Lab 6!!

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University of New Mexico, Main Campus *

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1110

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Geology

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Dec 6, 2023

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docx

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Lab 6 – Minerals: Gifts from the Earth 1. Two common minerals that are often misidentified for each other are plagioclase feldspar and potassium feldspar. Looking at both minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Plagioclase Feldspar: https://skfb.ly/6SYYO Potassium Feldspar: https://skfb.ly/6S68C These two minerals are similar in the fact that both have a glossy finish and the both present with a range of colors. But Potassium Feldspar has a lot more of a red tint and ranging red colors, while Plagioclase Feldspar is a white cream color. I think they are easy enough to distinguish between the two just based on the colors of each of them. 2. Two common minerals that are often misidentified for each other are amphibole and pyroxene. Looking at both minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Amphibole: https://skfb.ly/6UtON Pyroxene: https://skfb.ly/6SW8W Amphibole has distinct layers that can be seen, and it is very rigid. Pyroxene is also ridged. They both have similar color schemes. I would be very difficult to tell the difference between the two without having any other knowledge. Although Pyroxene does seem to look more like a granite. 3. The samples in the previous two questions have mineral cleavage, what is mineral cleavage? How can you tell if a sample has cleavage? All of the minerals seem to have been broken with a straight and not jagged edge. While an opposing side still is rough each of these have a clean flat break on another side. 4. Quartz is one of the most common minerals, describe what quartz looks like? Does it have cleavage? What unique properties does quartz have? Quartz: https://skfb.ly/6RzQJ Quartz is not smooth but lumpy on every side. There Is not a smooth edge or break. Quarts does not have any cleavage. Quarts is harder than glass and can have an electric charge which is quite unique. 5. Quartz can often be found in many different types of colors, such as rose quartz, amethyst, citrine, etc. Why does this happen? Can you rely solely on color to identify minerals? What else can you use outside of color to identify minerals? Color is very misleading because minerals can be found in many different colors. Quartz has many different color variations due to other minerals getting mixed in and changing the makeup of that quart. Another way to make to identify a mineral is to run it across a white ceramic plate and seeing the residue that is left behind. 6. Sometimes color can be useful for identifying minerals, what is a way in which you can routinely identify this mineral? (Hint, think about the name of the mineral) Olivine: https://skfb.ly/6TGo7 A way to routinely identify this mineral is by its color. It usually has an olive-green hue that makes it standout compared to other minerals, and makes it hard to misidentify.
7. Garnet often identified by its octohedryal crystal shape. How can you distinguish between a crystalline face and cleavage? Garnet: https://skfb.ly/6qw6I Crystalline and cleavage are smooth, but one have small break in it that the other one doesn’t. 8. Two common minerals that are often misidentified for each other are muscovite and biotite. Looking at both minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Muscovite: https://skfb.ly/6RMTF Biotite: https://skfb.ly/6TZMV Both of these minerals are flat with rigid parts around the outside. But they do have a distinction in color. Biotite is much darker in pigment than Muscovite is. Muscovite has perfect striking for cleavage that Biotite doesn’t have. 9. Halite, Calcite, and Gypsum are three minerals that look similar? Looking at these minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Do they have unique diagnostic properties? Halite: https://skfb.ly/M8U8 Calcite: https://skfb.ly/6UtDQ Gypsum: https://skfb.ly/6SZoI All three of these minerals have a light white cream color to them. But Halite is the only one with a shiny glossy finish. Gypsum is very dull, and has a lot of striking. Calcite is white but with red within is has the step-like parts perfect for cleavage. 10. Another mineral often mistaken for calcite by appearance is fluorite, how can you tell if a mineral is fluorite? Fluorite: https://skfb.ly/6TpTp Fluorite is similar to Calcite at first glance. But it lacks step-like properties and is much darker in color than Calcite. It has purple while, Calcite has red. 11. Two common minerals that are often misidentified for each other are pyrite and chalcopyrite. Looking at both minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Pyrite: https://skfb.ly/6TKJr Chalcopyrite: https://skfb.ly/6RFJE I do not understand how these two could be misidentified. Based purely on there appearance one looks similar to sand. With the appearance of a grain texture. While the other is glossy and appears metallic. These don’t look anything alike. 12. Two common minerals that are often misidentified for each other are galena and graphite. Looking at both minerals, in what ways are they similar? In what ways are they different? What can you use to tell them apart? Galena: https://skfb.ly/HV8V Graphite: https://skfb.ly/6DOvt Galena and Graphite are both dark grey. But Graphite has a metallic look and leaves a metallic streak. Galena has gold specks within the creases that are rather shiny but the rest of the mineral is rather dull.
13. Halite often breaks into square pieces, look at the molecular structure of halite to describe why it breaks into these shapes? 3D model of chemical structure of halite, the larger green balls are Cl atoms and the smaller grey balls are Na atoms: https://skfb.ly/66rpT Looking at the atomic chemical structure the mineral is built completely in a square form. The inner make up is not circular or round whatsoever. The only possible way for it to break is into square pieces. 14. The composition of each mineral gives it unique properties. The orientation of the atoms also impacts the properties of the mineral. For example, Graphite is very soft, so soft that we use it to mark paper (Typically we refer to this as “pencil lead” because originally pencils used to contain a lead mineral Galena in them). In contrast, diamonds are very hard, so hard that we use them to line things like drill bits and saw blades. Both items have the same chemical composition, C, but have very different properties. Explain why graphite is softer than diamonds? 3D model of graphite atomic structure: https://skfb.ly/AOF7 3D model of diamond atomic structure: https://skfb.ly/EG9W Diamonds, makeup is much more condensed. And tightly knit together, where graphite is spread out and has lots of room for movement in between atoms. 15. Color is not always a useful property for mineral identification. The samples at this station are all examples of the mineral hematite. Their different appearance is the result of the different environments in which they formed. Nonetheless, every sample of hematite has one reliable diagnostic property that will always tell you what it is. What is that diagnostic property? Earthen Hematite: https://skfb.ly/6utYX Specular Hematite: https://skfb.ly/6UqTP Hematite is translucent which helps to identify what it is without misidentifying it for something else. It also has a metallic luster that makes it slightly shimmer. 16. Magnetite is our society’s other major source of iron. You are hired as a mine engineer to design a process to extract magnetite iron ore out of a crushed rock. How would you extract out the magnetite iron ore? 3D model of magnetite: https://skfb.ly/6AyyF Video demonstration of magnetite with a magnet: https://youtu.be/Yf9Q4fFyrcc To extract the magnetite, they would place a magnate over the crushed rock and the magnetite will stick to it, so it can easily be lifted away. It having a magnetic charge makes this process much easier. 17. Although gypsum is no longer a component in most modern toothpastes, it is still widely used throughout our society. The average American home contains tons of gypsum in the form of dry wall as it has flame retardant properties. What about the chemical composition of gypsum (CaSO 4 · 2H 2 O) gives it theses flame retardant properties? Gypsum has water properties within which help to make the chemical compound fire resistant. .
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