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ebook swift programming ranch guide guidesIt looks like your browser needs updating. For the best experience on Quizlet, please update your browser. Learn More. Magma chamber a large underground pool of liquid rock found beneath the surface of the Earth. Partial melting occurs when only a portion of a solid is melted Geothermal gradient is the rate of increasing temperature with respect to increasing depth in the Earth's interior. Porphyritic texture has a distinct difference in the size of the crystals, with at least one group of crystals obviously larger than another group. Vesicular texture a volcanic rock texture characterized by a rock being pitted with many cavities (known as vesicles) at its surface and inside. This texture is common in aphanitic, or glassy, igneous rocks that have come to the surface of the earth, a process known as extrusion. Pluton Bodies of intrusive igneous rock Batholith largest of all plutons How igneous rocks form by the freezing of a melt How the composition of a magma is classified Texture and composition Factors that control the formation of magma Temperature, Pressure, and composition. Sequence of mineral formation according to Bowen's reaction series. It looks like your browser needs updating. For the best experience on Quizlet, please update your browser. Learn More The tendency for minerals with lower melting points to melt 1st, thus altering the chemical composition of the melt How does the composition of a melt produced by partial melting compare with the composition of the parent rock. Melt produced by partial melting contains- higher amounts of SiO2 than the parent rock, as the first-melting minerals are SiO2 rich How is Bowen's Reaction Series used to predict the order in which different minerals melt. Shows us the order in which minerals form from magma cooling in a perfect lab setting What magma composition does partial melting of peridotite produce.http://ethio3f.com/ehpea/userfiles/f55-operation-manual.xml
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Magmatic differentiation occurs when partial crystallization of the magma in turn changes the chemical composition of the magma, thus forming a secondary magma What are the first minerals to crystallize from a basaltic magma. Olivine, pyroxene, and Ca-rich plagioclase feldspar (removing most of the Fe, Mg, and Ca from the magma) What are the last minerals to crystallize at low temperature in Bowen's Reaction Series. K-feldspar, muscovite mica, and quartz What are the different factors that affect magma composition? (crystal settling, magma mixing, assimilation, melting of different source rocks, etc.). crystal settling earlier-formed minerals are denser than the melt and settle toward the bottom of the magma Magma mixing alters the composition of a magma by mixing with another magma body Assimilation incorporating country (host) rock into the magma body What is the role of volatiles in generating basaltic magma within subduction zones. It facilitates the melting of basaltic rock, creating Why are rocks of intermediate (andesitic) and felsic (granitic) compositions generally not found in ocean basins. The minerals that comprise andesitic and granitic rocks require conditions to form that are not possible in places like the mantle Along which plate boundary is andesitic magmas generated. CONTINENTAL CRUST What is the sequence of rock compositions produced during differentiation. Helens by Helicopter Helens by Helicopter Rocks make up the majority of the Earth's crust. One of the most common rock is granite. A Crystal is a solid formed by a repeating, three-dimensional pattern of atoms, ions, or molecules and having fixed distances between the different parts. The magma (molten rock under the surface) and lava (molten rock on the surface) hardens into igneous rock. The parent rock can be either sedimentary, igneous, or even another metamorphic rock.http://elrey-uslugi.ru/media/f502-calculator-manual.xml The current custom error settings for this application prevent the details of the application error from being viewed remotely (for security reasons). It could, however, be viewed by browsers running on the local server machine. Chapter 22 Summary Glossary About the Author Appendix 1 List of Geologically Important elements and the Periodic Table Appendix 2 Answers to Review Questions Appendix 3 Answers to Exercises Versioning History On some other planets or their satellites, such as the Moon, the rock cycle is virtually dead because the core is no longer hot enough to drive mantle convection and there is no atmosphere or liquid water. As we’ll see in more detail below, magma is rock that is hot to the point of being entirely molten.Intrusive igneous rock