0
Because of friction and the rigidity of the rock, the rocks cannot glide or flow past each other. Rather, stress builds up in rocks and when it reaches a level that exceeds the strain threshold, the accumulated potential energy is dissipated by the release of strain, which is focused into a plane along which relative motion is accommodated-the fault.
What else can I help you with?
What happens when pressure builds up along a fault?
When pressure builds up along a fault, it can result in an earthquake as the stored energy is released through sudden movement along the fault line. This movement can cause the rocks on either side of the fault to slip, producing seismic waves that we feel as shaking on the Earth's surface.
What happens when enough stress builds up in a brittle rock the rock breaks caused a what to form?
Reverse fault
What happens when friction between opposute sides of a fault is high?
High friction between opposite sides of a fault can cause stress to build up, leading to a potential earthquake when that stress is released suddenly as the fault slips. This can result in intense shaking and ground displacement along the fault line.
Which is not an example of potential energy a ball traveling at 10ms a compressed spring or stress along a fault line?
stress along a fault line stress along a fault line
Does stress build in areas where rock along fault lines snag and remain locked?
Yes, stress can build up along fault lines where rocks snag and remain locked. This stress can accumulate over time until it is released in the form of an earthquake when the built-up energy exceeds the strength of the rocks holding the fault together.
What builds up in fault zones when crustal blocks stick together?
Stress
What happens when friction on opposite side of a fault is high?
High friction on opposite sides of a fault can cause stress to build up in the rocks. When the stress exceeds the strength of the rocks, it can result in an earthquake as the rocks suddenly shift along the fault line.
When enough stress builds up in brittle rock the rock breaks causing a what to form?
When enough stress builds up in brittle rock, it breaks and causes a fault to form. A fault is a fracture or zone of fractures in the Earth's crust where there has been displacement of the rock on either side. This process is often associated with tectonic activity, such as earthquakes. The breakage and movement along the fault can lead to significant geological changes in the surrounding area.
Describe what happens along a fault beneath earths surace when an earthquake occurs?
When an earthquake occurs, stress along a fault builds up until it exceeds the strength of the rocks. This causes the rocks to break and move relative to each other, releasing stored energy in the form of seismic waves that cause the ground to shake. The movement along the fault can be vertical, horizontal, or a combination of both, depending on the type of fault.
What often occurs along faults or breaks in earths crust where movements occur?
Earthquakes often occur along faults or breaks in Earth's crust where movements occur. These movements happen when stress builds up along the fault and is released suddenly, causing the rocks to break and generate seismic waves. Earthquakes can range in intensity depending on the magnitude of the movement along the fault.
As plates move what happens when pressure builds up and then rocks break?
When pressure builds up along a fault line, eventually the rocks will break along that fault, causing an earthquake. The sudden release of built-up pressure sends seismic waves that shake the ground, causing the movement we feel during an earthquake.
What happens to rocks along a fault line?
Rocks along a fault line can break and shift due to tectonic forces, causing movements such as sliding past each other or being compressed together. The friction and pressure along the fault line can lead to earthquakes when the accumulated stress is released suddenly. Over time, the rocks along a fault line can also undergo deformation, such as folding and faulting.
