Srednji Ural
(Middle Ural)



The Srednji Ural is roughly the area of the Ural around the towns of Nizhne Tagil and Ekatarinburg.

19 Parts'ezda mine
(XIX Parts'ezda mine)

The 19 Parts'ezda mine is a copper mine of the Uralian Chalcopyrite Belt close to Bajmak

Calcite Chrysocolla Mimetesite Volborthite

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Akhtenskoye mine

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The Akhtenskoye mine is located north of  Magnitka north of  Zlatoust. Akhtenskoye is an iron ore deposit, which is the type locality for Akhtenskite.

Akhtenskite Cryptomelane Nsutite Pyrolusite Vernadite

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Alapaikha peak

Alapaikha peak is a late magmatic chromite deposit. The chromite occurs in serpentinised harzburgite and serpentinite.


Geology of Mineral Deposits, V.I. Smirnov, 1976, p109

Aramashevsk mine

Located in the Alapaevsk district. It is a low temperature hydrothermal deposit in schist.

Antimonite Gold Quartz


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Bazhenovskoye is a rodingite. This means it is an altered fragment of the old oceanic crust, from the ocean that once was situated between Asia en Europe. Bazhenovo is located near Asbest. The mine is currently operated by the JSC UralAsbest The mine is operated since 1885 and is Russia largest asbestos mine.

Apophyllite-(KF) Brucite Chabazite-Ca Chromferide Clinobehoite Clinochrysotile Clinotobermorite Diopside Epsomite Grossular Heazlewoodite Hydromagnesite Hydrotalkite Laumontite Lizardite Magnesioriebeckite Magnesite Manasseite Pectolite Plombierite Roggianite Rosenhahnite Spessartine Stilbite-Ca Talc Tobermorite Uwarowite Vesuvianite Xonotlite

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 Grossular  (Hessonite)
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Located near Zlatoust, Beryaush is a rapakivi granite intrusion with syenites and nepheline syenites in the central part of the intrusion.

Aegirine Albite Allanite-(Ce) Biotite Hastingsite Magnetite Muscovite Nepheline Titanite Zircon



Beresovsk is a mining town northeast of Ekatarinburg. Beresovsk is the oldest mine of Russia and was discovered in 1745 (some sources report 1744). Beresovsk is geologically a complex deposit. The host rock is metamorphic rock, mostly formed from siluric volcanosediments. Then there are ultrabasic intrusion, mainly serpentinites. Finally there are many granite and aplite veins. The ultrabasic intrusions brought chromium to the deposit, while the granite brought lead, gold and other elements. This explains the formation of some rare lead chromates in the secondary mineralisation.

Individual mines are:  Preobrazhenski mineTsvetnoi mineSevernaya mine, Kirovsk mine, Yuzhnaya mine, Vspomogatelnaya mineKlyuchevsky mine, Staropyshimskoye mine, 5 shaft and the Leninskaya shaft. On maps I so far located the positions of 11 shafts, but I have difficulty to pair the names with the locations. Any helkp is welcome. click here to get a Google earth placemark of the Beresovsk shafts. So far I know 'berezovsk-4' is the Severnaya mine.

Acanthite Actinolite Aikinite Anglesite Ankerite Annabergite Antigorite Aragonite Azurite Barite Bayldonite Beudantite Bindheimite Bismite Bismuth Bismutite Bornite Brucite Bushmakinite Calcite Caledonite Cassedanneite Cassiterite Cerussite Chalcocite Chalcopyrite Chromite Chrysocolla Copper Cornubite Cosalite Covellite Crocoite Cuprite Dolomite Dravite Duftite Embreyite Emplectite Ferrimolybdite Fluoroapatite Fornacite Galena Galenobismuthite Gaspeite Gersdorffite Goethite Gypsum Hessite Ilmenite Jarosite Karminite Lead Leadhillite Lepidocrocite Linarite Liroconite Livingstonite Magnesiofoitite Malachite Marcasite Massicotite Microcline Millerite Mimetesite Minium Molybdenite Morenosite Mottramite Muscovite Nickeline Nontronite Olivenite Opal Pentlandite Pharmacosiderite Phoenicochroite Phosgenite Polydymite Prehnite Preisingerite Pyrite Pyrolusite Pyromorfite Pyrophyllite Pyrrhotite Quartz Rutile Scheelite Schorl Scorodite Senarmontite Siderite Silver Sphalerite Sternbergite Stolzite Sudoite Tennantite Tetradymite Tetrahedrite Tirolite Titanite Torbernite Tungstenite Vanadinite Vauquelinite Violarite Wittichenite Wulfenite Zircon