typically crystallizes at depths of hundreds of metres to tens of kilometres below the surface. To change its position in the rock cycle, intrusive igneous rock has to be uplifted and exposed by the erosion of the overlying rocks. Once exposed, they are weathered, both physically (by mechanical breaking of the rock) and chemically (by weathering of the minerals), and the weathering products — mostly small rock and mineral fragments — are eroded, transported, and then deposited as sediments. Transportation and deposition occur through the action of glaciers, streams, waves, wind, and other agents, and sediments are deposited in rivers, lakes, deserts, and the ocean. How long might it take for this entire process to be completed? At depths of hundreds of metres or more, they become compressed and cemented into sedimentary rock. Again through various means, largely resulting from plate-tectonic forces, different kinds of rocks are either uplifted, to be re-eroded, or buried deeper within the crust where they are heated up, squeezed, and changed into metamorphic rock. Chapter 22 Summary Glossary About the Author Appendix 1 List of Geologically Important elements and the Periodic Table Appendix 2 Answers to Review Questions Appendix 3 Answers to Exercises Versioning History By consolidated, we mean hard and strong; real rocks don’t fall apart in your hands. A mixture of minerals implies the presence of more than one mineral grain, but not necessarily more than one type of mineral (Figure 3.1). A rock can be composed of only one type of mineral (e.g., limestone is commonly made up of only calcite), but most rocks are composed of several different minerals. A rock can also include non-minerals, such as fossils or the organic matter within a coal bed or in some types of mudstone. This could be because we removed or broke something or maybe the address you used is incorrect. We suggest that you check that the web address (URL) is typed correctly and reload the page. Since we have already tested on the chapter vocabularly you do not have to worry about it for this test. Please print them out and have them ready for class on Monday the 17th when we will go over and review them to make sure you have the concepts right. You must take notes on your section of the article, and turn them in on the day you present. This will be an informal presentation, do not worry about props, posters, or visual aids of any kind (unless you get super excited and want to earn some bonus points).The final will be cumulative, and worth approximately 15 of your semester grade.Bring them with you next week and correct them in class as we go over them. Whatever you got right you do not need to study, and whatever is left are your study questions. Sarah Maddy. Please refer to the appropriate style manual or other sources if you have any questions.For the article summary, see Igneous rock summary.Igneous rocks constitute one of the three principal classes of rocks, the others being metamorphic and sedimentary. Are rocks and minerals the same. From fossil records to volcanoes, learn more about rocks in this quiz. Whereas sedimentary rocks are produced by processes operating mainly at Earth’s surface by the disintegration of mostly older igneous rocks, igneous—and metamorphic—rocks are formed by internal processes that cannot be directly observed and that necessitate the use of physical-chemical arguments to deduce their origins. Because of the high temperatures within Earth, the principles of chemical equilibrium are applicable to the study of igneous and metamorphic rocks, with the latter being restricted to those rocks formed without the direct involvement of magma. Magma is thought to be generated within the plastic asthenosphere (the layer of partially molten rock underlying Earth’s crust) at a depth below about 60 kilometres (40 miles). Because magma is less dense than the surrounding solid rocks, it rises toward the surface. It may settle within the crust or erupt at the surface from a volcano as a lava flow. Rocks formed from the cooling and solidification of magma deep within the crust are distinct from those erupted at the surface mainly owing to the differences in physical and chemical conditions prevalent in the two environments. Within Earth’s deep crust the temperatures and pressures are much higher than at its surface; consequently, the hot magma cools slowly and crystallizes completely, leaving no trace of the liquid magma. The slow cooling promotes the growth of minerals large enough to be identified visually without the aid of a microscope (called phaneritic, from the Greek phaneros, meaning “visible”). On the other hand, magma erupted at the surface is chilled so quickly that the individual minerals have little or no chance