Ефузивни скали [Nature Category:
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“Ефузивните (вулканични) скали са магмени скали, които се образуват от лава, застинала на земната повърхност, за разлика от интрузивните скали, формирани под повърхността. Изливането на лавата става или през сравнително малки отвори, при което се образуват вулкански конуси или по-големи по дължина пукнатини, т.нар. пукнатинни вулкани. Примерни ефузивни скали са липарит, риолит, диабаз, трахит, базалт, андезит. …” (Wikipedia) (Wikipedia translated)
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