equations that transform known stresses (or strains) at a point to stresses (or strains) in an inclined plane, they result into an equation of a circle on a coordinate system whose horizontal axis is formed by the normal stress (or strain) and the vertical axis is formed by the shear stress (or strain). It is called the Mohr's circle since the technique was first developed by a German engineer called Otto Mohr.
B. M. Sadgrove has written: 'Water retention tests on horizontal joints in thick-walled reinforced concrete structures' 'Water retention tests of horizontal joints in thick-walled reinforced concrete structures' -- subject(s): Reinforced concrete, Strains and stresses, Testing
The plural of "stress" is "stresses."
There are a number of stresses inflicted upon bridges. Some of these stresses include compression, tension, as well as bending.