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Aikinite                Cerussite              Crocoite                Gold                    Pyromorphite


Glucine Moraesite Uralolite


Borodulinskoye is a Rhodonite deposit located just southeast of Ekaterinburg

Alleghanyite Rhodochrosite Sonolite


Degtyarskoye deposit is located in the Tagil-Magnitogorsk greenstone belt. The deposit consists of sericite-quartz-chlorite-schist, volcanosedimentary rocks and limestone of the Karamalytash formation. It is part of the Uralian Chalcopyrite belt.

Acanthite Arsenopyrite Bornite Chalcanthite Chalcocite Chalcopyrite Cubanite Digenite Galena Gold Goslarite Magnetite Malachite Mawsonite Pyrite Rutile Silver Sphalerite Stannoidite Tennantite Tetrahedrite

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol II, p140


Gaiskoye is located in the Tagil-Magnitogorsk greenstone belt. It is a stratiform deposit in volcanosedimentary rocks.

Altaite Arsenopyrite Betekhtinite Bonattite Bornite Calaverite Chalcopyrite Coloradoite Galena Germanite Gold Hessite Krennerite Marcasite Mawsonite Perroudite Poitevinite Pyrite Selenium Siderotile Sphalerite Stannoidite Tellurobismutite Tennantite Tetrahedrite

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The Goroblagodat deposit is an iron deposit at the contact of a  diorite-syenite intrusion and volcanosedimentary rocks of the Tura group. The sedimentary rocks formed magnetite skarns.

Bornite Calcite Chalcopyrite Epidote Fluorite Fluoroapatite Galena Hematite Magnetite Marcasite Orthoclase Pyrite Pyrrhotite Quartz Sphalerite Titanite

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol I  pp40-43

Gumeshevskoye mine

Gumechevskoye is a copper skarn of Hercynian age, surrounded by rocks of the proterozoic Tagil-Magnitogorsk greenstone belt. The mine is located about 1km north of Polevskoi zavod along the Chusovaya river. The deposit was discovered in 1702 and mining commenced 1709. The mine is equally famous for large ornamental malachite blocks as Mednorudyansk. The mine closed at the end of the 19th century.

Azurite Brochantite Copper Cuprite Malachite Nsutite Tenorite


Gusevogorsk is the eastern part of the Kachkanar deposit. In references both deposits are often dealt with separately, but geologically they are one. See Kachkanar for details. The mineralogy below is what I found for Gusevogorsk, but the Kachkanar mineralogy will also occur here.

Atheneite Bornite Bowieite Braggite Chalcopyrite Cooperite Cuprorhodsite Erlichmanite Gold Ilmenite Iridium Isoferroplatinum Kotulskite Laurite Magnetite Mertieite-I Osmium Palladium Platinum Potarite Pyrite Sperrylite Stibiopalladinite Vysotskite

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol I, pp35-37
The geochemistry of gold and it's deposits, geological survey of Canada, bulletin 280, 1979, p 39


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Kachkanar is a magmatic iron deposit low in titanium content. It is a dunite-pyroxenite intrusion into ordovician schists and silurian diabase. The large dunite intrusion formed nine bodies of dunite rock. Only the western  body is called Kachkanar, the 8 more easterly bodies form the Gusevogorsk intrusion. The ore is rich in vanadium and PGM elements. It is likely that the minerals stated under Gusevogorsk also occur here.

Awaruite Bornite Chalcopyrite Ilmenite Magnetite Osmium Pentlandite Platinum Pyrite Pyrrhotite Wairaurite

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol I, pp35-37

Katsina Yama
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Epidote (var Pushkinite)

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 "Pushkinite" ( Epidote)


Located south of Nizhne Tagil, 'Kirovgrad' is a group of deposits of the Uralian Chalcopyrite belt.

