Teacher Notes
|
||||
---|---|---|---|---|
Mineral Crystal Shapes![]() IntroductionIn this activity, paper crystals will be constructed to illustrate and enhance students’ knowledge of different crystal shapes. The constructed paper crystals will then be compared to actual mineral samples. Concepts
MaterialsAragonite, 2*
Ballpoint pen Felt-tipped markers (optional) Glue, tape or paper cement Gypsum, 2* Halite, 2* Index card Master sheets of unit cell lattice models (cubic, hexagonal, monoclinic, orthorhombic, tetragonal, triclinic)* Paint Plagioclase, 2* Quartz, 2* Ruler Scissors Zircon, 2* *Materials included in kit. Safety PrecautionsWash hands thoroughly with soap and water after handling mineral samples. Follow all laboratory safety guidelines. DisposalAssembled paper crystal shapes, paper crystal worksheets and minerals may be saved for future use. Prelab PreparationMake as many copies of the unit cell lattice model worksheets on white or colored paper as needed. Cut out and assemble each unit cell lattice model using the patterns and assembly instructions provided. Assembly Instructions for Crystal Lattice Models
Procedure
Teacher Tips
Correlation to Next Generation Science Standards (NGSS)†Science & Engineering PracticesDeveloping and using modelsDisciplinary Core IdeasMS-PS1.A: Structure and Properties of MatterHS-PS1.A: Structure and Properties of Matter Crosscutting ConceptsSystems and system modelsStructure and function DiscussionMinerals crystallize in a series of distinct crystal lattices based upon the sizes of the atoms, molecules or ions present, their shapes, charges and the number of each present. These crystal lattices are formed by a regular repeated pattern of atoms which are connected together called unit cells. Unit cells are the basic repeated building blocks of minerals. In many materials, the arrangements of atoms are very random. Minerals, however, crystallize in a highly regular and ordered manner. Because of this ordered repetitive nature, minerals take on very distinct and interesting shapes. Individual crystal lattices can be classified using a relatively small number of basic unit cells. The following table shows the basic unit cell structures and how they are formed. A mineral example for each unit cell is also given. {11943_Discussion_Table_2}
ReferencesGross, G.; Colangelo, E.; Holzer, M. A Demo A Day™—A Year of Earth Science Demonstrations; Flinn Scientific Inc.: Batavia, IL, 2001; pp 106–113. Recommended Products
|
||||