to grow. As a result, the rock is either composed of minerals that can be seen only with the aid of a microscope (called aphanitic, from the Greek aphanes, meaning “invisible”) or contains no minerals at all (in the latter case, the rock is composed of glass, which is a highly viscous liquid). This results in two groups: (1) plutonic intrusive igneous rocks that solidified deep within the crust and (2) volcanic, or extrusive, igneous rocks formed at Earth’s surface. Some intrusive rocks, known as subvolcanic, were not formed at great depth but were instead injected near the surface where lower temperatures result in a more rapid cooling process; these tend to be aphanitic and are referred to as hypabyssal intrusive rocks. The deep-seated plutonic rocks can be exposed at the surface for study only after a long period of denudation or by some tectonic forces that push the crust upward or by a combination of the two conditions. (Denudation is the wearing away of the terrestrial surface by processes including weathering and erosion.) Generally, the intrusive rocks have cross-cutting contacts with the country rocks that they have invaded, and in many cases the country rocks show evidence of having been baked and thermally metamorphosed at these contacts. The exposed intrusive rocks are found in a variety of sizes, from small veinlike injections to massive dome-shaped batholiths, which extend for more than 100 square kilometres (40 square miles) and make up the cores of the great mountain ranges. Get a Britannica Premium subscription and gain access to exclusive content. The coarser pyroclastic materials accumulate around the erupting volcano, but the finest pyroclasts can be found as thin layers located hundreds of kilometres from the opening. Most lava flows do not travel far from the volcano, but some low-viscosity flows that erupted from long fissures have accumulated in thick (hundreds of metres) sequences, forming the great plateaus of the world (e.g., the Columbia River plateau of Washington and Oregon and the Deccan plateau in India). Both intrusive and extrusive magmas have played a vital role in the spreading of the ocean basin, in the formation of the oceanic crust, and in the formation of the continental margins. Igneous processes have been active since the onset of the formation of Earth some 4.6 billion years ago. Their emanations have provided the water for the oceans, the gases for the primordial oxygen-free atmosphere, and many valuable mineral deposits. Indeed, in 1960 a sodium carbonate (Na 2 CO 3 ) lava with only 0.05 weight percent silica (SiO 2 ) was erupted from Ol Doinyo Lengai, a volcano in northern Tanzania, Africa. Because of the limited occurrence of such carbonate-rich igneous rocks, however, the following discussion will consider the chemistry of silicate rocks only. The major oxides of the rocks generally correlate well with their silica content: those rocks with low silica content are enriched in magnesium oxide (MgO) and iron oxides (FeO, Fe 2 O 3, and Fe 3 O 4 ) and are depleted in soda (Na 2 O) and potash (K 2 O); those with a large amount of silica are depleted in magnesium oxide and iron oxides but are enriched in soda and potash. Both calcium oxide (CaO) and alumina (Al 2 O 3 ) are depleted in the rocks that have a silica content of less than about 45 weight percent, but, above 45 percent, calcium oxide can be as high as 10 percent; this amount decreases gradually as the silica increases. Alumina in rocks that contain more than 45 percent silica is generally above approximately 14 weight percent, with the greatest abundance occurring at an intermediate silica content of about 56 weight percent. Because of the importance of silica content, it has become common practice to use this feature of igneous rocks as a basis for subdividing them into the following groups: silicic or felsic (or acid, an old and discredited but unfortunately entrenched term), rocks having more than 66 percent silica; intermediate, rocks with 55 to 66 percent silica; and subsilicic, rocks containing less than 55 percent silica. The latter may be further divided into two groups: mafic, rocks with 45 to 55 percent silica and ultramafic, those containing less than 45 percent. The subsilicic rocks, enriched as they are in iron (Fe) and magnesium (Mg), are termed femic (from fe rrous iron and m agnesium), whereas the silicic rocks are referred to as sialic (from si lica and al uminum, with which they are enriched) or salic (from s ilica and al uminum). The terms mafic (from ma gnesium and f errous iron) and felsic ( fel dspar and s ilica) are used interchangeably with femic and sialic. The silica content also reflects the mineral composition of the rocks. As the magma cools and begins to crystallize, silica