A chonolith is an igneous rock intrusion of irregular shape. A chonolith has a demonstrable base, which is absent in other types of irregularly shaped intrusions (batholiths, stocks and bosses).
Examples are:
the Spring Gulch chonolith composed of aplite, in Elko County in Nevada, USA.
the Nebo-Babel chonolith of gabbronorite in the West Musgrave area of Western Australia.
chonoliths in Norilsk, Russia.
a chonolith of dacite of Pleistocene age in Chinkuashih, Taiwan.
a chonolith of Cretaceous age in the Cortez Mountains, near Carlin in Nevada, USA.
a chonolith of andesite near Shavano in Colorado, USA.