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The thickness varies from a high of 60 kilometers in the farside highlands to a low near zero within impact basins.

In some of the basins, the crust really may have zero thickness, meaning that mantle material is exposed at the surface.

Here is a lovely view from Lunar Reconnaissance Orbiter.

These include Crisium on the nearside (the rightmost of the three northern round basins) and Moscoviense on the farside (just northwest of the center of the globe), as well as a couple of small craters within the south pole-Aitken basin on the farside.

Purple stars denote locations where the Kaguya orbiter saw olivine, a mantle mineral, exposed at the surface.

Basins have thin crust (blue and green), and are often rimmed by thick crust (red and orange).

This map of lunar crustal thickness was derived from an analysis of GRAIL's gravity data.