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Rocks are made of minerals and, as minerals are natural crystals, the geological world is mostly a crystalline world.

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Description

This course, Minerals and the crystalline state, introduces the study of minerals and crystal structures, using online text and interactive activities, including questions and answers, video clips, slidecasts and a Digital Kit.

Course learning outcomes

After studying this course, you should be able to:

  • give, with an appropriate example, the meaning of the terms phase, phase boundary and phase transformation, and interpret stability fields in terms of pressures and/or temperatures using a phase diagram
  • describe and recognise, giving examples, various physical properties of minerals, including lustre, cleavage, hardness and density
  • describe, giving mineral examples, the main differences between metallic, ionic and covalent structures and their type of bonding
  • explain the significance of various types of defects in crystals
  • explain the meaning of the terms lattice, unit cell, reflections and rotational symmetry, and how these relate to crystal systems.

Course content

  • Minerals and the crystalline state Unlimited

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Open University UK
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