...1-7. Keep track of which mineral you are working with as you record your observations. 2. Record your observations of each test in Part 1 of this worksheet. Refer to the job aids in the upper-right corner of the test screens to help you interpret what you observe. 3. Identify the minerals by comparing your observations with the Associate Program Material: Mineral Identification Worksheet. Write the name of each mineral in Part 2 of this worksheet. The minerals are numbered to conceal their identities, but they will include seven from the following list. To help you identify them, refer to the Mineral Identification Job Aid. • Borax • Calcite • Corundum • Graphite • Gypsum • Orthoclase feldspar • Pyrite • Quartz • Talc • Topaz 4. Identify two evolutionary processes of Earth, and explain them in Part 3 of this worksheet. 5. Post this worksheet as an attachment to your Assignments link. Delete the introductory instructions in this worksheet before you submit it to your instructor. Part 1: Recording Observations In the following chart, record your observations of each test for the seven minerals. After you have completed all tests, name the minerals in Part 2 of this worksheet. An example of how to fill out the chart is illustrated follows. |Recorded Observations for Minerals 1-7 ...
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...Joesmithite The Joesmithite mineral was named after Joseph Victor Smith. Joseph Victor Smith was born in 1928 and later died in 2007. As a young boy on his parents farm north of England, Joseph Victor Smith often wondered why part of the moon was white and part of it was black. In Dec of 1969 the question that often pondered his mind as a child began to once again trouble him. He reached a conclusion that the black material was basalt, this is no more than solidified lava. Additionally, Smith reached the verdict that the white color in the moon was rock enriched with feldspar. It was Smith determination the feldspar crystals, being lighter than that of basalt, floated to areas of the moon when part of the planet was melted lava. Joseph Victor Smith endured much criticism for his theory but during an interview in 1999 he noted that his theory of the hot moon had much more effect and support over the theory of cooler models. Smith had an overwhelming concern for our environment and the preservation of the earth. In the 1980’s his concern for threats to the human race presented by the earth (comets, colliding, asteroids and other natural hazards) within a combination of articles and conferences. Smith received the Roebling Medal in 1982 and in 1998 he organized the National Academy of Sciences Colloquium on Geology, Mineralogy, and Human Welfare. Smith documented more than 400 scientific articles that where published in journal such as Science, Nature, Journal of Geology...
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...iI chose to write about the mineral, Kaolinite. Kaolinite, also known as China clay, Kaolin, and White Clay is a very fine mineral. The chemical composition of Kaolinite is Al2Si2O5(OH)4. Kaolinite is used in a variety of materials such as paper, concrete, and paint. Kaolin is used in one of the most important pieces of equipment I have as a medic in the Army, Combat Gauze. Kaolin is impregnated into Quick Clot Combat Gauze and is used to stop massive hemorrhaging in trauma patients. Kaolinite is formed from the weathering of minerals such as Feldspar. Kaolinite can be found on almost every continent with the exception of Antarctica. Kaolinite or Kaolin, gets its name from the Chinese hill from which it was mined for centuries (Kao-Ling). As a raw mineral Kaolinite is virtually worthless, it takes a long list of processes to get the desired material from kaolin and this makes mining for kaolinite and long a carefully chosen procedure. Companies who mine kaolinite drill hundreds of core samples over extremely large areas before giving the go ahead for an actual mine to be constructed. Companies who mine for Kaolin usually have more than one mine because the quality of the kaolinite can vary within a single deposit. Even though Kaolinite is so abundant, I would consider it to be an extremely important mineral as it is important for the manufacturing of such important day to day materials. Ralph, J., & Chan, I. (2014, March 30). Kaolinite. : mineral information and data...
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...What is granite made up of? It is a rock, not a mineral, so it is built up of several different minerals, which include; Mica, quartz, hornblende, magnetite, and feldspar. Although some may argue against the inclusion of magnetite and mica I firmly believe that those minerals are some of the most prominent appearing in granite. Mica and quartz are known to be metallic and have a low hardness on the Mohs scale. Both of which were exemplified by our sample of granite. Along with a slight magnetic pull that our granite gave off, implying that the granite included magnetite too. Not to mention the granite is partly grey (A similar shade to hornblende), proving that yet another mineral, hornblende, is included within granite. Feldspar is also...
