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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Form&lt;/h2&gt;</text>
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                <text>&lt;em&gt;See&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/206"&gt;habit&lt;/a&gt;.&lt;/em&gt;</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Foliation&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This refers to any pervasive planar feature in a rock. It is produced by the arrangement of the constituent grains into sheet-like structures, usually in compositionally distinct layers. Foliations can be primary (e.g. bedding, fissility, flow banding) or secondary (e.g. cleavage).&lt;/span&gt;</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Flow banding&lt;/h2&gt;</text>
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                <text>This occurs when an inhomogeneous magma flows, thereby drawing out the inhomogeneities into bands of different compositions. When this happens on a very fine scale it is called flow lamination.</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Fissility&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This refers to the tendency of some sedimentary rocks to break along their bedding planes. Shales are fissile. Fissility is distinct from cleavage because cleavage is not aligned with the bedding planes.&lt;/span&gt;</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Fibrous&lt;/h2&gt;</text>
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                <text>&lt;span&gt;This texture consists of a mass of fine strand-like crystals. It often occurs in igneous rocks which have undergone rapid cooling.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Ferromagnesian mineral&lt;/h2&gt;</text>
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                <text>&lt;span&gt;A silicate mineral containing a high proportion of iron and/or magnesium. These minerals tend to be dark in colour. Common ferromagnesian minerals include olivine, pyroxenes, amphiboles, biotite mica and garnet.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Facetted&lt;/h2&gt;</text>
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                <text>A facetted crystal has a number of planar surfaces called faces. These are produced during the growth of the crystal.</text>
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                  <text>This glossary describes a number of geological terms with which the 1A students should become familiar.&lt;span&gt; It is by no means an exhaustive list, but is aimed to help you understand the material within the first year course.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Fabric&lt;/h2&gt;</text>
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                <text>&lt;span&gt;The fabric of a rock describes the geometric arrangement of its constituent grains. The term is most commonly applied to metamorphic rocks. These may display either linear or planar fabrics, depending on the deviatoric stresses present during their formation.&lt;/span&gt;</text>
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                <text>&lt;h2&gt;Extrusive&lt;/h2&gt;</text>
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                <text>&lt;span&gt;Rocks which have formed by the eruption of igneous material onto the surface of the Earth are described as extrusive.&lt;/span&gt;</text>
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                <text>&lt;em&gt;Compare with&lt;span&gt; &lt;/span&gt;&lt;a href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/212"&gt;intrusive&lt;/a&gt;.&lt;/em&gt;</text>
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                <text>&lt;h2&gt;Extinction&lt;/h2&gt;</text>
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                <text>&lt;span&gt;As a mineral grain is rotated under cross-polarised light it will periodically turn black. When the grain is black it is in extinction. The extinction positions occur at every 90° of rotation. This position is measured in degrees from a prominent feature of the mineral grain, such as a cleavage plane or a face of a euhedral crystal.&lt;/span&gt;</text>
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