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    Diamond Symbol

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    Diamond Symbol

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    Diamond Symbol How to insert diamond symbol using the alt key? Video

    DIAMOND SEVEN SYMBOL YAMASHITA TREASURE SIGN

    Diamond Symbol

    Below are the steps to insert the Diamond Sign in Word using the insert symbol dialog. This is how you may insert a Diamond symbol in Word using the insert symbol dialog.

    My favorite method is using the copy and paste method followed by the shortcut in Word for both Windows and Mac.

    The Alt Code method also comes simple. For any comments or questions about this guide, please let me know in the comments section below.

    Because it can only be scratched by other diamonds, it maintains its polish extremely well. Unlike many other gems, it is well-suited to daily wear because of its resistance to scratching—perhaps contributing to its popularity as the preferred gem in engagement or wedding rings , which are often worn every day.

    These diamonds are generally small, perfect to semiperfect octahedra, and are used to polish other diamonds. Their hardness is associated with the crystal growth form, which is single-stage crystal growth.

    Most other diamonds show more evidence of multiple growth stages, which produce inclusions, flaws, and defect planes in the crystal lattice, all of which affect their hardness.

    It is possible to treat regular diamonds under a combination of high pressure and high temperature to produce diamonds that are harder than the diamonds used in hardness gauges.

    Somewhat related to hardness is another mechanical property toughness , which is a material's ability to resist breakage from forceful impact.

    The toughness of natural diamond has been measured as 7. As with any material, the macroscopic geometry of a diamond contributes to its resistance to breakage.

    Diamond has a cleavage plane and is therefore more fragile in some orientations than others. Diamond cutters use this attribute to cleave some stones, prior to faceting.

    Usually, attempting to deform bulk diamond crystal by tension or bending results in brittle fracture. Other specialized applications also exist or are being developed, including use as semiconductors : some blue diamonds are natural semiconductors, in contrast to most diamonds, which are excellent electrical insulators.

    The conductivity and blue color originate from boron impurity. Boron substitutes for carbon atoms in the diamond lattice, donating a hole into the valence band.

    Substantial conductivity is commonly observed in nominally undoped diamond grown by chemical vapor deposition.

    This conductivity is associated with hydrogen-related species adsorbed at the surface, and it can be removed by annealing or other surface treatments.

    A paper reported that extremely thin needles of diamond can be made to vary their electrical resistance from the normal 5.

    Diamonds are naturally lipophilic and hydrophobic , which means the diamonds' surface cannot be wet by water, but can be easily wet and stuck by oil.

    This property can be utilized to extract diamonds using oil when making synthetic diamonds. However, when diamond surfaces are chemically modified with certain ions, they are expected to become so hydrophilic that they can stabilize multiple layers of water ice at human body temperature.

    The surface of diamonds is partially oxidized. The oxidized surface can be reduced by heat treatment under hydrogen flow. That is to say, this heat treatment partially removes oxygen-containing functional groups.

    The structure gradually changes into sp 2 C above this temperature. Thus, diamonds should be reduced under this temperature. At room temperature, diamonds do not react with any chemical reagents including strong acids and bases.

    It increases in temperature from red to white heat and burns with a pale blue flame, and continues to burn after the source of heat is removed.

    By contrast, in air the combustion will cease as soon as the heat is removed because the oxygen is diluted with nitrogen. A clear, flawless, transparent diamond is completely converted to carbon dioxide; any impurities will be left as ash.

    Jewelers must be careful when molding the metal in a diamond ring. Consequently, pyrotechnic compositions based on synthetic diamond powder can be prepared.

    The resulting sparks are of the usual red-orange color, comparable to charcoal, but show a very linear trajectory which is explained by their high density.

    Diamond has a wide bandgap of 5. This means that pure diamond should transmit visible light and appear as a clear colorless crystal. Colors in diamond originate from lattice defects and impurities.

    The diamond crystal lattice is exceptionally strong, and only atoms of nitrogen , boron and hydrogen can be introduced into diamond during the growth at significant concentrations up to atomic percents.

    Transition metals nickel and cobalt , which are commonly used for growth of synthetic diamond by high-pressure high-temperature techniques, have been detected in diamond as individual atoms; the maximum concentration is 0.

    Virtually any element can be introduced to diamond by ion implantation. Nitrogen is by far the most common impurity found in gem diamonds and is responsible for the yellow and brown color in diamonds.

    Boron is responsible for the blue color. Plastic deformation is the cause of color in some brown [51] and perhaps pink and red diamonds.

