<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<article article-type="research-article">
<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1956.031.235.01</article-id>
<title-group>
<article-title>Birnessite, a New Manganese Oxide Mineral from Aberdeenshire, Scotland</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Jones</surname>
<given-names>L. H. P.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">1</xref></contrib>
<contrib contrib-type="author">
<name>
<surname>Milne</surname>
<given-names>Angela A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN2">2</xref></contrib>
<aff>Commonwealth Scientific and Industrial Research Organization</aff></contrib-group>
<author-notes>
<fn fn-type="other" id="FN1"><label>1</label><p>Division of Plant Industry, c/o School of Agriculture, University of Melbourne, Victoria.</p></fn>
<fn fn-type="other" id="FN2"><label>2</label><p>Division of Building Research, Highett, Victoria; formerly of the Macaulay Institute for Soil Research, Aberdeen.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>12</month>
<year>1956</year>
</pub-date>
<volume>31</volume>
<issue>235</issue>
<fpage>283</fpage>
<lpage>288</lpage>
<copyright-statement>Copyright &#x00A9; 1956, The Mineralogical Society</copyright-statement>
<copyright-year>1956</copyright-year>
<abstract>
<title>Summary</title>
<p>A manganese pan near Birness contains grains of an optically uniaxial negative mineral near (Na<sub>0&#x00B7;7</sub>Ca<sub>0&#x00B7;3</sub>)Mn<sub>7</sub>O<sub>14&#x00B7;</sub>2&#x00B7;8H<sub>2</sub>O, giving an X-ray powder pattern similar to that of synthetic materials described as &#x2018;manganous manganite&#x2019; and &#x03B4;-MnO<sub>2</sub>. Material giving a similar pattern has been described from a natural occurrence in Canada, but no mineral name was assigned; the name <italic>birnessite</italic> is now proposed. The mineral is probably formed by air-oxidation of manganous oxides under alkaline conditions.</p></abstract>
</article-meta>
</front>
</article>
