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If you sit on a rock with a downward force of 'W' pounds, then the rock exerts an upward force of 'W' pounds on your derriere. We know that the sum of the forces on the seat of your pants must be zero. Otherwise the pants would be accelerating, either up or down.
No. Any object that was shot by gun, flung by slingshot, or thrown by hand, begins accelerating downward at the acceleration of gravity as soon as it leaves the propulsion system. Zero velocity is true at the top, but acceleration is constant throughout the trajectory ... 9.8 m/s downward.
The displacement and velocity of a rock that is dropped from rest after 4s, is 6 km/h. This can vary depending on the speed of the rock, and the surroundings.
39 m\s downward
"Weight" is the force exerted by gravity. Thus, 50 Newtons.
If you sit on a rock with a downward force of 'W' pounds, then the rock exerts an upward force of 'W' pounds on your derriere. We know that the sum of the forces on the seat of your pants must be zero. Otherwise the pants would be accelerating, either up or down.
the process that describes downward sliding of the rock material is Slump
A syncline is comprised of downward folding layers of rock.
fallen rock
my but
syncline
Sycline
A normal fault is the result of the downward movement of rock along the fault line.
Ultimately gravity.A2. In a scree or talus, the rocks will fall to eventually come to rest. The driving force is gravity.In a stream, they will be borne easily in steeper streams but in a stream of shallow angle, their movement will be slight. Indeed their only movement may be in a flood. The material will become more worn down as it proceeds downstream. But the force moving the water is still gravity.
No. Any object that was shot by gun, flung by slingshot, or thrown by hand, begins accelerating downward at the acceleration of gravity as soon as it leaves the propulsion system. Zero velocity is true at the top, but acceleration is constant throughout the trajectory ... 9.8 m/s downward.
a normal fault
Deltas are the repositories of eroded rock at the end of rivers. Because the amount of deposited material continues to grow, the sediments are pushed downward from their sheer weight and will eventually lithify or turn to sedimentary rock.