    Colored diamonds contain impurities or structural defects that cause the coloration, while pure or nearly pure diamonds are transparent and colorless.

    Most diamond impurities replace a carbon atom in the crystal lattice , known as a carbon flaw. The most common impurity, nitrogen, causes a slight to intense yellow coloration depending upon the type and concentration of nitrogen present.

    Diamonds of a different color, such as blue, are called fancy colored diamonds and fall under a different grading scale. In , the Wittelsbach Diamond , a Diamonds cut glass, but this does not positively identify a diamond because other materials, such as quartz, also lie above glass on the Mohs scale and can also cut it.

    Diamonds can scratch other diamonds, but this can result in damage to one or both stones. Hardness tests are infrequently used in practical gemology because of their potentially destructive nature.

    Diamonds also possess an extremely high refractive index and fairly high dispersion. Taken together, these factors affect the overall appearance of a polished diamond and most diamantaires still rely upon skilled use of a loupe magnifying glass to identify diamonds "by eye".

    Diamonds are extremely rare, with concentrations of at most parts per billion in source rock. Loose diamonds are also found along existing and ancient shorelines , where they tend to accumulate because of their size and density.

    Most diamonds come from the Earth's mantle , and most of this section discusses those diamonds. However, there are other sources. Some blocks of the crust, or terranes , have been buried deep enough as the crust thickened so they experienced ultra-high-pressure metamorphism.

    These have evenly distributed microdiamonds that show no sign of transport by magma. In addition, when meteorites strike the ground, the shock wave can produce high enough temperatures and pressures for microdiamonds and nanodiamonds to form.

    A common misconception is that diamonds are formed from highly compressed coal. Coal is formed from buried prehistoric plants, and most diamonds that have been dated are far older than the first land plants.

    It is possible that diamonds can form from coal in subduction zones , but diamonds formed in this way are rare, and the carbon source is more likely carbonate rocks and organic carbon in sediments, rather than coal.

    Diamonds are far from evenly distributed over the Earth. A rule of thumb known as Clifford's rule states that they are almost always found in kimberlites on the oldest part of cratons , the stable cores of continents with typical ages of 2.

    The Argyle diamond mine in Australia , the largest producer of diamonds by weight in the world, is located in a mobile belt , also known as an orogenic belt , [67] a weaker zone surrounding the central craton that has undergone compressional tectonics.

    Instead of kimberlite, the host rock is lamproite. Lamproites with diamonds that are not economically viable are also found in the United States, India and Australia.

    Kimberlites can be found in narrow 1 to 4 meters dikes and sills, and in pipes with diameters that range from about 75 m to 1. Fresh rock is dark bluish green to greenish gray, but after exposure rapidly turns brown and crumbles.

    They are a mixture of xenocrysts and xenoliths minerals and rocks carried up from the lower crust and mantle , pieces of surface rock, altered minerals such as serpentine , and new minerals that crystallized during the eruption.

    The texture varies with depth. The composition forms a continuum with carbonatites , but the latter have too much oxygen for carbon to exist in a pure form.

    Instead, it is locked up in the mineral calcite Ca C O 3. All three of the diamond-bearing rocks kimberlite, lamproite and lamprophyre lack certain minerals melilite and kalsilite that are incompatible with diamond formation.

    In kimberlite, olivine is large and conspicuous, while lamproite has Ti- phlogopite and lamprophyre has biotite and amphibole. They are all derived from magma types that erupt rapidly from small amounts of melt, are rich in volatiles and magnesium oxide , and are less oxidizing than more common mantle melts such as basalt.

    These characteristics allow the melts to carry diamonds to the surface before they dissolve. Kimberlite pipes can be difficult to find.

    They weather quickly within a few years after exposure and tend to have lower topographic relief than surrounding rock.

    If they are visible in outcrops, the diamonds are never visible because they are so rare. In any case, kimberlites are often covered with vegetation, sediments, soils or lakes.

    In modern searches, geophysical methods such as aeromagnetic surveys , electrical resistivity and gravimetry , help identify promising regions to explore.

    This is aided by isotopic dating and modeling of the geological history. Then surveyors must go to the area and collect samples, looking for kimberlite fragments or indicator minerals.

    The latter have compositions that reflect the conditions where diamonds form, such as extreme melt depletion or high pressures in eclogites.

    However, indicator minerals can be misleading; a better approach is geothermobarometry , where the compositions of minerals are analyzed as if they were in equilibrium with mantle minerals.

