File:Linarite on quartz (Blanchard Mine, Bingham, New Mexico, USA) (49052168032).jpg

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Linarite crust on quartz from New Mexico, USA. (~6.8 centimeters across at its widest)

Deep blue = linarite Glassy gray material = quartz

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5500 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfate minerals all have one or more sulfate anions (SO4 -2).

Linarite is a lead copper hydroxysulfate mineral - PbCuSO4(OH)2. It has a nonmetallic luster, dark blue color, and tends to form thin crusts of small crystals.

Host rock: Council Springs Limestone, Missourian Series, lower Upper Pennsylvanian

Locality: Blanchard Mine (also known as the Portales-Blanchard Mine; Hansonburg Lead Mine; McCarthy Lead Mine), ~5.3 air miles south of the "town" of Bingham, Hansonburg Mining District, eastern Socorro County, central New Mexico, USA


Photo gallery of linarite:

<a href="http://www.mindat.org/gallery.php?min=2403" rel="noreferrer nofollow">www.mindat.org/gallery.php?min=2403</a>
Date
Source Linarite on quartz (Blanchard Mine, Bingham, New Mexico, USA)
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/49052168032 (archive). It was reviewed on 7 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

7 December 2019

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Date/TimeThumbnailDimensionsUserComment
current21:06, 7 December 2019Thumbnail for version as of 21:06, 7 December 20192,794 × 1,786 (6.14 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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