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol II, p140

Kopeisk / Korkino

   Kopeisk                        Korkino

A point of ever lasting discussion in the mineral community is the question if minerals from burning coal dumps are genuine minerals or man made artifacts. The IMA, the authority in this field, has a peculiar view. All minerals discovered up until a certain date are accepted as mineral, the newer ones are man made.......  

Kopeisk and Korkino are towns in the Chelyabinsk coal basin. This basin consists of Triassic browncoal. The coal itself is not very interesting, but the mine waste was dumped on numerous local dumps. Pyrite within the coal oxidized and generated heat, causing remaining coal particles to catch fire. These spontaneous fires occur on many coal dumps and are known to rage for many years or decades. Most of the dumps in the Kopeisk-Korkino basin are not burning anymore, but they left behind an interesting mineralogy. 

A number of the minerals listed below are not IMA approved minerals because of the discussion whether or not they are man made. 

Aciculite Aegirine Afanasievaite Akermanite Albovite Alunogene Amminite Ammoniojarosite Andalusite Anglesite Anhydrite Anorthite Antarcticite Antlerite Aragonite Armacolite Atacamite Bassanite Bazhenovite Belosharite Biotite Blödite Boussingaultite Brochantite Brucite Calcite Calciumoxide Chalcanthite Chalcocite Chalcocyanite Chalcopyrite Chelyabinskite Chesofiite Chlorocuspidine Chlorohischite Chlorozincite Chondrodite Clinohumite Coalingite Cohenite Copiapite Copper Coquimbite Cordierite Corund Cottunite Covellite Cristobalite Cuprite  Cuspidine Diopside Dmisteinbergite Dolerophanite Dorrite Dypingite Efremovite Ellestadite  Enstatite Epsomite Esseneite Fayalite Ferro-Cadwadalerite Ferrosilite Fluorapatite Fluorellestadite Fluorite Fluormagnesiohastingsite Fluormagnesiohornblende Forsterite Galena Gehlenite Geikilite Giorgiosite Godovikovite Goethite Grandiferrite Graphite Gypsum Gyrolite Hematite Hercynite Hexahydrite Hibschite Huntite Hydrobasaluminite Hydromagnesite Ignicolorite Igumnovite Indialite Iron Khademite Kladnoite Koktaite Kopeiskite Krasnogorite Krasnoselskite Kruzhevite Kutyukhinite Laihunite Langebeinite Larnite Lausenite Lawrencite Lepidocrocite Leucite Leucorhörnite Lithargite Maghemite Magnesioferrite Magnesiowüstite Magnetite Malakhovite Mascagnite Massicotite Mayenite Mesohydrite Mohrite Molysite Mullite Nantokite Nesquehonite Norbergite Oldhamite Opal Osumilite Ovchinnikovite Oxiferberite  Paratacamite Pentahydrite Periclase Perkovaite  Perowskite Phlogopite Pickeringite Plattnerite Podnoginite Portlandite Pseudobrookite Pyrite Pyroaurite  Pyrrhotine Quartz Redikortsevite Rhomboclase Rhythmite Rorisite Rosickyite Rukavishnikovite Rutil Salmiac Sekaninaite Sellaite Sinjarite Spinel Spurrite Srebrodolskite Starkeyite Sulphaluminite Sulphur Svyatoslavite Tenorite Terriconite Thenardite Tinnunculite Titanite Topaz Torbakovaite Tridymite Troilite Tschermigite Vaterite Wagnerite Warwickite Wolframite Wollastonite Wüstite

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Brennende Abraumhlden und Aufschlüsse im Tscheljabinsker Kohlenbecken eine reiche Mineralienkuche, Boris Cesnokov et al, Mineralien Welt 3/98


Located north of Nizhne Tagil, the Krasnouralsk group of deposits is copper deposit of the Uralian Chalcopyrite belt. 

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol II, p140


Kungur is a city southwest of Perm, known for it's large caves. The caves and gypsum deposits in the area probably have individual names.


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Kurganovskoye is a rodonite deposit in the Srednji Ural.

Alabandite Bannisterite Calcite Chalcopyrite Cummingtonite Galena Manganocummingtonite Pyrite Pyrochroite Pyroxmangite Rhodonite Spessartine Sphalerite Tephroite

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Kushva is a pegmatitic nepheline syenite.

