Figure G-1
Pretend an object is set sliding on a huge frictionless plane in contact with the surface
of Earth as shown. Once the object is set in motion it will
1) theoretically slide to the right forever
2) slide back and forth
3) slow down and stop
because
4) of its inertia.
5) gravitational force decreases with increasing distance.
6) the object is sliding “uphill” and then “downhill” relative to the round Earth.
When the bottom string is pulled slowly in the heavy-ball-and-strings demonstration
(Figure 4.8 in your book), tension
A) in the top string is due to your pull plus the weight of the ball.
B) is about the same in both strings.
C) in the bottom string is zero.