Equant/Stout – Length, width, and breadth roughly equal
Common examples include: apophyllite, olivine, garnetContinue Reading
Common examples include: apophyllite, olivine, garnetContinue Reading
Common examples include: gypsum, quartz, plagioclase, stauroliteContinue Reading
Common examples include: garnet, pyriteContinue Reading
Common examples include: fluorite, pyrite, galena, haliteContinue Reading
Common examples include: hedenbergite, quartzContinue Reading
Common examples include: agate (and other chalcedony)Continue Reading
Common examples include: limonite, turquoise, cinnabar, quartz, realgar, lazuriteContinue Reading
Common examples include: hemimorphite, elbaiteContinue Reading
Common examples include: heulandite, subhedral zircon Amygdules or amygdales (/əˈmɪɡdjuːlz, -deɪlz/) 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. Amygdules usually form after the rock has been emplaced, and are often associated with low-temperature alteration. Amygdules may often be concentrically zoned.Continue Reading
Common examples include: stilbiteContinue Reading
Common examples include: feldspar, topaz, vanadiniteContinue Reading
Common examples include: pyrophyllite, aragonite, wavellite, “pyrite suns”Continue Reading