Aegirine Albite Allanite-(Ce) Analcime Augite Cancrinite Fluoroapatite Hastingsite Magnetite Nepheline Oligoclase Platinum Titanite


Lebyazhinsk resembles a magmatic apatite-magnetite type deposit. Other sources state it as a skarn. A combination is of course possible. More information about this locality is welcome!

Fluoroapatite Magnetite

Geology of Mineral Deposits, V.I. Smirnov, 1976, p115


Lipovka is a granite pegmatite in the Rezh district of the Srednji Ural. It gained most fame as type locality of magnesiotantalite. A granite pegmatite cuts a serpentine close to a contact with marl.

Asbolane Bismutomicrolite Bismutotantalite Calcite Chrysoberyl Clinochlore Cordierite Dravite Dumortierite Dwornikite Elbaite Ferrocolumbite Ferrotantalite Lepidolite Magnesiotantalite Microcline Pecoraite Phenakite Phlogopite Quartz Tremolite Uranmicrolite

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Malaya Sedelnikovaya

Malaya Sedelnikovaya is a metamorphosed sedimentary manganese deposit. It is mainly used to quarry rhodonite for ornamental purposes, for instance for the construction of Majakovskaya station of the Moscow subway.

Bustamite Kellyite Manganocummingtonite Pyroxmangite Rhodonite Tephroite

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(Takovaya, Izumrudni Kopi)

Malyshevo is not so much a locality, but more a mining district. Therefore I would favor the name Izumrudny Kopi district (Emerald mines district). But the name 'Malyshevo' got  more popular. It all started in 1831, when the first emerald was found here by accident. Not soon afterwards the firt mine, the Sredjensky mine, was opened here. 

The Malyshevo district consists of complex hydrothermally altered rocks. To the west it borders the granite massif of Adui. In the east the Malyshevo complex borders granodiorites, serpentinitesgabbros and pyroxenedunites of the Asbestov intrusion.
Basically the Malyshevo complex consists of schist. But the schists where hydrothermally altered into talc and serpentinite. Bauxitisation, kaolinisation  and chloritisation also took place. More interestingly some elements like beryllium migrated from the Adui granite into the altered schist at the contact zone.

Individual mines in the district are: Artyom mine, Aulsky mine, Berjozovaya Rostcha, Krasnoarmejski mine (Chitny), Krasnobolotski mine, Krupskaya mine, Lublinsky mine, Mariinski mine, Ostrovnoye mine, Pervomaiskoye mine (Troitsky mine), Sredjensky mine and, Starkovsky mine

Allanite-(Ce) Analcime Anatase Antigorite Bavenite Behoite Bertrandite Beryl Bityite Bromellite Brookite Chabazite-Ca Chondrodite Chrysoberyl Clinobehoite Clinochlore Clinohumite Clinozoisite Corund Enstatite Euclase Garronite Helvite Ilmenite Isokite Laumontite Margarite Microlite Molybdenite Monazite-(Ce) Opal Paragonite Protojoseite Pyrochlore Rutile Scheelite Thorite Titanite Topaz Xenotime-(Y) Zircon

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   Aleksandrite            Beryl

Alexandrite aus dem Ural, Helmut Leithner, Lapis April 1980, pp25-28
Die Smaragdgruben des Urals, Evgenji Burlakov et al, Lapis 7-8/1997, pp44-55

Mednorudyansk mine

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The Mednorudyansk mine triggers the reflex 'malachite!' with most collectors. The deposit was discovered in 1814 by Demidov, who also operated the Vysokogorsky mine in Nizhne Tagil. The Mednorudyansk mine is located on the southern slope of Vysokaya sopka, inside the town of Nizhne Tagil. The main product was malachite (hence the background of this website). In 1834 a 3000 pound chunk of solid malachite was dug up. The malachite from here was used to decorate the Winters palace in St.Petersburg. Mednorudyansk was mined by shafts of which the Nadezhda shaft was one. Since 1972 the deposit is mined by an open pit and the shafts are closed.

