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Kondyor Massif of Eastern Siberia

The Kondyor Massif is a  perfectly circular geological shaping in Eastern Siberia, Russia, approximately 600 km west-to-southwest of Okhotsk, or practically 570 km south-east of Yakutsk. From space it would seem that an effect hole or the caldera of an extinct volcano, however Kondyor Massif is not, one or the other. It is the thing that geologists allude to as an “intrusion”.

An interruption structures when liquid magma of volcanic rock takes shape underneath the surface of the earth, and is gradually pushed up through the world's mantle, a process that can take a huge number of years. As the rock gradually cools into a strong, the diverse parts of the magma solidify into minerals. Since the magma set underground before they achieve the surface of the covering, they are additionally called "plutons", to pay tribute to the Roman god Pluto, the lord of the underworld. 

Kondyor Massif is around 10 kilometers in breadth with edges arriving at to a stature up to 600 meters. A little waterway, bolstered by rainwater gathering inside the raised edge streams out of the massif through a cut in the edge. Kondyor Massif is novel due to its curious structure, as well as for the mineral veins inside it - gold, silver, platinum and heaps of other rare minerals.

Kondyor Massif is a vital wellspring of platinum and is the site of a monstrous platinum mine. Mining began here in 1984, and till 2011 the Kondyor mine has delivered around 85 tons of platinum. An alternate exceptional and extremely curious mineralogical gimmick of the store is the vicinity of coarse precious stones of platinum-iron compound, covered with gold. The Kondor Massif even has its own particular extraordinary mineral known as Konderite, a mixture of copper, platinum, rhodium, lead, and sulfur.
Kondyor Massif Of Eastern Siberia




Source : wikipedia

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