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laccolith
This term is a specialized geological descriptor used primarily in academic, technical, and professional contexts. It describes a specific structural geometry of igneous intrusion, distinguishing it from sills, which are flat, or batholiths, which are much larger and more irregular. The term carries a neutral, descriptive tone and is rarely encountered outside of earth sciences.
Because it refers to a specific geological feature, it is treated as a standard countable noun. Geologists may refer to a single laccolith or multiple laccoliths within a regional volcanic province.