Serpentine Mortar and Pestle CW436
$85.00
In stock
SKU
cw436
These are example of Serpentine Mortar and Pestle crystal as shown in the image.
Weight: 1981 grams approx
Serpentine is a wonderful healing stone! It also inspires longevity and retrieval of ancient wisdom It can be used to clear the clouded areas of the chakras and to stimulate the Crown Chakra. It enhances meditative states.
Serpentine is the true stone of our Mother Earth, it’s forgotten magical history, and it’s epic future. It is a magnesium Silicate Mineral that occurs in a rather fibrous form. It is a heavy, dense stone that is often linked to the appearance of a snake or reptile. It varies in colors from yellowish-greens to deep green and in some cases even black. This one of a kind stone is spread across the globe, however its most commonly found in the deposits of Great Britain, USA, Brazil, and South Africa. It’s color has birthed some of its popular nicknames as “New Jade”, “Olive Jade”, and “Snake Jade”| More Info | The serpentine subgroup (part of the kaolinite-serpentine group) are greenish, brownish, or spotted minerals commonly found in serpentinite rocks. They are used as a source of magnesium and asbestos, and as a decorative stone.[1] The name is thought to come from the greenish color being that of a serpent.[2] The serpentine group describes a group of common rock-forming hydrous magnesium iron phyllosilicate ((Mg, Fe)3Si2O5(OH)4) minerals, resulting from the metamorphism of the minerals that are contained in ultramafic rocks.[3] They may contain minor amounts of other elements including chromium, manganese, cobalt or nickel. In mineralogy and gemology, serpentine may refer to any of 20 varieties belonging to the serpentine group. Owing to admixture, these varieties are not always easy to individualize, and distinctions are not usually made. There are three important mineral polymorphs of serpentine: antigorite, chrysotile and lizardite. The serpentine group of minerals are polymorphous, meaning that they have the same chemical formulae, but the atoms are arranged into different structures, or crystal lattices.[4] Chrysotile, which has a fiberous habit, is one polymorph of serpentine and is one of the more important asbestos minerals. Other polymorphs in the serpentine group may have a platy habit. Antigorite and lizardite are the polymorphs with platy habit. |
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