The statement that is not true of a batholith is:
"It is often a small part of a sill."
A batholith is a large mass of intrusive igneous rock that solidified from magma deep in the Earth's crust, and it is typically much larger than a sill, which is a smaller, sheet-like intrusion of igneous rock that has spread between layers of sedimentary rock. Batholiths are generally not considered to be parts of sills, as they represent a different scale and form of igneous intrusion.