Free-Fall Time Calculator

Calculate the free-fall time of a uniform-density sphere via t_ff = √(3π/32Gρ), from either a mass density or a molecular-cloud number density, with the exact collapse trajectory and a comparison scale against real cloud, planet, and stellar densities.

Free-fall time calculator

How long a uniform-density sphere of gas would take to collapse to a point under its own gravity alone, with nothing — pressure, rotation, magnetic fields — holding it up: tff=3π32Gρt_{\rm ff} = \sqrt{\dfrac{3\pi}{32 G \rho}}. Widely used in star formation as the natural collapse timescale for a molecular cloud or clump, to compare against how long star formation actually takes there.

tfft_{\rm ff}3.3929 Myr
ρ\rho = 3.8492 × 10⁻¹⁹ kg/m³ = 3.8492 × 10⁻²² g/cm³
Milliseconds1.0707 × 10¹⁷ ms
Seconds1.0707 × 10¹⁴ s
Minutes1.7845 × 10¹² min
Hours2.9742 × 10¹⁰ hr
Days1.2393 × 10⁹ day
Years3.3929 × 10⁶ yr
Thousand years3392.89 kyr
Million years3.3929 Myr
Billion years0.003393 Gyr
00.84821.72.543.39elapsed time (Myr)0%25%50%75%100%radius (% of r₀)84% of r₀ left at 50% of t_ff

The exact collapse trajectory of a uniform sphere's outer edge, normalized to its own r₀ and t_ff — the same shape for every density. Collapse starts slowly and plunges only right at the end: half of the total free-fall time passes before the radius has shrunk by even a sixth.

10³ s10 s10 s10 s10 s10 s10 s10¹⁰ s10¹¹ s10¹² s10¹³ s10¹⁴ sDiffuse molecular cloudTypical GMC clumpDense prestellar coreThe Sun's mean densityEarth's mean densitythis density

Log scale — free-fall time spans upward of ten orders of magnitude across these presets alone, from a rocky planet's density (minutes) to a diffuse molecular cloud's (millions of years).

Leave a cloud of gas with nothing holding it up — no pressure, no rotation, no magnetic field, nothing but its own gravity — and it collapses to a point in a finite, calculable time. That number, the free-fall time, is one of the most-used timescales in star formation: it’s the natural clock against which every slowing-down mechanism (turbulence, magnetic support, rotation, radiative feedback) gets measured, and it sets the baseline question “is this cloud collapsing about as fast as gravity alone would allow, or is something holding it back?”

The formula

tff=3π32Gρt_{\rm ff} = \sqrt{\frac{3\pi}{32 G \rho}}

ρ\rho is the sphere’s (uniform) mass density and GG is the gravitational constant. Only density enters — not size, not mass on its own — because for a uniform sphere, size and mass cancel out of the collapse time exactly: a denser cloud always collapses faster than a puffier one, regardless of how big or how massive either actually is.

Two ways to specify density

Molecular clouds are almost always quoted as a number density of particles per cubic centimeter, not a mass density, so this calculator accepts either:

Reading the visuals

What this does and doesn’t capture

A real molecular cloud isn’t uniform, isn’t spherical, and isn’t pressure-free — it has internal structure, turbulence, magnetic fields, and (usually) at least some thermal or non-thermal support against gravity. A cloud with a nonuniform density collapses hierarchically — denser clumps inside it reach their own, shorter, local free-fall time and collapse first, well before the cloud’s overall average density would suggest — so tfft_{\rm ff} computed from an average density is best read as an order-of-magnitude reference clock, not a precise prediction for any one particular clump. Comparing a cloud’s actual star-formation timescale to this reference clock is exactly how astronomers quantify how much something besides gravity must be holding star formation back.

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Changelog

  • 2026-09-06Published.