Yes, that's possible.
the non fundamental forces are Tension,Torque,Elastic,Normal,Gravity,Friction.
what is elastic and inelastic collision what is elastic and inelastic collision what is elastic and inelastic collision
the elastic is medium
since freezing elastic object decreases its elastic limits, increasing temperature would increase elastic limits.
Normal, Friction, Tension, and Elastic Forces.
the non fundamental forces are Tension,Torque,Elastic,Normal,Gravity,Friction.
Elastic
the non fundamental forces are Tension,Torque,Elastic,Normal,Gravity,Friction.
Yes, that's possible.
the non fundamental forces are Tension,Torque,Elastic,Normal,Gravity,Friction.
the force's involved are gavitational,normal,elastic and friction because then you sit on the horse gravity is keeping you up
The height of the bounce decreases because of many factors but two main factors are gravity and friction. * * * * * Gravity has nothing to do with the decrease in height. The two main factors are friction and the fact that the collision is not elastic.
The mechanism for stress to be released from friction along a fault is known as elastic rebound. Vibrations occur when rocks elastically return to their original shape causing damage from the seismic waves being sent out.
elastic
suffix for elastic
At a slip fault the plates on either side of the fault are under a force that impels them to move past each other, but restrained by friction and the interlocking of their shapes. These opposing forces distort the rocks of the plate edges near the fault, producing elastic deformation. When the strain becomes great enough to overcome static friction or to break the interlocking sections of rock, or when any shock occurs that jars the fault and allows it to start moving, the friction between the plates will be reduced to dynamic friction (for so long as the plates keep moving). Then elastic forces in the distorted rocks will cause them to spring suddenly back to their proper shapes, producing movement of the rocks either side of the fault, parallel to the fault, of sometimes several metres. This sideways movement releases a great deal of elastic potential energy, producing the S-waves of an earthquake. Elastic rebound caused a problem for seismologists monitoring underground nuclear tests before the Comprehensivve Test Ban Treaty came into effect. An explosion itself produces only P-waves, which ought to have allowed seismologist to tell underground explosions apart from earthquakes. But in practice the P-waves from the explosions could jar elastically-deformed faults into movement, which produced S-waves from the elastic rebound.