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...Abstract Central Texas contains Precambrian rocks, which were exposed due to the Llano uplift. This paper looks further into the Devil’s Waterhole of Ink’s Lake to get a better understanding of the area. First the geology of the Llano uplift is studied to get a better understanding of how the rocks in the area were formed. The rocks in the area, which consists of Valley Springs Gneiss and Town Mountain Granite, are studied even further to see the composition of each and how each was formed. The Valley Spring Gneiss is split into amphibolite, biotite gneiss, quartz-feldspar gneiss, and quartzite. Each of the five different rock samples were observed and studied in the area to give us a better understanding of their compositions, how they were formed, and what their protoliths are. The Devil’s Waterhole of Ink’s lake is the area of focus in studying Precambrian rock. Throughout the Ink’s Lake region we will take focus on the Precambrian metamorphic rock that was exposed due to the Llano uplift. The Llano uplift contains some of the oldest rocks in North America and is exposed in Ink’s Lake, Texas. This is exposed due to the oceanic-continent collision, which drove the Llano uplift upward. After the weathering away of the younger rock on top, the currently exposed metamorphic rock is more easily observed. Following the Llano uplift exposure, there was an intrusion of the Town Mountain Granite, which we will also look further into. We also observe the areas reactions such as...
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...Part 1: Recording Observations In the chart below, record your observations of each test for the seven minerals. After you have completed all tests, name the minerals in Part 2 of this worksheet. An example of how to fill out the chart is illustrated below. |Recorded Observations for Minerals 1–7 | |Tests |Example |Mineral 1 | |Example: Fluorite |80% certain |I am almost certain this mineral is fluorite, but I am not completely sure. Fluorite and gypsum| | | |are both white, shiny, have white streaks, cleave, and show no reaction to acid. However, the | | | |specific gravity of this mineral is 3.18, which is higher than gypsum, so I am pretty sure it | | | |is fluorite. | |Mineral 1: Pyrite |95% ...
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...Tufa is a variety of limestone, formed by the precipitation of carbonate minerals from ambient temperature water bodies. | Arkose is a detrital sedimentary rock, specifically a type of sandstone containing at least 25% feldspar. | Syenite a coarse-grained gray igneous rock composed mainly of alkali feldspar and ferromagnesian minerals. | Tephrite is an igneous, volcanic (extrusive) rock, with aphanitic to porphyritic texture. | Monolith a large single upright block of stone, especially one shaped into or serving as a pillar or monument. | Peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. | Amphibolite is a coarse-grained metamorphic rock that is composed of amphibole minerals and plagioclase feldspar. | Magnetite is a mineral and one of the three common naturally-occurring oxides of iron. | Rhyolite is an igneous, volcanic rock, of felsic (silica-rich) composition (typically > 69% SiO2 | Pelite is a term applied to metamorphic rocks derived from a fine-grained sedimentary protolith. | Turbidite a type of sedimentary rock composed of layered particles that have originated from the oceans. | Siltstone is a sedimentary rock which has a grain size in the silt range, finer than sandstone and coarser than claystones. | Pumice is a light-colored, extremely porous igneous rock that forms during explosive volcanic eruptions. | Limestone is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of...
