IPA: /ˈpɪsəˌlaɪθ/
KK: /ˈpɪsəˌlaɪθ/
A small, round mass formed from layers of material, typically calcium carbonate, that is larger and less regular than a type of sediment called oolite.
The geologist discovered a pisolith while examining the sediment layers.
Pisolith → It is formed from "piso" (from Greek "pison", meaning pea) and "-lith" (from Greek "lithos", meaning stone). The word refers to a stone that resembles or is made up of pea-sized particles.
Think of 'pea' ('piso') and 'stone' ('lithos') to remember that a pisolith is a stone made up of small, pea-sized particles.