normal
Normal faulting results from expansive stresses, where the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of faulting is common at divergent plate boundaries where new crust is being formed.
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
Basically, if we cut away the earth to look at the strata (the rock layers), they form an "S" shape (forwards or backwards). Use the link and check out a drawing. You'll have to scroll down to figure 101-7 to see it. The picture says it all.
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
Normal faulting results from expansive stresses, where the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of faulting is common at divergent plate boundaries where new crust is being formed.
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.
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.
Frank John Vecchio has written: 'The response of reinforced concrete to in-plane shear and normal stresses'
In a normal fault, the crust moves along a downward sloping fault plane, with the hanging wall moving down relative to the footwall. This movement is caused by tensional stresses pulling the crust apart.
Holds that a bone grows or remodels in response to the demands placed on it.
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.