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                <text>&lt;h2&gt;Plagioclase feldspar&lt;/h2&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Na[AlSi&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;8&lt;/sub&gt;] – Ca[Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;8&lt;/sub&gt;]&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Framework silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;triclinic (+) (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in hand specimen:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; white&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Cleavage:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; two at 90°&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Hardness:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 6-6.5&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;none&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;low&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;~0.010, 1&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt; &lt;/span&gt;order grey&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Extinction:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;inclined&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Twinning:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;lamellar, very common&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;strong&gt;&lt;span&gt;M403 &lt;/span&gt;&lt;/strong&gt;&lt;strong&gt;&lt;span&gt;Plagioclase feldspar, oligoclase&lt;/span&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;strong&gt;Ytterby&lt;/strong&gt;&lt;strong&gt;, Sweden&lt;/strong&gt;&lt;strong&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;A cleavage fragment of white plagioclase feldspar&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Pearly lustre on cleavage planes&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Two sets of cleavage at 90°&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Fine parallel striations due to lamellar twinning&lt;/p&gt;
&lt;p class="NoSpacing"&gt;&lt;strong&gt;&lt;span&gt;M404 &lt;/span&gt;&lt;/strong&gt;&lt;strong&gt;&lt;span&gt;Plagioclase feldspar, labradorite&lt;/span&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;strong&gt;Labrador&lt;/strong&gt;&lt;strong&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Dark grey, light where fragments are small due to cracking along cleavage&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Schiller (blue iridescence), characteristic of labradorite&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Very fine parallel striations due to lamellar twinning&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l100"&gt;L100 Alkali granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l101"&gt;L101 Granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l102"&gt;L102 Hornblende biotite granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l112"&gt;L112 Rhyolite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l120"&gt;L120 Granodiorite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l130"&gt;L130 Andesite, porphyritic (porphyrite)&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l141"&gt;L141 Gabbro&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l162"&gt;L162 Basalt, porphyritic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l172"&gt;L172 Ultramafic cumulate&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/metamorphic-rocks/l504"&gt;L504 Garnet schist&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;span&gt;Plagioclase feldspar forms a continuous solid solution between the sodic endmember (albite, or Ab) and the calcic endmember (anorthite, or An). The series is sub-divided into albite (An&lt;sub&gt;0-10&lt;/sub&gt;), oligoclase (An&lt;sub&gt;10-30&lt;/sub&gt;) andesine (An&lt;sub&gt;30-50&lt;/sub&gt;), labradorite (An&lt;sub&gt;50-70&lt;/sub&gt;), bytownite (An&lt;sub&gt;70-90&lt;/sub&gt;) and anorthite (An&lt;sub&gt;90-100&lt;/sub&gt;).&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;plagioclase&lt;br /&gt;feldspar&lt;/div&gt;
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        <name>felsic</name>
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        <name>igneous</name>
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                <text>&lt;h2&gt;Clinopyroxene (augite)&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;(Ca,Mg,Fe&lt;sup&gt;2+&lt;/sup&gt;,Fe&lt;sup&gt;3+&lt;/sup&gt;,Ti,Al)&lt;sub&gt;2&lt;/sub&gt;[(Si,Al)&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;]&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Chain silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal&lt;/em&gt;&lt;em&gt;&lt;span&gt; &lt;/span&gt;system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;monoclinic (+)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in hand specimen:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; black&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Cleavage:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; two at 90°&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Hardness:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 5.5-6&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless, pale brown or pale grey&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;variable weak to moderate&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;moderate&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;0.018-0.033; 1&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt; &lt;/span&gt;order pink to 2&lt;sup&gt;nd&lt;/sup&gt;&lt;span&gt; &lt;/span&gt;order orange&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Extinction:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;inclined&lt;span&gt; &lt;/span&gt;&lt;em&gt;&lt;br /&gt;Twinning:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;simple, common&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l141"&gt;L141 Gabbro&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l161"&gt;L161 Basalt, amygdaloidal&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l162"&gt;L162 Basalt, porphyritic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l172"&gt;L172 Ultramafic cumulate&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;span&gt;Clinopyroxene contains calcium. It encompasses a range of solid solutions from (Mg,Fe)&lt;sub&gt;2&lt;/sub&gt;[Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;] to Ca(Mg,Fe)[Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;]. The physical and optical properties detailed above refer to augite, a clinopyroxene common in mafic igneous rocks.&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;clinopyroxene&lt;br /&gt;augite&lt;/div&gt;
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        <name>ultramafic</name>
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                <text>&lt;h2&gt;Orthopyroxene&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;(Mg,Fe)&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Chain silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;orthorhombic (+) (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in hand specimen:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; black &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Cleavage:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; two at 90°&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Hardness:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 5-6&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in plane polarised light: &lt;/span&gt;&lt;/em&gt;&lt;span&gt;colourless, reddish or greenish &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Pleochroism:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; variable weak to strong&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Relief:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; moderate &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Birefringence:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 0.007-0.020; 1&lt;sup&gt;st&lt;/sup&gt; order grey to 2&lt;sup&gt;nd&lt;/sup&gt; order purple&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Extinction: &lt;/span&gt;&lt;/em&gt;&lt;span&gt;straight&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;span&gt;Orthopyroxene has two end-member compositions: enstatite, Mg&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;, and ferrosilite, Fe&lt;sup&gt;2+&lt;/sup&gt;&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;6&lt;/sub&gt;.&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;orthopyroxene&lt;/div&gt;
