Amygdule

{{Short description|Infilled vesicle in extrusive igneous rock}}

{{For|part of the human brain|Amygdala}}

File:Vesicles in basaltic lava.JPG in Germany]]

Amygdules or amygdales ({{IPAc-en|ə|ˈ|m|ɪ|ɡ|dj|u:|l|z|,_|-|d|eɪ|l|z}}) form when the vesicles (pores from gas bubbles in lava) of a volcanic rock or other extrusive igneous rock are infilled with a secondary mineral, such as calcite, quartz, chlorite, or one of the zeolites.{{cite book |last=Grapes |first=Rodney H. |year=2011 |title=Pyrometamorphism |url=https://archive.org/details/pyrometamorphism00grap_972 |url-access=limited |edition=2nd |location=Berlin, Germany |publisher=Springer Verlag |page=[https://archive.org/details/pyrometamorphism00grap_972/page/n126 115] |isbn=978-3-642-15587-1}} Amygdules usually form after the rock has been emplaced, and are often associated with low-temperature alteration. Amygdules may often be concentrically zoned. Rocks containing amygdules can be described as amygdaloidal.

The word is derived from the Latin word amygdala, meaning "almond tree", and the Greek word αμυγδαλή, meaning "almond"{{spaced en dash}}reflecting the typical shape of an infilled vesicle. Amygdule is more common in American usage, while amygdale is more common in British usage.