    Finding kimberlites requires persistence, and only a small fraction contain diamonds that are commercially viable. The only major discoveries since about have been in Canada.

    Since existing mines have lifetimes of as little as 25 years, there could be a shortage of new diamonds in the future. Diamonds are dated by analyzing inclusions using the decay of radioactive isotopes.

    Depending on the elemental abundances, one can look at the decay of rubidium to strontium , samarium to neodymium , uranium to lead , argon to argon , or rhenium to osmium.

    Those found in kimberlites have ages ranging from 1 to 3. The kimberlites themselves are much younger. Most of them have ages between tens of millions and million years old, although there are some older exceptions Argyle, Premier and Wawa.

    Thus, the kimberlites formed independently of the diamonds and served only to transport them to the surface.

    The reason for the lack of older kimberlites is unknown, but it suggests there was some change in mantle chemistry or tectonics. No kimberlite has erupted in human history.

    Such depths occur below cratons in mantle keels , the thickest part of the lithosphere. These regions have high enough pressure and temperature to allow diamonds to form and they are not convecting, so diamonds can be stored for billions of years until a kimberlite eruption samples them.

    Host rocks in a mantle keel include harzburgite and lherzolite , two type of peridotite. The most dominant rock type in the upper mantle , peridotite is an igneous rock consisting mostly of the minerals olivine and pyroxene ; it is low in silica and high in magnesium.

    However, diamonds in peridotite rarely survive the trip to the surface. They formed in eclogite but are distinguished from diamonds of shallower origin by inclusions of majorite a form of garnet with excess silicon.

    Diamond is thermodynamically stable at high pressures and temperatures, with the phase transition from graphite occurring at greater temperatures as the pressure increases.

    Thus, the deeper origin of some diamonds may reflect unusual growth environments. In the first known natural samples of a phase of ice called Ice VII were found as inclusions in diamond samples.

    The mantle has roughly one billion gigatonnes of carbon for comparison, the atmosphere-ocean system has about 44, gigatonnes. It can also be altered by surface processes like photosynthesis.

    This variability implies that they are not formed from carbon that is primordial having resided in the mantle since the Earth formed.

    Instead, they are the result of tectonic processes, although given the ages of diamonds not necessarily the same tectonic processes that act in the present.

    Diamonds in the mantle form through a metasomatic process where a C-O-H-N-S fluid or melt dissolves minerals in a rock and replaces them with new minerals.

    Diamonds form from this fluid either by reduction of oxidized carbon e. Using probes such as polarized light, photoluminescence and cathodoluminescence , a series of growth zones can be identified in diamonds.

    The lozenge in heraldry is a diamond-shaped charge , usually somewhat narrower than it is tall. A mascle is a voided lozenge—that is, a lozenge with a lozenge-shaped hole in the middle—and the rarer rustre is a lozenge containing a circular hole.

    A field covered in a pattern of lozenges is described as lozengy ; a similar field of mascles is masculy. In axiomatic set theory , the lozenge refers to the principles known collectively as the diamond principle.

    Cough tablets have taken the name lozenge, based on their original shape. According to the Oxford English Dictionary the first use of this sense was in In Finland, the lozenge is associated with salmiak , through Apteekin Salmiakki.

    Thus, the lozenge is commonly called salmiakkikuvio "salmiak shape". The pattern is often used even if the candy is not actually lozenge-shaped.

    In Finnish military ranks , the lozenge is found in the insignia of conscript officer students one lozenge and conscript officer candidates two lozenges.

    To implement 10 U. C , the Secretary of the Navy has prescribed the following distinctive mark for wear by members of military societies which are composed entirely of honorably discharged officers and enlisted personnel, or by the instructors and members of duly organized cadet corps.

    A white distinctive mark will be worn on blue, green, or khaki clothing; and a blue distinctive mark will be worn on white clothing.

    The lozenge is used in the Army , Marine Corps , and Air Force on the insignia of their respective first sergeants. In modal logic , the lozenge expresses that there is "possibility.

    The lozenge technically a mascle can be used on public roadways in the United States and Canada to mark a specific lane for a particular use.

    The lane will usually be painted with a lozenge at a regular interval, and signage will be installed to indicate the restrictions on using the lane.

    Prior to 17 January , lozenges could also be used to mark bicycle-only lanes, often in conjunction with a bicycle icon. In the United Kingdom , lozenges are used on tramway signs.

