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Chelotriton paradoxus
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Chelotriton paradoxus

We traveled around the world to find some good samples to show you.

Below is a series of new specimens of amphibian Chelotriton paradoxus from the Miocene mid. recently recovered and restored.

Samples are available.

Read here

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49° TORINO EUROMINERAL EXPO
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Hi guys we are in Torino Mineral Show with a truly exceptional lot of minerals from Iran and Bosnia. Our stand is c/o Zoic our partner!

📍 49° TORINO EUROMINERAL EXPO https://www.euromineralexpo.it

⏰ Program:

2-3-4 October 2020

Timetables:

Visitors:
Friday: from 9:00 to 19:00 (last admission time: 18:00)
Saturday: from 9:00 to 19:00 (last admission time: 18:00)
Sunday: from 9:00 to 19:00 (last admission time: 18:00)

#3bminerals #dinosaures #fòssils #minerals #meteorits #geologia #Chelotryton #Paradoxus #Rhodocrosite #Blenda #Barasaurus #Besairiei #Kutnahorite #Aragonite #Dioptase #PietraPaesina #Expominer

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EXPO MINER Barcellona
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Today begins the new edition of #Expominer! We will be waiting for you with our stand along with 110 other exhibitors. We are waiting!

📍 @ FiradeBarcelona on the Montjuïc site in Barcelona http://bit.ly/2nNv0ZX

⏰ Program:

November 8 and 9, from 10 a.m. to 8:30 p.m.
November 10, from 10 to 20

#3BMinerals #dinosaure # fòssils #minerals #meteorits #geologia #Chelotryton #Paradoxus #Rococrosite #Blenda #Barasaurus #Besairiei #Kutnahorite #Aragonite #Dioptase #PietraPaesina #Expominer

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Mineral Exhibition Rome 2018 – Mostra di Minerali Roma 2018
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Mineral Exhibition Rome – 1 e 2 Dicembre 2018

3B Minerals is present with its own collection at the table of Zoic srl at Stand number 2.

Mostra di Minerali Roma 2018

Il 3B Minerals è presente con la propria collezione al tavolo di Zoic srl presso lo stand 2 .

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Steatite of  Meleto quarry
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The  “Scaly-Clays Complex”  is the prevailing  rock formation  in the section of the Appennines between Emilia and Tuscany, but many different kinds of alloctonous rocks may be observed there; ophiolites are frequent and, among them, the so-ca/led “Green Rocks”  (gabbros, diabases, serpentinites).  They are chaotically and accidentally embedded in the clastic sedimentary clays; probably  originated  by intensive submarine  volcanic  activity between Corsica and Tuscany, they were fragmented   and moved along the Appennines by orogeny between Cretaceous and Pliocene.  

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Gyspum Flower of the Cetine Mine-Italy
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NEW FINDING FROM THE CETINE DI COTORNIANO (SIENA)
For those mineral collectors who visited the Cetine di Cotorniano mine since young age, the finding of a “gypsum flower” specimen constitutes much more than a simple wish. This nightmare was driven by the picture of an old specimen stored in the mineral collection of the Natural History Museum of Genova and published on the “Guida ai Minerali”. The extreme difference between that specimen and those found after the closure of mine workings at Le Cetine di Cotorniano gave rise to a myth about “gypsum flowers”.

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