Stock (geology)
Smaller igneous intrusion From Wikipedia, the free encyclopedia
In geology, a stock is an igneous intrusion that has a surface exposure of less than 100 square kilometres (40 sq mi),[1][2] differing from batholiths only in being smaller. A stock has a discordant relationship with the rocks that it intrudes. Many stocks are cupolas of hidden batholiths.[3][2] Some circular or elliptical stocks may be volcanic plugs, which fill the vents of now extinct volcanoes.[4][5] A boss is a small stock.[6]

Examples
- the Alta and Clayton Peak stocks (composed of granodiorite), near Park City, Utah[7]
- the Hellroaring Creek and Salal Creek stocks (of granite-granodiorite and quartz monzonite, respectively) in British Columbia, Canada[8][9]
- the Céret stock (of gabbro and diorite) in Pyrénées-Orientales, France[10]
- the Parashi stock (of tonalite) in La Guajira Department, Colombia[11]
- stocks of syenite in the Caldera de Tejeda on Gran Canaria[12]
- Ailsa Craig granitic boss, which forms a volcanic plug, in Scotland[5]
References
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