Final answer:
Mercury's tall cliffs are due to the global compression of its crust after cooling and contracting, which is different from the Moon's geological history.
Step-by-step explanation:
The tall cliffs on Mercury, also known as scarps, are a result of the planet's unique geological history. Unlike the Moon, Mercury has a very large metal core and, as a result, experienced significant cooling and contraction after its formation. This cooling caused Mercury's crust to crack and form the tall cliffs that can be seen intersecting its craters.
These long, curved cliffs on Mercury's surface testify that global compression of Mercury's crust occurred after most of the craters had already been formed. Therefore, the presence of many tall cliffs on Mercury compared to the Moon can be attributed to the planet shrinking and wrinkling its crust during its past.