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<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.1988.052.368.14</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>New Minerals</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Ashoverite, a New Mineral, and Other Polymorphs of Zn(OH)<sub>2</sub> from Milltown, Ashover, Derbyshire</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Clark</surname>
<given-names>A. M.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Fejer</surname>
<given-names>E. E.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Cressey</surname>
<given-names>G.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Tandy</surname>
<given-names>P. C.</given-names>
</name></contrib>
<aff>Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1988</year>
</pub-date>
<volume>52</volume>
<issue>368</issue>
<fpage>699</fpage>
<lpage>702</lpage>
<history>
<date date-type="received">
<day>31</day>
<month>3</month>
<year>1988</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1988, The Mineralogical Society</copyright-statement>
<copyright-year>1988</copyright-year>
<abstract>
<title>Abstract</title>
<p>Four polymorphs of Zn(OH)<sub>2</sub> have now been recorded from an oxidised vein exposure near Milltown, Ashover, Derbyshire; sweetite, w&#x00FC;lfingite, <italic>&#x03B3;</italic>-Zn(OH)<sub>2</sub>, and ashoverite. The last is a new mineral, a tetragonal modification of Zn(OH)<sub>2</sub> containing minor quantities of Pb, Cd and Ca. Its unit cell dimensions are <italic>a</italic> 6.825(2) and <italic>c</italic> 33.36(4) &#x00C5;, giving V = 1554 &#x00C5;<sup>3</sup>; Z = 32; space group <italic>I</italic>4<sub>1</sub>/<italic>amd</italic>, <italic>I</italic>4<sub>1</sub> <italic>md</italic>, or <inline-formula><mml:math><mml:mrow><mml:mi>I</mml:mi><mml:mover><mml:mn>4</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>2</mml:mn><mml:mi>d</mml:mi></mml:mrow></mml:math></inline-formula>; <italic>D</italic><sub>meas</sub>. 3.3, D<sub>calc</sub> 3.44 g cm<sup>&#x2212;3</sup>. Ashoverite occurs as colourless platy crystals associated with fluorite; it is uniaxial positive with <italic>&#x03C9;</italic> 1.629(2), <italic>&#x03B5;</italic> 1.639(2). The chemical composition of sweetite is compared with that of ashoverite.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>ashoverite</kwd>
<kwd>new mineral</kwd>
<kwd>zinc hydroxide</kwd>
<kwd>sweetite</kwd>
<kwd>Milltown</kwd>
<kwd>Derbyshire</kwd>
</kwd-group>
</article-meta>
</front>
</article>
