FAIRLY SIMPLE GEOLOGY EXERCISES for STUDENTS AND THEIR TEACHERS |
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FAIRLY SIMPLE MINERAL IDENTIFICATION EXERCISE John J. Thomas Purpose An exercise in the identification of minerals that uses minerals with very distinct characteristics. The students will learn the characteristics of minerals and the process of identification. They will practice with the properties one uses in mineral identification. They will also learn how to use a simple identification chart. This exercise is designed so that the student has success. The worksheet at the end can be done either by first identifying the minerals and then doing the worksheet or by skipping the actual identification and simply using the Mineral Identification Chart to fill in the worksheet. Definitions
Teacher Information This exercise is designed so that the student has SUCCESS. The minerals all have distinct properties. The only mineral descriptions on the Identification Chart are those of the minerals they (and you) will have in front of them. All of the definitions are probably strange to you. The following is a more detailed description of each of these properties and the techniques for testing them. Hardness - how hard materials are. The hardness is defined by Moh's Scale of Hardness. Moh's scale uses ten common minerals ranging from talc (1, the softest) to diamond (10, the hardest). The steps from 1 to 10 are not a regular step scale (diamond is about 100 times as hard as the #9 mineral). There are hardness kits that can be used for testing hardness, but they are unnecessary. We have very nice testers around us:
You test hardness by scribing the mineral the way you would draw a line. Run your fingernail along the mineral as though the mineral is hard fudge and your fingernail is a knife you are using to cut it. Don't pick at it. Then scratch across the cut line. If you scratched it with your hardness tester, you will feel a notch. The harder the mineral the more you may have to lean into it to scratch it. Don't be afraid! You will not hurt it. The ease of making a scratch lets you decide how hard the mineral is. For example, if you can scratch a mineral easily with your fingernail, it has hardness 1. If it is quite difficult to scratch, 2, not hard and not easy = 1 1/2. If you can just barely scratch the mineral, 2-2 1/2. Check yourself by seeing how hard it is to scratch the same mineral with the penny. Luster - the way that anything reflects light. The scale that we use is a subjective one, but it is quite usable, especially at the opposite ends of the range. This exercise uses a simple one from the following examples:
Color - exactly that. The color of the mineral. This is the least diagnostic characteristic of a mineral (sorry for the bad news). Quartz, for example, can be clear, white, gray (smoky quartz), almost black, purple (amethyst), green, yellow, and pink (rose). Sometimes color is the only thing you have to use. Streak, which is the color of the mineral when it is powdered, is always a correct color. Cleavage - the way a mineral splits. Mica (biotite and muscovite) are excellent examples of this. Take a piece of mica and peel the sheets apart. This is cleavage. Watch the students with the mica or they will reduce your samples to a pile of very small flakes. Special Properties - these are properties of minerals specific to one or two minerals. Examples are:
Return to the top of the web page. Materials
Sources of materials - both of these suppliers are good, helpful, and quick. Their catalogs are free and are neat!
Return to the top of the web page. Student Exercise Give a sample of each of the minerals on the equipment list to your students (we usually let them work in pairs) and let them identify each of them. Give them each a copy of the identification chart and the identification sheet to help them with the identification. You will have to go over each of the properties of minerals so that they will understand them. Test the hardness of all of them. Do the luster of kaolinite (dull) and biotite (metallic). Have them describe the color of each. Let them split the biotite and learn what cleavage is. Show them some special properties such as the fizz of calcite. Let them feel talc, smell kaolinite, and taste halite. Then give them the worksheet and let them follow the trail of the geologist. Return to the top of the web page. MINERAL IDENTIFICATION CHART
Return to the top of the Mineral Identification Chart. Return to the top of the web page. MINERAL IDENTIFICATION SHEET Mineral # ____ Mineral # ____ Mineral # ____ Return to the top of the web page. MINERAL WORKSHEET Barbara R. Thomas The last letter of one word becomes the first letter of the next word. Example: scratch heavy (scratch heavy). The number of spaces indicates the number of letters in the answer. Clues _ _ _ _ _ _ A gray mineral that is softer than a nail, but harder than a fingernail. _ _ _ _ Makes calcite fizz. _ _ _ _ Kaolinite does not shine. It is ________. _ _ _ _ _ Kaolinite, talc, and gypsum are _______ colored. _ _ _ _ A mineral that feels greasy. _ _ _ _ _ Often used to tell minerals apart. _ _ _ _ _ A geologist studies them. _ _ _ _ Halite tastes like ________. _ _ _ _ Biotite forms ________ sheets. _ _ _ _ Used to test how hard a mineral is. Return to the top of the web page.
Barbara R. Thomas The last letter of one word becomes the first letter of the next word. Example: scratch heavy (scratch heavy). The number of spaces indicates the number of letters in the answer. Clues G A L E N A A gray mineral that is softer than a nail, but harder than a fingernail. A C I D Makes calcite fizz. D U L L Kaolinite does not shine. It is ________. L I G H T Kaolinite, talc, and gypsum are ________ colored. T A L C A mineral that feels greasy. C O L O R Often used to tell minerals apart. R O C K S A geologist studies them. S A L T Halite tastes like ________. T H I N Biotite forms ________ sheets. N A I L Used to test how hard a mineral is. Return to the top of the Mineral Worksheet. Return to the top of the web page. An Adobe® Acrobat® PDF® copy of Mineral Identification is available by clicking on the link. If you do not have a copy of Adobe® Acrobat® Reader® for PDF® files, click on the link to download a free copy.
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