is taken from the magma to be combined with the other cationic oxides to form the silicate minerals. Two moles of SiO 2 are needed to be combined with one mole each of CaO and Al 2 O 3 to make the calcium-rich plagioclase, CaAl 2 Si 2 O 8 ( anorthite ). However, in a case where magma does not have enough silica relative to the magnesium oxide to produce the pyroxene, the magma will compensate by making a magnesium-olivine ( forsterite; Mg 2 SiO 4 ), along with the pyroxene, since the olivine requires only one-half as much silica for every mole of magnesium oxide. On the other hand, a silicic magma may have excess silica such that some will be left after all the silicate minerals were formed from the combination of the oxides; the remaining “free” silica crystallizes as quartz or its polymorphs. These three minerals substitute in part for enstatite, albite (NaAlSi 3 O 8, requiring three moles of silicon for one mole of sodium), and orthoclase feldspar (KAlSi 3 O 8, requiring three moles of silicon for one mole of potassium), respectively. Quartz clearly will not be present in these rocks. Minerals such as magnesium-olivine, nepheline, and leucite are termed undersaturated (with respect to silica), and the subsilicic rocks that contain them are termed undersaturated as well. In the case of rocks that have excess silica, the silicic rocks will have quartz and magnesium-pyroxene, which are considered saturated minerals, and the rocks that contain them are termed supersaturated. The current custom error settings for this application prevent the details of the application error from being viewed remotely (for security reasons). It could, however, be viewed by browsers running on the local server machine. Close this message to accept cookies or find out how to manage your cookie settings. Cambridge University PressMicrostructures of some slowly cooled mafic and ultramafic igneous rocks also show evidence of reduction of interfacial free energy, but this effect is minimal in granitoids. Symplectic intergrowths, including myrmekite, are useful for inferring some metamorphic reactions. Similar intergrowths occur in oxide and sulphide minerals. Microstructural evidence is important for inferring metamorphic reactions, but requires care in interpretation. Evidence of parent rock-types can be seen in less deformed metamorphic rocks. Many metamorphic minerals show compositional zoning, as revealed especially by X-ray composition images. Microstructures formed at highest metamorphic temperatures commonly show evidence of partial melting, producing migmatites, some with magmatic microstructures. Melting can also occur in some sulphide rocks. EC574010 INSPECTION Wash the bearings, bushes, collars, and covers in a solvent.NOTE: 9Apply the molybdenum disulfide grease on the bearing when installing. 9Install the bearing by pressing it on the side hav- ing the manufacture's marks or numbers. Install: 9Cap 1 NOTE: Install the cap with its mark a facing forward. 13. To dispose of a damaged or worn-out shock absorber, take the unit to your Yamaha dealer for this disposal procedure. 5-60. Do not apply the grease on the bearing outer race because it will wear the rear shock absorber surface on which the bear- ing is press fitted. No good Check each couplers and Repair or replace.Mauvais Magnetventilspule Changer. Nicht in Ordnung Erneuern oder Alle Stecker - und Kabelverbin- reparieren. Nicht in Ordnung Magnetventilspule Erneuern. Non funziona Controllare tutti gli accoppiatori e i Ripararlo o sostituirlo.Non funziona Controllare il funziona- Controllare l’elettrovalvola. Sostituirlo. mento dell’elettrovalvola. EC652040 SOLENOID VALVE OPERATION 1. Disconnect the solenoid valve coupler. 2. Connect 12V battery to the solenoid valve coupler. No good Check entire ignition Repair or replace.No good Check TPS. TPS coil Replace. In Ordnung Nicht in Ordnung TPS kontrollieren. TPS-Spule Erneuern. Controllare il collegamento dell’intero Non funziona Ripararlo o sostituirlo.Non funziona Controllare il TPS. EC692000 TPS COIL INSPECTION 1. Remove: 9Carburetor 9Mixing chamber top Refer to “CARBURETOR AND REED VALVE” section in the CHAPTER 4. 2. Refer to “IDLE SPEED ADJUSTMENT” sec- tion in the CHAPTER 3. Ausrichtmarkierungen a am TPS 11. Segnare le indicazioni a di posi- 11.Accord- ingly, if a mixture of air and fuel is too lean, abnormal combustion will occur, and engine seizure may result. In this case, step up the jet needle clip by one groove and move down the needle to lean out the mixture. Therefore, carburetor setting requires the change of the jet needle. 1. Therefore, carburetor setting requires the change of the jet needle. 