Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia, and scientists have to climb down into hot crevasses to find the stuff. That being said, it is usually pretty ugly and massive material in terms of specimen appeal on the macro level. THIS piece, brought to my attention by my friend Dmitriy Belakovskiy of the Fersman Museum, has rheniite draped liberally on one side of the specimen and actual hardened rock made from the bubbly lava on the other! This shows the origins of the material so well, compared to most rather chunky specimens. Even aside from the lava, it is a really rich specimen with LOTS of bright microcrystalline rheniite. 8.9 x 7.8 x 7.7 cm
Atribusyon: Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
Malaya kang:
para ibahagi – para kopyahin, ipamahagi, at i-transmit ang akda
para i-remix – para i-adapt ang akda
Sa ilalim ng mga kondisyong ito:
atribusyon – Dapat magbigay ka ng isang maayos na pag-credit, ibigay ang link sa lisensiya, at tukuyin kung may mga pagbabagong ginawa. Magagawa mo ito sa isang risonableng paraan, pero hindi sa paraan na para bang ineendorso ka o ng paggamit mo ng naglisensiya sa'yo.
share alike – Kung ire-remix mo, babaguhin, o magdadagdag ka sa materyal, dapat mong ipamahagi ang mga ambag mo sa ilalim ng pareho o katulad na lisensiya.
This work is free and may be used by anyone for any purpose. If you wish to use this content, you do not need to request permission as long as you follow any licensing requirements mentioned on this page.
The Wikimedia Foundation has received an e-mail confirming that the copyright holder has approved publication under the terms mentioned on this page. This correspondence has been reviewed by a Volunteer Response Team (VRT) member and stored in our permission archive. The correspondence is available to trusted volunteers as ticket #2010022810018255.
Naglalaman ng mga karagdagang impormasyon ang talaksan na ito, marahil nadagdag mula sa kamerang digital o scanner na ginamit upang makalikha o gawing digital ito. Kung nabago ang talaksan mula sa orihinal na katayuan, maaaring hindi maipapakita ng lubusan ang detalye ng binagong larawan.