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Rock Candy
Rock Candy

... 1. Lay out your samples of candy and determine which are models of a mineral and which are models of rocks. Use the information below to help you decide: ROCKS are made of one or more minerals. This means that the material that makes up an individual rock or several samples of the same kind of rock ...
JEOPARDY - OH Anderson Elementary
JEOPARDY - OH Anderson Elementary

... heat and pressure, this makes anthracite a _____type of rock. ...
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... What are some of the hardest types rocks? ...
The Rock Cycle
The Rock Cycle

... Form when minerals precipitate from a solution or when a solution evaporates Limestone = calcite which grows together along with minerals and sediments  Rock salt – used in mfg. of glass, paper, soap and dairy products – also table salt ...
Rocks - staffordscience
Rocks - staffordscience

...  Proposed by James Hutton in the late 1700s.  Interactions among Earth’s water, air, land, and living things can cause rocks to change from one form to another  The continuous processes that cause rock to change make up the rock cycle ...
Weathering, Soil and Unstable Slopes
Weathering, Soil and Unstable Slopes

... Affect of Fracturing on Weathering • As a rock fractures and breaks apart there is an increase in the rate of weathering. • WHY?? • As a rock breaks into smaller pieces the surface area increases allowing more exposure to weathering. ...
Origin of Rocks
Origin of Rocks

... they are formed. • Igneous rocks: formed from the cooling of molten rock. • Sedimentary rocks: formed from sediments being compacted and cemented. • Metamorphic rocks: existing rock that is changed by heat, pressure, or chemical reactions. ...
GY 111 Lecture Note Series Lab 3: Introduction to Sedimentary Rocks
GY 111 Lecture Note Series Lab 3: Introduction to Sedimentary Rocks

... is due to “rusted iron”). Black shales form in areas where there is no oxygen (anaerobic environments) and there is plenty of organic material like swamps (the black colour is carbon). Green shales form in areas that are anaerobic but where organic material is not abundant (e.g., lagoons and estuari ...
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Chapter 6 Notes: Rocks

... Medium grays-green colors Coarse grained member Andesite ...
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... What are three examples of a mineral’s luster?(19) ___________, (20)_________________, and (21)_________________. 22. How do scientists measure the hardness of a mineral? 23. What is the softest mineral according to Moh’s scale? 24. What is the hardest mineral according to Moh’s scale? 25. What is a ...
Chapter Test C - Stout Middle School
Chapter Test C - Stout Middle School

... Answers will vary. Sample answer: Under a microscope a nonfoliated rock will not have mineral grains that are aligned. Answers will vary. Sample answer: Limestone is formed from the remains, or fossils, of animals that once lived in the ocean. Answers will vary. Sample answer: Rocks recrystallize wh ...
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What is Weathering

... C. Name one way igneous and sedimentary rocks differ. D. What type of natural rock does human-made concrete most resemble? II. The Rock Cycle A. Draw a diagram of the rock cycle. Label and describe each class of rock and the processes that form each B. What conditions are necessary in order for meta ...
Soil Mechanics Laboratory
Soil Mechanics Laboratory

... shape. The color, crystal size, and general appearance of quartz will vary greatly, so that a large number of varieties have been named. Regardless of color, crystal size, shape, mode of origin, etc., all quartz is characterized by a hardness of 7 (it will scratch glass and steel), conchoidal fractu ...
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... These are called fossils. Sedimentary rocks are usually made from individual grains of one or more types of rock, mineral or biological material which are stuck together by sediment “glue” – fine mud or silt particles – and minerals that have grown in the tiny spaces between the grains after they we ...
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Basalt - New Haven Science

... Sandstone is a sedimentary rock that sometimes looks like pieces of beach sand that have been glued together. The color and strength of sandstone vary. Some sandstones are soft, almost crumbly. The grains may be small, medium, or large. The edges may be rounded or sharp, depending on how much the ro ...
rock_id_lab
rock_id_lab

... (several kinds of mineral crystals are present); light colors (rich in quartz or feldspars); sometimes distinctive minerals are present such as olivine (green) or alkali feldspar (pink). Some ...
Science 8-Chapter 13HD Les 2 Notes Ans
Science 8-Chapter 13HD Les 2 Notes Ans

