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<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.1964.033.267.04</article-id>
<title-group>
<article-title>Pumpellyite in Snowdonian Soils and Rocks</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Jenkins</surname>
<given-names>D. A.</given-names>
</name><degrees>B.A., Ph.D.</degrees>
<aff>Dept. of Biochemistry and Soil Science, University College of North Wales, Bangor</aff></contrib>
<contrib contrib-type="author">
<name><surname>Ball</surname>
<given-names>D. F.</given-names>
</name><degrees>M.A.</degrees>
<aff>The Nature Conservancy, Penrhos Road, Bangor</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1964</year>
</pub-date>
<volume>33</volume>
<issue>267</issue>
<fpage>1093</fpage>
<lpage>1096</lpage>
<copyright-statement>Copyright &#x00A9; 1964, The Mineralogical Society</copyright-statement>
<copyright-year>1964</copyright-year>
<abstract>
<title>Summary</title>
<p>Detrital grains, noted during the mineralogical examination of certain Snowdonian soils, have been identified as varieties of the mineral pumpellyite : the source of one variety has been located in dolerites exposed in the area, and the identity of this variety confirmed by X-ray analysis.</p></abstract>
</article-meta>
</front>
</article>
