A high force foot strike will be 8-10 g's, while a more a low force foot strike will measure 4-6 g's. Source: http://www.udel.edu/PR/UDaily/2007/may/stress050107.html
Approximately 1-1.5 times your body weight is generated on each foot strike while walking barefoot. This force helps to stimulate the muscles, bones, and connective tissues in the feet, contributing to their strength and resilience. It's essential to develop good foot strength and proper walking mechanics to manage and distribute this force effectively.
The type of stress force that produces a strike-slip fault is transform stress. This stress occurs when two tectonic plates slide past each other horizontally, causing displacement along a fault line. Strike-slip faults are often associated with transform plate boundaries, such as the San Andreas Fault in California.
Friction is a force that is generated when two surfaces rub against each other. It is useful for preventing slipping or sliding.
The distance would depend upon the force of each individual strike.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
The action force of walking is the force exerted by the foot pushing against the ground to propel the body forward. This force is equal in magnitude and opposite in direction to the reaction force exerted by the ground pushing back against the foot, allowing us to move forward with each step.
How much what is generated each year
strike-slip
A force is needed to start something moving and to stop it once it is moving. A force can make something speed up or slow down. Friction is a force generated when surfaces move across each other.
Electrostatic force is created by the attraction or repulsion of electrically charged particles. This force arises from the interaction between the electric fields generated by these charged particles. Like charges repel each other, while opposite charges attract each other, leading to the creation of electrostatic force.
A strike-slip fault has a shearing force, where the two blocks on either side of the fault move horizontally past each other. This type of fault is characterized by lateral movement along the fault line caused by horizontal forces.
When two objects grind past each other, the force generated is called friction. Friction opposes the motion between the two surfaces and is influenced by factors such as the materials involved, their roughness, and the normal force pressing them together.