Assignment 1 - Mineral Identification 10 week-1 (2)

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Raritan Valley Community College *

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157

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Geology

Date

Jan 9, 2024

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docx

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4

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Assignment 1 – Virtual Mineral Identification Introduction Mineral identification is a necessary skill all geologist must poses. Essentially all modern day materials (not made from plants) are made with minerals that had to be identified in the field in order to be extracted, processed, and repurposed as human technology. While you complete the lab, thinGF broader about each mineral, how did it most likely form? What group does it belong to? What environment might we find that mineral forming today? Part 1 - Pre-lab exercise (4 points) In your own words, provide a definition for the following mineral properties. Mineral Property Definition Color The hue of the rock (yellow, purple, magenta, etc..) Streak The hue of the rock when powdered Hardness Resistance to being damaged Cleavage Breaking the mineral along the weak spot to get an even split Crystal Form The shape of the crystal Fracture a broken piece of the mineral not placed along the Cleavage Luster Light relfelcted off mineral Part 2 – Mineral Identification (4 points)
Visit http://profharwood.x10host.com/GEOL101/Labs/Minerals/index.htm and read the introductory instructions. Familiarize yourself with how the virtual lab works by experimenting with a few samples prior to getting started. Once familiar, use the virtual lab to identify mineral samples and complete the table located below. (You only need to do the first 12). Sample Number Color Streak Hardnes s Clea vage Crystal Form Fracture Luster Other Mineral Name 1 White White 2 1 none irregular non- metallic none Gypsum 2 red brown white 7 0 none conhoidal non- metallic none Garnet 3 yellow/gol d gray 6 0 pyrittohedron irriegular metallic magneti c pyrite 4 clear white 7 0 hexagonal con non none Quartz 5 red brown white 9 0 hexagonal conhoidal non none corundum 6 grey white 6 2 none irreg non none plagioclas e 7 grey grey 6 0 none irreg strong metallic magneti c magnetite 8 green white 5 1 hex con non none apatite 9 pink white 6 2 none irreg non none orthoclase 10 clear white 2 3 cubic con non salty halite 11 clear white 2 1 none irreg non none muscovite 12 green white 7 0 none con non bobe olivine Part 3 Post Lab Reflection (12 points) 1. Pretend you are a professional geologist taking your RVCC student intern on a hunt for bauxite for the aluminum industry. Describe in detail how you would go about training the young intern while identifying bauxite in the field among other rocks. Remember, in the field, rocks and minerals weather, become covered in biological material, and or oxidize.
To find bauxite the first step is understanding where it is located, bauxite is located near tropical and subtropical regions. Looking up geological surveys conducted by government agencies to find information on the specific place that contains bauxite. Conduct a field survey to look for sign of weathered rock and use sensing technology like satellite images. 2. Of the minerals identified in the lab exercise, which are you most likely to find in a dried sea bed? Explain why each mineral has the possibility to exist in this location AND how you would be able to tell the difference between them. Dried sea beds provide exceptional mineral making material beause of the evaporation of water. The mineral that could be found is halite and gypsum the dissolved water evaporates and the salt form the crystals. They can appear in different shapes due to impurities. 3. Reflect on the mineral identification lab, select three minerals that stood out to you. Explain what critical thinking and data analysis skills you used in order to identify that mineral. Pyrite, often referred to as "fool's gold," has a brassy yellow color and metallic luster. It forms cubic crystals and can also appear as irregular masses. One of its key features is its hardness; it scratches easily and leaves a greenish-black streak when rubbed against a rough surface. Quartz, on the other hand, comes in a variety of colors and crystal shapes, but it is commonly recognized for its hexagonal prismatic crystals and a hardness of 7 on the Mohs scale, meaning it can scratch glass. Quartz is also often transparent or translucent, allowing light to pass through. Halite, or rock salt, typically occurs as colorless or white cubic crystals. It has a hardness of 2.5 on the Mohs scale and is easily scratched by a fingernail. A distinctive characteristic of halite is its salty taste; if you were to lick it, it would taste salty, providing a
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quick and unique way to confirm its identity. By paying attention to these specific traits, geologists can accurately differentiate between pyrite, quartz, and halite in various geological settings.