A 10.0 kg stone slides down a snow-covered hill (the figure (Figure 1)), leaving point A with a speed of 11.0 m/s. There is no friction on the hill between points A and B, but there is friction on the level ground at the bottom of the hill, between B and the wall. After entering the rough horizontal region, the stone travels 100 m and then runs into a very long, light spring with force constant 2.40 N/m. The coefficients of kinetic and static friction between the stone and the horizontal ground are 0.20 and 0.80, respectively.
A 10.0 kg stone slides down a snow-covered hill (the figure (Figure 1)), leaving point A with a speed of 11.0 m/s. There is no friction on the hill between points A and B, but there is friction on the level ground at the bottom of the hill, between B and the wall. After entering the rough horizontal region, the stone travels 100 m and then runs into a very long, light spring with force constant 2.40 N/m. The coefficients of kinetic and static friction between the stone and the horizontal ground are 0.20 and 0.80, respectively.
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M6
Transcribed Image Text:A 10.0 kg stone slides down a snow-covered hill (the
figure (Figure 1)), leaving point A with a speed of 11.0
m/s. There is no friction on the hill between points A
and B, but there is friction on the level ground at the
bottom of the hill, between B and the wall. After entering
the rough horizontal region, the stone travels 100 m and
then runs into a very long, light spring with force constant
2.40 N/m. The coefficients of kinetic and static friction
between the stone and the horizontal ground are 0.20
and 0.80, respectively.
Figure
A
20 m
15 m
B
Rough
< 1 of 1
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