A fact from Mosesite appeared on Wikipedia's Main Page in the Did you know column on 12 December 2007, and was viewed approximately 2,808 times ( disclaimer) ( check views). The text of the entry was as follows: Did you know... that when yellow crystals of mosesite, a very rare mineral found in deposits of mercury, are heated to 186 °C (367 °F), they become isotropic? A record of the entry may be seen at Wikipedia:Recent additions/2007/December.

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This article was developed from a term paper for a Fall 2007 Mineralogy class at the University of Houston taught by Dr. Jon Snow.—Preceding unsigned comment added by 74.7.31.34 ( talk • contribs)

The composition of Mosesite is variable, Mosesite is an anion exchanger and the anion concentration differences between samples was highlighted in the paper "Ree-examination of Mosesite" by Switzer, Foshag et al. Axiosaurus ( talk) 09:45, 19 December 2012 (UTC) reply