Cuprosklodowskite
id:
cuprosklodowskite-258-15819241
title:
Cuprosklodowskite
text:
Cuprosklodowskite is a secondary uranium mineral formed by alteration of earlier uranium minerals. Its empirical formula is Cu(UO2)2(HSiO4)2·6(H2O). Cuprosklodowskite is a nesosilicate mineral, It is grass green to dark green in color, and its crystal habit is typically acicular, flat bladed crystals. It is a strongly radioactive mineral. Cuprosklodowskite was discovered in 1933 at the Kalongwe deposit in (then) Katanga province, Belgian Congo, the type locality. It was named in the mistaken bel
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Cuprosklodowskite
date created:
date modified:
2023-02-02T16:29:53Z
main entity:
{"identifier":"Q2479128","url":"https://www.wikidata.org/entity/Q2479128"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/0/0b/Cuprosklodowskite-27211.jpg","width":720,"height":464}
fields total:
13
integrity:
14