1. The jet needle setting parts, having the same taper angle, are available in different straight portion diameters and in different taper starting positions. White smoke Unstable at low speeds Lower jet needle clip position. The front fork setting includes the following three factors: 1. Setting of air spring characteristics 9Change the fork oil level. Always adjust each front fork to the same setting. Rebound damping tends to become weaker, resulting in lack of a sense of con- tact with the road surface or in a vibrating handlebar. To set a stiff spring: 9Change the rebound damping. Die una sensazione di guida rigida. The rear suspension setting includes the follow- ing two factors: 1. Setting of spring preload 9Change the set length of the spring. Never use one whose overall length is greater than standard. In doing so, no representation of affiliation, association or the like is intended, unless otherwise stated. Moreover, we are in fact owners of intellectual property, property that is a valuable asset to our business. Any reprinting or unauthorized use without the written permission of Yamaha Motor Co., Ltd. is expressly prohibited. Printed in Japan. This model is the culmination of Yamaha’s vast experience in the production of pacesetting racing machines. It represents the highest grade of craftsmanship and reliability that have made Yamaha a leader. Dieses Modell entspricht fort-. Off-road use on public lands may also be illegal. Please check local regulations before riding. Take care to not spill any gasoline on the engine or exhaust system. Never refuel in the vicinity of an open flame, or while smoking. 6. GASOLINE CAN CAUSE INJURY. If you should swallow some gasoline, inhale excess gasoline vapors, or allow any gasoline to get into your eyes, con-. Dar- faisant le plein.If there is any question you have regarding this manual or your machine, please consult your Yamaha deal- EC070001 F.I.M. MACHINE WEIGHTS: Weights of machines without fuel. The information has been complied to provide the mechanic with an easy to read, handy reference that contains com- prehensive explanations of all disassembly, repair, assembly, and inspection operations. In this revised format, the condition of a faulty component will precede an arrow symbol and the course of action required will follow the symbol, e.g., 9 Bearings. General information INSP Specifications Regular inspection and adjustments Engine Chassis Electrical Tuning CHAS ELEC Illustrated symbols 8 to r are used to identify the specifications appearing in the text. When washing the machine with high pres- sured water, cover the parts as follows. 9 Silencer exhaust port 9 Side cover air intake port 9 Water pump housing hole at the bottom. EC133000 GASKETS, OIL SEALS AND O-RINGS 1. All gaskets, oil seals, and O-rings should be replaced when an engine is overhauled. Bauteile zu verwenden.Always replace piston pin clips after one use. Replace distorted circlips. When installing a circlip 1, make sure that the sharp-edged corner 2 is posi- tioned opposite to the thrust 3 it receives. See the sectional view. Using the correct special tool will help prevent damage caused by the use of improper tools or improvised tech- niques. The shape and part number used for the special tool differ by country, so two types are provid- ed. La forma e il numero categorico usati per l’utensile speciale sono diversi a seconda del paese, quindi vengono forniti due tipi. Continue pushing the “ENGINE STOP” button till the engine comes to a stop. EC152000 CLUTCH LEVER The clutch lever 1 is located on the left handle- bar;. Pull it toward the handlebar to acti- vate the front brake. EC157000 REAR BRAKE PEDAL The rear brake pedal 1 is located on the right side of the machine. EC15F000 VALVE JOINT This valve joint 1 prevents fuel from flowing out and is installed to the fuel tank breather hose. Always use fresh, name-brand gasoline, and mix the oil and gas the day of the race. Do not use premix that is more than a few hours old. Never start or run the engine in a closed area. The exhaust fumes are poisonous; they can cause loss of consciousness and death in a very short time. Mixing oil: Mixing ratio: Yamalube “2-R” 15:1 2. Perform the pre-operation checks on the machine. 3. Start and warm up the engine. Check the idle speed, and check the operation of the controls and the “ENGINE STOP”. Tighten all such fasteners as required. 