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RARE OLIVINE CUMBERLANDITE STONE - MAGNETIC- CRYSTALS *1 PLACE ON EARTH* 566 Gr For Sale
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RARE OLIVINE CUMBERLANDITE STONE - MAGNETIC- CRYSTALS *1 PLACE ON EARTH* 566 Gr:
$25.00
You are offerding on a RARE 566 Gram OLIVINE CUMBERLANDITE STONE THIS IS A RARE CUMBERLANDITE MAGNETIC STONE THAT CAN ONLY BE FOUND IN 1 VERY SMALL PLACE. Please look at all the pictures. The cumberlandite you see, is the specimen you will receive with your winning offer. Up for sale is a unique Super Rare Multi-Mineral Cumberlandite specimen. This 100% real Cumberlandite Multi-Mineral Rock features around 24 different minerals. Some of the minerals found in Cumberlandite are: Olivine, Titanium, Iron, Magnetite, Ilmenite, and Hercynite Spinel and many others. Some interesting Information and facts: These rare specimens come from one small 4 acre spot and can’t be found in any other place in the world!!! Cumberlandite was often mistaken for and sold as a Meteorite because of its appearance. It’s very heavy for its size and its magnetic. CUMBERLANDITE is world renown and was formed over 1.5 Billion years ago when a volcano erupted and 24 different minerals mixed together with molten rock forming a magnetic rock rich in minerals. CUMBERLANDITE is known as the “Stone of Venus” and is said to be connected with Templar symbolism of the divine female in the heavens, symbolized by the planet Venus. CUMBERLANDITE has been been used as a healing stone and is said to good for mental acuity, and mental and physical communication. Its also said to assist in the treatment of disorders of the brain, the sympathetic nervous system and the thyroid and parathyroid glands. CUMBERLANDITE is classified into three different types 1 Monotonuous Cumberlandite - no white plagioclase crystals.... 2 Ornament Cumberlandite - varying white plagioclase crystals.... 3 Tenuous Cumberlandite - greenish and or blueish plagioclase crystals.... The rock is an uncommon type known as a troctolite. It is black with phenocrysts of plagioclase in a medium grained matrix of magnetite, ilmenite, olivine and hercynite spinal. The abundance of magnetite and ilmenite, may be responsible for the high density and magnetic property. Locally the parallel orientation of the lath like plagioclase crystals gives the rock a flow lamination. Rock age is uncertain but said to be from Late Proterozoic to Devonian.
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