Apollo hammer drop
On the Moon with g = 1.62 m/s², David Scott’s hammer and feather hit the dust together after ~3 s—air resistance is the only reason they don’t on Earth.
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Free fall describes vertical motion under a constant gravitational acceleration g with no air resistance. In this idealized model, the only force acting on the object is gravity, so its vertical position follows a simple quadratic curve in time. This calculator focuses on three classroom staples—time to hit the ground, impact velocity, and kinetic energy—and lets you explore different worlds using presets for Earth, Moon, Mars, and Jupiter.
We measure height from the ground upward and take upward as the positive direction. With initial height h0 (meters), initial vertical velocity v0 (m/s), and gravity magnitude g (m/s²) acting downward, the height at time t seconds is y(t) = h0 + v0 t − (g/2) t². The time to impact is the non-negative solution of y(t)=0:
thit = ( v0 + √( v02 + 2 g h0 ) ) / g.
The impact velocity (signed, upward positive) is vimpact = v0 − g thit, and the impact speed is |vimpact|. Kinetic energy on impact is KE = ½ m |vimpact|²; if mass is not provided, the calculator reports KE per kilogram (J/kg), which equals ½ |v|².
Only g changes. On the Moon (≈1.62 m/s²), falls are slower and impact speeds are lower for the same height. On Mars (≈3.71 m/s²) they are in between Earth (≈9.80665 m/s²) and the Moon. Jupiter’s strong gravity (≈24.79 m/s²) produces much shorter fall times and higher impact speeds. Use the presets to compare how g reshapes the height–time curve and your results.
Drop (no initial push) from h0=10 m on Earth (g=9.80665). Then thit = √(2h/g) ≈ √(20/9.80665) ≈ 1.43 s. Impact speed is |v| ≈ g·t ≈ 9.80665 × 1.43 ≈ 14.0 m/s. If the mass is 2 kg, the kinetic energy at impact is ½·2·14.0² ≈ 196 J. Changing only g to the Moon stretches the time to ≈3.5 s and lowers the speed to ≈5.7 m/s.
Acceleration due to gravity is (approximately) constant near a planet’s surface. Integrating constant acceleration gives a linear velocity change in time and a quadratic position curve. That’s why the height–time graph is a downward-opening parabola whose curvature increases with larger g.
Tip: Use a small positive v0 to model tossing an object upward before it falls. The calculator automatically includes the up-and-down portion in the total time to impact.
On the Moon with g = 1.62 m/s², David Scott’s hammer and feather hit the dust together after ~3 s—air resistance is the only reason they don’t on Earth.
Drop from 180 m on Earth and you’ll fall for roughly 6 s, reaching ~77 m/s—long enough to recite Newton’s apple story twice.
Jupiter’s 24.79 m/s² gravity means a 10 m drop takes only 0.9 s, but impact speed rockets to ~22 m/s—double Earth’s energy per kilogram.
Give an object an upward toss (say +5 m/s) and total time grows: it “pauses” at the apex before the calculator’s quadratic brings it back to Earth.
Leaving mass blank shows KE per kg = ½ v² — useful when you just want the punch of the impact without choosing an object.