9 When any of the following parts have been replaced, they must be broken in. After cleaning machine thoroughly, prepare it for storage as fol- lows: 1. Drain the fuel tank, fuel lines, and the carbu- retor float bowl. To avoid warpage, tighten multi-faste- ner assemblies in a crisscross fashion, in pro- gressive stages, until full torque is reached. Wenn Teile mit mehreren Befestigungselementen festgezogen werden, die Schrauben und Muttern kreuzweise und in meh- reren Schritten. G Clamp the radiator breather 2 Clamp the frame at its locating tape. 3 CDI magneto lead Clamp it at the rear of the radia- hose, CDI magneto lead and 4 Neutral switch lead (except for tor fitting boss. B Pass the high tension cord to 3 High tension cord 4 CDI unit band the right of the radiator hose so 5 CDI unit that the high tension cord does 6 CDI unit lead not contact the radiator hose. B Pass the brake hose into the brake hose holders. C If the brake hose contacts the spring (rear shock absorber), correct its twist. B Pass the “ENGINE STOP” button lead in the middle 4 “ENGINE STOP”. Before using this machine, check the following points. EC321000 GENERAL INSPECTION AND MAINTENANCE Item Routine Page. Prima di usare questo veicolo, controllare i punti che seguono. IC321000 ISPEZIONE E MANUTENZIONE GENERALI Voce. Scalding hot fluid and steam may be blown out under pressure, which could cause serious injury. If it splashes, wash it away with water. 1. Place a container under the engine. 2. Remove: 9 Coolant drain bolt 1 3. Remove: 9 Radiator cap Drain the coolant completely. Handling notes of coolant: The coolant is harmful so it should be handled with special care. Throttle grip free play.Never run the engine without the air filter element in place;. NOTE: Squeeze out the excess oil. Element should be wet but not dripping. 5. Install: 9 Filter guide 1 NOTE: Align the projection a on filter guide with the hole b in air filter element. NOTE: Be sure the machine is positioned straight up when inspecting the oil level. Never attempt to remove the oil check bolt just after high speed operation. A dangerous loss of braking performance may occur if the brake system is not properly bled. Repeat the bleeding procedure when the tiny bubbles in the system have disappeared. j. Add brake fluid to the level line on the reservoir. Brake pedal height a a: Zero mm (Zero in) NOTE: The brake pedal height is the vertical distance from the inside top end of the footrest. NOTE: Replace the drive, driven sprockets and drive chain as a set.EC36U070 STEERING HEAD INSPECTION AND ADJUSTMENT 1. Elevate the front wheel by placing a suitable stand under the engine. 2. Check: 9 Steering shaft Grasp the bottom of the forks and gently rock the fork assembly back and forth. Avoid over-tightening.Scalding hot fluid and steam may be blown out under pressure, which could cause serious injury. When the engine has cooled, open the radiator cap by the following procedure: Place a thick rag, like a towel, over the radi- ator cap, slowly rotate the cap counter-. Needle holder Jet needle Float chamber Float pin. EC463000 REMOVAL POINTS EC463110 Throttle valve 1. NOTE: 9 Use a petroleum based solvent for cleaning. Blow out all passages and jets with com- pressed air. 9 Never use a wire. 2. Be sure to use the set pin. If the set pin is not used, the power valve constituent parts will result in damage. EC474000 INSPECTION EC474102 Cylinder head 1. Eliminate: 9 Carbon deposits Use a rounded scraper 1. EC474502 Piston ring 1. Install: 9 Piston ring Into the cylinder. Refer to “Cylinder” and “Piston”.Cylinder mark Piston mark (color) A (red) B (orange) C (green) D (purple) NOTE: When you purchase a cylinder, you cannot des- ignate its size. Choose the piston that matches the above chart. Measure at all four points.Zum Kupplungsdeckel. Verso la protezione della frizio- 11. EC4K4200 Bearing 1. EC4G3210 Oil seal NOTE:. EC4H4600 Bearing 1. Inspect: 9 Bearing 1 Rotate inner race with a finger.If the segment gets an impact, it may be damaged. Take care not to give an impact to the segment when removing the bolt. Do not use a hammer to drive out the crankshaft. NOTE: Install the bearing by pressing its outer race parallel. EC4N5102 Oil seal 1. Install: 9 Oil seal (left) 1 9 Oil seal (right) 2 NOTE: 9 Apply the lithium soap base grease on the oil. Note the position of each part. NOTE: 9 Apply the molybdenum disulfide oil on the shift fork grooves. Use the dial gauge 1. Wheel axle bending limit: 0.5 mm (0.020 in) NOTE: The bending value is shown by one half of the dial gauge reading. A Front B Rear 2. Connect the transparent hose 2 to the bleed screw 1 and place a suitable contain- er under its end. Never attempt to pry out piston seals and dust seals. Install the brake hose so that its pipe por- tion a a directs as shown and lightly touch- es the projection b b on the master cylinder. Refer to “REAR BRAKE ADJUSTMENT” section in the CHAPTER 3. EC5A5911 Front brake hose 1. Install the brake hose so that its pipe por- tion a a directs as shown and lightly touch- es the projection b b on the master cylinder. If it does, correct its twist. Refer to “BRAKE FLUID LEVEL INSPEC- TION”. So it is recommended that the front fork be maintained at the dealers.