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...DESIGN OF A GLASS TANK FURNACE AIM- Design of a regenerative and fired glass tank furnace of 200ton per day capacity to produce a sheet glass using furnace oil as fuel melted at 1500oC. Given composition of the sheet glass- Sio2 Al2O3 CaO MgO R2O Fe2O3 71 0.4 9 3 16 0.6 DIFFERENT PARTS OF A GLASS TANK FURNACE. 1. Doghouse assembly 2. Melting end 3. Crown 4. Bridge 5. Conditioning and Refining end 6. Regenerators 7. Portsland Burneses 8. Bubblers 9. Temprature Measurments 10. Furnace video camera 11. Furnace cooling System 12. Furnace exhust system 13. Auxillary System Sl.NO. | Refractories | Using Area | Properties | 1. | AZS(alumina-zirconia-silica) | Glass contact zone | 1. High corrosion resistance up to 1600 degree Celsius 2. AZS contains:- Alumina= 46 - 50% Zirconia= 33 - 41% Silica = 12 - 16% | 2. | Siliminite | Used in the back up layer of AZS | 1. High CCS and RUL value 2. High corrosion resistance 3. High refractorinessAlumina =42 – 63% | 3. | Fire clay | Used in the lower temperature zone such as flue line | It is also Aluminosilicate compound but it contains less amount of Alumina. | 4. | Insulation | Exterior area of furnace | It is also aluminosilicate material containing high porosity. | 5. | Zircon ramming mass | Furnace bottom | These...
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...Shiny Shiny Shiny Specks Specific Gravity 3.18 5.1 2.8 2.7 2.6 2.65 2.4 2.2 Cleavage & Fracture Cleavage Fracture Fracture Cleavage Fracture Fracture Cleavage Fracture Hardness 4 3.1-5.4 1-2.9 1-2.9 3.1-5.4 6.1-10 1-2.9 1-2.9 Acid No Reaction No Reaction No Reaction Active bubbling and Fizz No reaction No reaction No Reaction Light bubbling and fizz Part 2: Naming the Minerals Name the minerals in the following table. Then, insert a percentage of how certain you are in your identification. Finally, explain your percentage of certainty: What was confusing about this mineral? What other minerals do you think it could be? Remember, the minerals include seven of the following: borax, calcite, corundum, graphite, gypsum, orthoclase feldspar, pyrite, quartz, talc, and topaz. Identification of Mineral Percent Certain Explanation of Certainty Example: Fluorite 80% certain I am almost certain this mineral is fluorite, but I am not completely sure. Fluorite and gypsum are both white, shiny, have white streaks, cleave, and show no reaction to acid. However, the specific gravity of this mineral is 3.18, which is higher than gypsum, so I am pretty sure it is fluorite. Mineral 1: Pyrite 100% I am certain this mineral is pyrite because it is the only mineral listed on mineral identification worksheet that has a gold color...
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...Granite is made up primarily of three minerals: quartz, alkali feldspar (alumina and silica) and plagioclase feldspar (sodium and calcium). Granite may also contain additional minerals such as mica, hornblende and occasionally pyroxene. The Granite texture is very granular, and can come in many different colors ranging from white, pink, light or dark gray. The composition of Granite is felsic and is a very plentiful rock in the Earth's continental crust. The lighter density of the felsic composition lets the granite escape subduction, keeping this rock closer to the surface.https://en.wikipedia.org/wiki/Granite. The Pikes Peak Mountain Range is one home to this Intrusive rock. The Peaks formations that occurred were due to magma that has moved in a upward motion cutting across pre existing rock which creates forms known as plutons...
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...Versus All-Ceramic Crowns | | 14 | Conclusion | | 15 | References | | INTRODUCTION The word ceramic is derived from the Greek word keramos which literally means ‘burnt stuff’ but which has come to mean more specifically a material produced by burning or firing. The term ceramic refers to any product made from a non-metallic inorganic material usually processed by firing at a high temperature to achieve desirable properties. This material is opaque, relatively weak and porous and would be unsuitable for dental applications. It consisted mainly of kaolin. The more restrictive term porcelain refers to a specific compositional range of ceramic materials originally made by mixing kaolin (hydrated aluminosilicate), quartz (silica), and feldspars (potassium and sodium aluminosilicates), and firing at high temperature. Dental ceramics for metal-ceramic restorations...