Azurite Brochantite Chalcocite Chalcopyrite Chalcosiderite Chrysocolla Copper Cuprite Cyanotrichite Delafossite Libethenite Magnetite Malachite Olivenite Pseudomalachite Pyrite Pyrolusite Reichenbachite Wavellite


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Murzinka District

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Kazennitsa            Semeninskii

Murzinka is not a true locality but rather an old mining district, located roughtly 150km north of Ekaterinburg. The district is discussed as a whole because in history there were countless small mines and pits, often no deeper that 10 meters. It is impossible to research each of these pits separately. Individual mines include: Alabashka mine, Karnilova mine, Sissikova mine, Yushakova mine, Shaitanka mine ,  Kazennitsa mine,  Meshcherskii mine,  Mokrusha mine, Novaya mine,  Novgorodnaya mine Semeninskii mine,  Suvorovskaya mine,  Topaznitsa mine,  Vatikha mine.

The geology of Murzinka requires a more regional description. Murzinka is located in the Murzinka-Adui megaanticlinorium, which is located in the Eastern Ural megazone. The Murzinka-Adui megaanticlinorium is regarded as a micro continent, or a continental fragment that became separeated during the Odrovicium. The rocks of the megaanticlinorium consist mainly of three metamorphic units. The oldest one dates back to the upper Paleozoicum and consists of biotite gneiss, garnet-biotite-gneiss and two mica gneiss. A little younger is unit consisting of amphiboles and amphibole-biotite gneiss. The youngest unit consists of graphite-mica schists and quartzites with lenses of amphibole gneisses. 

Murzinka is a granite with large pegmatite veins, up to 3 meter in width.

Albite Beryl Elbaite Hambergite Kanonerovite Lepidolite Microlite Masutomilite Orthoclase Quartz Topaz
(Kazennitsa mine, is the type locality for Kanonerovite)

Russische Topase und Berylle, Helmuth Leithner, Lapis september 1981, pp9-14


Newyansk is the name of a concession on the Vysokaya mountain in Nizhne Tagil. See Nizhne Tagil for more information.

Brass Iridium Osmium Palladseite Platinum Rutheniridosmine Ruthenium Sorosite Tetraferroplatin

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Nizhne Tagil

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The Nizhne Tagil deposit was discovered in 1696 as iron mine (magnetite ore). The first mining activity was at Vysokaya hill, which was also known as Magnitnaya hill. In 1721 mining started on this hill in the Vysokorskoye mine (see separate entry below). After the owner of the mine, Demidov, died the consession was split into three. These three consessions have very familiar names to today's mineral collectors: Revda, Nizhne Tagil and Newyansk. Later in the 18th and 19th century the Revda and Newyansk where split up further, so Vysokaya mountain had the Revdinsky, Suksunsky, Verkh-Isetsky, Alapayevsky and Newyanski mines. The name Vysokogorsky mine seemed to be some universal name for all the mines on the mountain. In 1990 the main quarry of the Vysokogorsky mine closed and was partially flooded.

Nizhne Tagil is often mentioned as platinum occurence.  The source of this platinum, or better these PGM minerals is a differentiated dunite-pyroxenite intrusion. The country rocks are volcanosediments and metavolcanics of the Tagil-Magnitogorsk greenstone belt. The intrusion itself measures about 6km east-west and 12km north south and is also known as Solovjovaya Gora. In the streams next to Solovjovaya Gora are many platinum placers, which are also a very important source for PGM minerals. One such placer is Novy Log  placer about 2km west of the massif. Another one is the Bobrovka river.

Arsenopyrite Awaruite Bowieite Braggite Brass Chromite Clinochrysotile Cooperite Cuprostibite Diopside Erlichmanite Ferronickelplatinum Galena Gold Gupeiite Hausmannite Hexaferrum Irarsite Iridium Isoferroplatinum Kashinite Laurite Palladium Platinum Pyrrhotite Sperrylite Stannite Tetraferroplatin Tin Tulameenite Volborthite Vysotskite

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 Arsenopyrite            Osmium                Palladium            


Located near Ekatarinburg, Nyzepetrovsk is consists of peralkaline and nepheline syenites, trachytes and phonolites.

Aegirine Albite Andradite Biotite Calcite Chalcopyrite Fluorite Fluoroapatite Grossular Hastingsite Magnetite Nepheline Orthoclase Pyrochlore Titanite


Ozernoye is a copper deposit of the Uralian Chalcopyrite Belt.

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol II, p140


Pervouralskoye is a dunite-pyroxenite intrusion



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Shabry is located close to Ekatarinburg and is one of the typical Talc mines of the Ural. The Talc is formed by metamorphose of ultrabasic rocks from the ancient ocean floor.