... ways that rocks form. Write the type of rock that forms in each box on the right. Parent rocks are squeezed, heated, or exposed to hot fluids. ...
Sedimentary Rocks
Sedimentary Rocks

... a. andesitic composition c. ultramafic composition b. basaltic composition d. granitic composition 3. A rock that forms when magma hardens beneath Earth’s surface is called an ____. a. intrusive metamorphic rock b. extrusive igneous rock c. intrusive igneous rock d. extrusive sedimentary rock Answer ...
Rocks and Minerals
Rocks and Minerals

... • Removal of “strips” of soil and rock to expose ore • Large volume of material is removed, resource extracted and the tailings are returned ...
TYPES OF ROCKS AND THEIR FORMATION
TYPES OF ROCKS AND THEIR FORMATION

... otherwise used up. This water leaves behind the minerals that it held in suspension or solution, which assist to cement the sediments into the solid mass called sedimentary rock. The process of formation of sedimentary rock is continuous and occurs over long periods of time. In some places on earth ...
Weathering Outline- Standards Teacher Copy
Weathering Outline- Standards Teacher Copy

... 2. Chemical: _Tranformation od rock into one or more NEW compounds. Which change the rocks composition: Example:rust__________________________________________________________ a. Water: Water will react chemically with the rocks _____________________________________________________________ b. Granite ...
Crystallization
Crystallization

...  Has a fixed chemical formula  Has an orderly crystalline structure  Over 4000 minerals!  But only eight groups commonly found in earth’s rocks. ...
GG 101L SEDIMENTARY ROCKS SUPPLEMENTARY READING
GG 101L SEDIMENTARY ROCKS SUPPLEMENTARY READING

... bed. Farther downstream, slower flow carries only pebbles. Even farther downstream there may be some sand, and eventually, when the stream has merged with other streams into a slow-flowing lazy river, only silt or clay will be transported. Of course the character of streams and rivers changes depend ...
Activity worksheet: Chocolate Geology
Activity worksheet: Chocolate Geology

... Does anyone remember the TV programme “Mighty Morphin’ Power Rangers”? How did these guys get their name? It was because they “morphed“ or changed from one thing into another. Think of a caterpillar. What happens to it? In a process called metamorphosis, it changes into a butterfly. So metamorphic r ...
Types of Rock
Types of Rock

... that has a banded appearance and is made up of granular mineral grains. It typically contains abundant quartz or feldspar minerals. ...
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Mudrock



Mudrocks are a class of fine grained siliciclastic sedimentary rocks. The varying types of mudrocks include: siltstone, claystone, mudstone, slate, and shale. Most of the particles are less than 0.0625 mm (1/16th mm or 0.0025 inches) and are too small to study readily in the field. At first sight the rock types look quite similar; however, there are important differences in composition and nomenclature. There has been a great deal of disagreement involving the classification of mudrocks. There are a few important hurdles to classification, including:Mudrocks are the least understood, and one of the most understudied sedimentary rocks to dateIt is difficult to study mudrock constituents, due to their diminutive size and susceptibility to weathering on outcropsAnd most importantly, there is more than one classification scheme accepted by scientistsMudrocks make up fifty percent of the sedimentary rocks in the geologic record, and are easily the most widespread deposits on Earth. Fine sediment is the most abundant product of erosion, and these sediments contribute to the overall omnipresence of mudrocks. With increased pressure over time the platey clay minerals may become aligned, with the appearance of fissility or parallel layering. This finely bedded material that splits readily into thin layers is called shale, as distinct from mudstone. The lack of fissility or layering in mudstone may be due either to original texture or to the disruption of layering by burrowing organisms in the sediment prior to lithification. From the beginning of civilization, when pottery and mudbricks were made by hand, to now, mudrocks have been important. The first book on mudrocks, Geologie des Argils by Millot, was not published until 1964; however, scientists, engineers, and oil producers have understood the significance of mudrocks since the discovery of the Burgess Shale and the relatedness of mudrocks and oil. Literature on the elusive yet omnipresent rock-type has been increasing in recent years, and technology continues to allow for better analysis.
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