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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.1960.032.250.04</article-id>
<title-group>
<article-title>&#x03B2;-Ferric Oxyhydroxide</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Mackay</surname>
<given-names>A. L.</given-names>
</name><degrees>M.A., Ph.D., F.Inst.P.</degrees>
<aff>Birkbeck College Crystallographic Laboratory, London.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>250</issue>
<fpage>545</fpage>
<lpage>557</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>The crystallographic properties of the hydrated iron oxide obtained by the hydrolysis of FeCl<sub>3</sub> are described. The characterizing X-ray powder pattern can be indexed on a tetragonal unit cell with <italic>a</italic> 10&#x00B7;48 and <italic>c</italic> 3&#x00B7;023 &#x00C5;. This cell is shown to contain eight formula units of FeOOH but Cl<sup>-</sup> or other anions are necessary for the crystallization of the material The structure is that of hollandite or &#x03B1;-MnO<sub>2</sub>. The unit cell has been confirmed by electron diffraction from single crystals having dimensions about 5000 &#x00D7; 500 &#x00D7; 500 &#x00C5;. and twinning, which produces hexagonal stars, has been studied. On heating, the structure breaks down and recrystallizes as &#x03B1;-Fe<sub>2</sub>O<sub>2</sub>, probably with an intermediate stage involving a spinel phase.</p></abstract>
</article-meta>
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