Buergerite Dolomite Hematite Hydroxylapatite Schorl Talc

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   Dolomite          Hematite / Talc

Solovjovaya Gora

A more correct name for the Nizhne Tagil platinum occurence. But because Nizhne Tagil is better known I put it there. So see Nizhne Tagil a little higher on this very page.

Sukhoi Log

Sukhoi Log is a not so long ago discovered gold-pgm deposit northeast of Ekatarinburg. Sukhoi Log is a stratabound gold deposit is limestone of the Riphean Khomolkhinsk Formation. It is a very promising deposit economically and there is an impressive array of minerals allready known to occur at this locality. A lot of them are probably only as microscopic inclusions.

Acanthite Altaite Arsenopyrite Baddeleyite Berzelianite Calaverite Cervelleite Chalcopyrite Chromium Cobaltite Cooperite Copper Cubanite Cylindrite Dyscrasite Enargite Galena Galenobismuthite Gersdorffite Gold Greenockite Heazlewoodite Hessite Iodargyrite Iron Isoferroplatinum Joseite-A Krennerite Lead Magnetite Maucherite Millerite Molybdenite Monazite-(Ce) Nickeline Pentlandite Petzite Platinum Pyrite Pyrrhotite Rammelsbergite Rutile Safflorite Scheelite Silver Skutterudite Sphalerite Stutzite Tetraferroplatin Tetrahedrite Tin Titanium Tulameenite Umangite Violarite Xenotime-(Y)


Syssert is again an ultrabasic relict of the ancient oceanic floor

 Buergerite Magnetite Osmium Planerite Volborthite

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Uktus is a complex Dunite intrusion, located just southeast of Ekatarinburg. Several blocks of Dunite, lay inside a zone of Clinopyroxenite and Wehrlite. The latter one is cut by Gabbro. The complex aso contains small amounts of Chromitite.

Brugnatellite Chromite Cuproiridsite Cuprorhodsite Erlichmanite Isoferroplatinum Lithiophorite Osmium Platinum Tetraferroplatin Tulameenite

Pt Alloys from Chromitites of Uralian-Alaskan complexes, Russia, by G.Garuti et al, Canadian Mineralogist Vol 40 pp.357-376


The Volkovo deposit is located in the northern part of the Srednji Ural. Geologically it is located in the most northern part of the Tagil massif. This part of the Tagil massif is also known as the Volkovo gabbrol massif. It is a magmatic copper deposit with gabbro, gabbro-diorite and quartz-diorite as main rocks.

Anorthite Azurite Biotite Bornite Bytownite Chalcocite Chalcopyrite Fluoroapatite Galena Labradorite Magnetite Malachite Merenskyite Pyrite Pyrrhotite Sphalerite

Ore Deposits of the USSR, by V.I. Smirnov, 1977, Vol II pp 107-112

Vysokogorskoye mine
(Gora Vysokaya)

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For the complex history of this mine see Nizhne Tagil, above. Gora Vysokaya means high mountain

Located close to Nizhne Tagil this mine is an iron skarn deposit, probably of Hercynian age, located inside the proterozoic Tagil-Magnitogorsk greenstone belt.

Magnetite, native Iron

Zolotaya Gora

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Zolotaya Gora, or 'Golden mountain' is also known as Karabash. It is a so called rodingite. In this case the rodingite is a metamorphically altered gabbroid rock of the Tagil-Magnitogorsk greenstone belt.. The fluids for this alteration came from seawater, much like the formation of rodingites in the Alps. Surrounding the rodingite is serpentinite. In the following tectonic activity the serpentinite is ductile, but the rodingite is not and cracked. Inside these cracks gold is deposited. Karabash is regarded part of the Uralian Chalcopyrite belt

Antimony Arsenopyrite Auricupride Awaruite Breithauptite Calcite Chalcocite Chalcopyrite Chromite Cohenite Copper Cuprostibite Fluoroapatite Galena Graphite Gudmundite Ilmenite Lead Lizardite Magnetite Nickeline Nisbite Pyrrhotite Seinajokite Tetraauricupride Titanite Ullmannite Vermiculite Vesuvianite Zlatogorite Zlatogorite

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Auricupride            Lizardite

Ore deposits of the USSR, V.I. Smirnov, 1977, Vol II, p140