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                <text>&lt;h2&gt;Olivine&lt;/h2&gt;</text>
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&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;(Mg,Fe)&lt;sub&gt;2&lt;/sub&gt;[SiO&lt;sub&gt;4&lt;/sub&gt;]&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Orthosilicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;orthorhombic (+) (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in hand specimen:&lt;/em&gt; pale green&lt;br /&gt;&lt;em&gt;Cleavage: &lt;/em&gt;none, instead it has characteristic curving cracks&lt;em&gt;&lt;br /&gt;Hardness:&lt;/em&gt; 7&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt; colourless&lt;br /&gt;&lt;em&gt;Relief:&lt;/em&gt; moderate &lt;br /&gt;&lt;em&gt;Birefringence:&lt;/em&gt; 0.035; 2nd order pink&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;strong&gt;&lt;span&gt;M100 Olivine&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;North Carolina&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;A mass of rather irregular crystals of olivine&lt;br /&gt;Yellow-green colour&lt;br /&gt;Vitreous lustre&lt;br /&gt;No cleavage&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l141"&gt;L141 Gabbro&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l162"&gt;L162 Basalt, porphyritic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l172"&gt;L172 Ultramafic cumulate&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;Olivine has two end-member compositions: forsterite, Mg&lt;sub&gt;2&lt;/sub&gt;[SiO&lt;sub&gt;4&lt;/sub&gt;], and fayalite, Fe&lt;sub&gt;2&lt;/sub&gt;[SiO&lt;sub&gt;4&lt;/sub&gt;]. The physical and optical properties detailed above refer to forsterite&lt;strong&gt;.&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;Forsteritic olivine is a common constituent of mafic and ultra-mafic rocks.&lt;br /&gt;Cracks are often filled with serpentinite alteration.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;olivine&lt;br /&gt;forsterite&lt;br /&gt;fayallite&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;L161&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Basalt, amygdaloidal&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Cenozoic&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Lava, Skye&lt;/p&gt;
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text five columns omega"&gt;
&lt;div class="element-text"&gt;
&lt;div class="element-text"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text five columns omega"&gt;
&lt;div class="element-text"&gt;
&lt;div class="element-text"&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
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&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Fine-grained, greenish black rock comprising dark and white minerals.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Contains&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/172"&gt;amygdales&lt;/a&gt;, mostly white, though some have black cores.&lt;/p&gt;
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&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Fine-grained plagioclase&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/215"&gt;laths&lt;/a&gt;&lt;span&gt; &lt;/span&gt;and irregular clinopyroxene (augite) grains, replaced with calcite. Many of the plagioclase laths have been almost entirely altered.&lt;/p&gt;
&lt;p&gt;The amygdales are filled with&lt;span&gt; &lt;/span&gt;&lt;span&gt;zeolite&lt;/span&gt;, growing in spherulitic and radiate patterns. Many have rims of calcite and fine-grained chlorite.&lt;/p&gt;
&lt;p&gt;Some vein material -&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/203"&gt;granular&lt;/a&gt;&lt;span&gt; &lt;/span&gt;quartz with&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/257"&gt;sutured contacts&lt;/a&gt;.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Fine-grained → rapid,&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/191"&gt;extrusive&lt;/a&gt;&lt;span&gt; &lt;/span&gt;crystallisation.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Gas bubbles trapped within lava produced&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/264"&gt;vesicles&lt;/a&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Circulation of fluids → precipitation of zeolite within the vesicles.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;span&gt;Zeolites&lt;/span&gt;&lt;span&gt; &lt;/span&gt;are produced at low temperatures. They are commonly precipitated in basaltic volcanic piles.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;amygdaloidal basalt&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;L141&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Gabbro&lt;/h2&gt;</text>
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&lt;div class="element"&gt;
&lt;div class="element-text five columns omega"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;Very dark grey, coarse-grained rock, typical grain size 1-2 mm.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Main mineral phases are black clinopyroxene, greenish olivine and pale grey feldspar. The rock is cross-cut by a small number of hairline white veins.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Plagioclase feldspar&lt;span&gt; &lt;/span&gt;&lt;br /&gt;-&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/258"&gt;Tabular&lt;/a&gt;&lt;span&gt; &lt;/span&gt;phenocrysts making-up ~50% of the rock. Characteristic&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/169"&gt;lamellar twinning&lt;/a&gt;. Some are&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/267"&gt;zoned&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;Olivine&lt;span&gt; &lt;/span&gt;&lt;br /&gt;-&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/236"&gt;Phenocrysts&lt;/a&gt;&lt;span&gt; &lt;/span&gt;have been extensively altered, rendering them almost unrecognisable. The olivine has decomposed to magnetite and serpentine. Relict olivine grains display characteristic curving cracks and&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/189"&gt;euhedral&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/206"&gt;form&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;Clinopyroxene (augite)&lt;span&gt; &lt;/span&gt;&lt;br /&gt;-&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/211"&gt;Interstitial&lt;/a&gt;&lt;span&gt; &lt;/span&gt;grains making-up ~35% of the rock.&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/241"&gt;Poikilitic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;texture. Inclined&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/190"&gt;extinction&lt;/a&gt;. Interference colours from first order pink to second order orange. Pale grey under plane polarised light. Some simple twinning.&lt;/p&gt;
&lt;p&gt;Accessory minerals&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Opaque, interstitial, probably magnetite.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Coarse grained → slowly cooled,&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/212"&gt;intrusive&lt;/a&gt;.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Hydrothermal&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/170"&gt;alteration&lt;/a&gt;&lt;span&gt; &lt;/span&gt;of olivine after crystallisation of the rock.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;gabbro&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
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