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...track of which mineral you are working with as you record your observations. 2. Record your observations of each test in Part 1 of this worksheet. Refer to the job aids in the upper-right corner of the test screens to help you interpret what you observe. 3. Identify the minerals by comparing your observations with the Associate Program Material: Mineral Identification Worksheet. Write the name of each mineral in Part 2 of this worksheet. The minerals are numbered to conceal their identities, but they will include seven from the following list. To help you identify them, refer to the Mineral Identification Job Aid. • Borax • Calcite • Corundum • Graphite • Gypsum • Orthoclase feldspar • Pyrite • Quartz • Talc • Topaz 4. Identify two evolutionary processes of Earth, and explain them in Part 3 of this worksheet. 5. Post this worksheet as an attachment to your Assignments link. Delete the introductory instructions in this worksheet before you submit it to your instructor. Part 1: Recording Observations In the following chart, record your observations of each test for the seven minerals. After you have completed all tests, name the minerals in Part 2 of this worksheet. An example of how to fill out the chart is illustrated follows. |Recorded Observations for Minerals 1-7 ...
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...In addition to the radioactive minerals, there was also found niobium, molybdenum, some rare earths and the very rare and unusual thucholite. Plus a modest amount, (618 tons) of feldspar was harvested in 1925 the year McQuire & Robinson Radium & By Products Co. increased their stake to 50 acres. As for the uraninite mined, a few hundred pounds of it was sent to various museums (an example is ROM #M12500) and sold to collectors due to their high quality. In the end, Harry McQuire applied to the Lieutenant Governor of Ontario to surrender the charter for the McQuire-Robinson Radium and By-Product Limited as of April 1932. Several of the McQuire brother's land claims in the Lawson Bay area fell into tax arrears to be sold off by the government in 1939. Harry did better than his brother spending his later life in the upper class Forest Hill area of Toronto. The discovery of high grade uranium and thorium ores attracted 'rock...
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...Associate Level Material Comparison Worksheet Use the following table to compare extrusive and intrusive rocks. Describe and compare each type in at least 150 words. Extrusive Rock Intrusive Rock Extrusive rock refers to igneous volcanic rock formation in which hot magma from inside the Earth flows out to the surface as lava or explodes violently into the atmosphere to fall back as pyroclastic. This is different from intrusive rock formation, in which magma does not reach the surface. The main effect of extrusion is that the magma can cool much more quickly in the open air or under seawater, and there is less time for the growth of crystals. Often, some of the lava fails to crystallize at all, becoming an interstitial natural glass or obsidian. If the magma contains abundant volatile components which are released as free gas, then it may cool with large or small vesicles (bubble-shaped cavities) like those found in pumice or scoria. These rocks form many kilometers below the Earth’s surface, as molten rock called magma flows into cracks or underground chambers. There, the magma cools very slowly over thousands to millions of years. As it cools, elements combine to form common silicate minerals, the building blocks of igneous rocks; the mineral crystals can grow quite large if space allows. Rocks that form in this way are called intrusive igneous or plutonic rocks. The mineral crystals within them are large enough to see without a microscope. There are many different...
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... A mineral is homogenous, naturally occurring substance formed through geological processes that has a characteristic chemical composition, a highly ordered atomic structure and specific physical properties. Physical properties citrine rose quartz prasiolite 1. COLOR agate milky quartz amethyst smoky quartz jasper Physical properties The color of a mineral when it is powdered is called the streak of the mineral. Physical properties metallic adamantine glassy The luster of a mineral is the way its surface reflects light. pearly dull waxy Hardness-Mohs scale 1 talc 2 gypsum 3 calcite 4 fluorite 5 apatite 6 feldspar 7 quartz 8 topaz 9 corundum 10 diamond Cleavage Cleavage is the way a mineral breaks. one direction mica two directions feldspar three directions calcite Fracture Fracture is breakage that is not flat. The two main kinds of fracture are conchoidal (shell-shaped, as in quartz) and uneven. conchoidal Others… Heft is how heavy a mineral feels in the hand, an informal sense of density. Taste is definitive for halite (rock salt), of course, but a few other evaporite minerals also have distinctive tastes. What is a rock? A rock is a naturally occurring aggregate of minerals and/or other rock fragments Rock classification Igneous Sedimentary Metamorphic Igneous rocks Igneous rocks form when molten rock (magma) cools and solidifies, with or without crystallization...
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