This answer shows that the close orbital period around a spherical body of uniform density is
$$T = \sqrt{\frac{3 \pi}{G\rho}}$$
and so the orbit's period $T$ is defined only by the body's density $\rho$, not its size. It takes about 90 minutes to orbit the Earth in a low orbit, and it would likewise take 90 minutes for an atom to orbit a spherical speck of dust with a similar average density to that of Earth. (uncharged, unpolarizable dust, ignoring other forces e.g. Coulomb, Van der Waals, Casimir, etc.)
Let's compare cliffs on a spherical planet, small asteroid, and piece of dust. Assume the height of each cliff divided by the radius of the object is the same, and call the fraction
$$f = \frac{h}{R}.$$
So if $f=$ 1%, then that's 64 km on Earth, 64 m on a 1 km radius asteroid, and 10 microns on a 1 mm radius piece of dust.
The fall time is
$$t=\sqrt{\frac{2h}{a}} = \sqrt{\frac{2fR}{a}}$$
where $a$ is the gravitational acceleration, keeping it simple by assuming it's constant though it changes slightly as we fall from such a great height.
$$a = \frac{GM}{R^2}$$
$$M = \frac{4}{3} \pi \rho R^3$$
$$a = \frac{4}{3} \pi G \rho R$$
So
$$t = \sqrt{\frac{3f}{2\pi G \rho}}$$
For spherical bodies of the same density with cliffs of heights as a fixed fraction of radius, the time it takes to fall down the cliff is independent of the size of the body, and varies as the inverse square root of the density of the body.
For a $0.01 R$ cliff on a body of density 5.51 g/cm^3 (Earth's average density) that works out to 114 seconds, or about 2 minutes, and compares to 5063 seconds or 84 minutes for an orbit that skims the surface.