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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.1941.026.175.01</article-id>
<title-group>
<article-title>On a Crystal of Augelite from California</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Peacock</surname>
<given-names>M. A.</given-names>
</name><degrees>M.A., Ph.D., D.Sc.</degrees>
<aff>Associate Professor of Mineralogy, University of Toronto</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Moddle</surname>
<given-names>D. A.</given-names>
</name><degrees>M.A.</degrees>
<aff>Ontario Department of Mines.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1941</year>
</pub-date>
<volume>26</volume>
<issue>175</issue>
<fpage>105</fpage>
<lpage>115</lpage>
<copyright-statement>Copyright &#x00A9; 1941, The Mineralogical Society</copyright-statement>
<copyright-year>1941</copyright-year>
<abstract>
<title>Summary</title>
<p>A large well-formed crystal of augelite from the andalusite deposit on White Mountain, Mono Co., California, shows the forms <italic>c</italic>(001), <italic>b</italic>(010), <italic>a</italic>(100), <italic>j</italic>(130), <italic>k</italic>(120), <italic>l</italic>(230), <italic>m</italic>(110), <italic>s</italic>(210), <italic>t</italic>(310), <italic>r</italic>(021), <italic>f</italic>(201), <italic>x</italic>(<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>2</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>01</mml:mn></mml:mrow></mml:math></inline-formula>), <italic>n</italic>(111), <italic>p</italic>(221), <italic>o</italic>(<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>11</mml:mn></mml:mrow></mml:math></inline-formula>), with <italic>a : b : c</italic> = 1&#x00B7;6419 : 1 : 0&#x00B7;6354, <italic>&#x03B2;</italic> = 112&#x00B0; 26<inline-formula><mml:math><mml:mrow><mml:mstyle scriptlevel='+1'><mml:mfrac><mml:mn>1</mml:mn><mml:mn>2</mml:mn></mml:mfrac></mml:mstyle></mml:mrow></mml:math></inline-formula>
&#x2032; (Spencer, in the structural setting); the forms <italic>j k l s t p</italic> are new or confirmatory. Cleavages (110), (<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>2</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>01</mml:mn></mml:mrow></mml:math></inline-formula>), also new (001), (<inline-formula><mml:math><mml:mrow><mml:mover><mml:mn>1</mml:mn><mml:mo>&#x00AF;</mml:mo></mml:mover><mml:mn>01</mml:mn></mml:mrow></mml:math></inline-formula>). Spencer's optical orientation is confirmed; Z (acute bisectrix): <italic>c</italic> = +34 <inline-formula><mml:math>
<mml:mrow>
<mml:mstyle scriptlevel='+1'>
<mml:mfrac>
<mml:mn>1</mml:mn>
<mml:mn>2</mml:mn>
</mml:mfrac>
</mml:mstyle>
</mml:mrow>
</mml:math>
</inline-formula>&#x00B0; 2V = 52&#x00B0;. The unit cell with <italic>a</italic> 13&#x00B7;10, <italic>b</italic> 7&#x00B7;96, <italic>c</italic> 5&#x00B7;06 &#x00C5;., <italic>&#x03B2;</italic> = 112&#x00B0; 26 <inline-formula><mml:math>
<mml:mrow>
<mml:mstyle scriptlevel='+1'>
<mml:mfrac>
<mml:mn>1</mml:mn>
<mml:mn>2</mml:mn>
</mml:mfrac>
</mml:mstyle>
</mml:mrow>
</mml:math>
</inline-formula> &#x2032;, contains 4[Al<sub>2</sub>PO<sub>4</sub>(OH)<sub>3</sub>]. The space-group obtained from the morphology by Donnay's law, and independently from the X-ray extinctions, is <inline-formula><mml:math><mml:mrow><mml:msubsup><mml:mrow><mml:mi>C</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn><mml:mi>h</mml:mi></mml:mrow><mml:mrow><mml:mn>3</mml:mn></mml:mrow></mml:msubsup><mml:mo>&#x003D;</mml:mo><mml:mi>C</mml:mi><mml:mn>2</mml:mn><mml:mo>&#x2215;</mml:mo><mml:mi>m</mml:mi></mml:mrow></mml:math></inline-formula>, accepting the holohedral class indicated by the absence of pyroelectricity (Martin's method). The X-ray powder spectrum is reproduced and partially indexed.</p></abstract>
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