    For instance, speed limits are shown as a black lozenge on a white background, containing the speed limit in kilometres per hour. Diamonds can also symbolize wealth and status.

    As the early royal families, aristocrats, and wealthy families held collections of diamonds, and it is not uncommon to find diamonds of adorn wallets, bags, phone cases, or even clothing.

    While diamonds have become more popular and prevalent, they, at the same time, remain a luxury product that is reserved for those who can afford it.

    Diamonds, besides love and wealth, can represent the symbol of extravagance and beauty. For example, from Hollywood award shows to presidential dinners, diamonds may be found on accessories and jewelry e.

    The way the light sparkles and reflects on a gemstone of the diamond can be immediately captivating that gives a sense of elegance as well.

    Unfortunately, diamonds have also come to represent some of the worst tragedies and conflicts in our lifetime.

    The gemstone mining has resulted in child slavery and child soldiers, and even civil wars in Sierra Leone and Liberia.

    These symbols are considered to be the building blocks of all matter, of everything. As such, the diamond and triangle symbol is indicative of the journey our souls make while we are achieving higher understanding it is an enlightened or clarified soul that is able to refract its light from the insight out and serve as a beacon to the outer world.

    On this path there will be many labyrinth turns representative of the angles and facets of the diamond. This symbol shown is a common motif among Native peoples indigenous to North America, Canada, and Mexico.

    This homecoming was seen as intensely powerful to Native thought. Just as the migratory journey is analogous of the spiritual path of reuniting with the Divine self — so too is the biological journey of the butterfly symbolic of the same said spiritual path.

    The earth has long been worshipped by ancient mystics. Indeed, earth magic is rooted in the ideology that all things of the earth are born from her, and therefore vibrate with earth energy.

    This symbol would be used in ritual for such clarifications. This rune is called the Dagaz and is the Symbol of the Dawn.

    This rune speaks of the partnership between night and day with the center-point represented as the dawn. Metaphorically, the dawn marks an awakening to all new understandings.

    This diamond motif is seen throughout the ages and cultures. For our purposes, we look again to the Futhark for symbolic insight where this is known as the Ingwuz rune and is the foundational geometric symbol of creation.

    Many translated example sentences containing "diamond symbol" – German-​English dictionary and search engine for German translations. Für die im Unicode-Standard diamond genannten Zeichen (auf die Spitze gestellte Quadrate) kann die für Spielkartensymbole zutreffende Übersetzung „​Karo“. Suchen Sie nach diamond symbol-Stockbildern in HD und Millionen weiteren lizenzfreien Stockfotos, Illustrationen und Vektorgrafiken in der. Schau dir unsere Auswahl an diamond symbol an, um die tollsten einzigartigen oder spezialgefertigten, handgemachten Stücke aus unseren Shops zu finden. Solid carbon comes in different forms known as allotropes depending on the type Epic Games Zahlungsmethoden chemical bond. Non-necessary Non-necessary. May 12, Diamond-like glass". Retrieved 1 June No kimberlite has erupted in human history. April Those potentially synthetic diamonds require more investigation in a specialized lab. Kimberlites can be found in narrow 1 to 4 meters dikes and sills, and in pipes with diameters that range from about 75 m to 1. May 15,

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    Sales Tax: Washington State residents will be charged Bubbleschooter tax. The Diamond (♦) Symbol Alt Code is 4. Every symbol in Word has a unique code that you can use to insert the symbol into your document. This code is well known as “Alt code”. Below are the steps to type this symbol on your keyboard (using the Alt code provided above. apl functional symbol diamond underbar: u+ 25c6 e2 97 black diamond: u+ 25c7 e2 97 white diamond: u+ 25c8 e2 97 white diamond containing black small diamond: u+ ♢ e2 99 a2: white diamond suit: u+ ♦ e2 99 a6: black diamond suit: u+ 26cb ⛋ e2 9b 8b: white diamond in square: u+ e2 9d black diamond minus white x: u+ 27d0 e2 9f white diamond with centred dot: u+ 27e1 e2 9f a1. The quickest way to produce a small black diamond ♦ is to hold Alt down and type no. 4 on the numeric key pad, then release Alt (Num Lock must be on for this to work). Alternatively, use the Insert, Symbols menu: A shortcut to open the menu is to press Alt+I then press S on its own (i.e. without Alt). Significance of Diamond Symbolism. The diamond symbol has long been valued for its immaculate beauty. Its physical appearance is associated with valuable attributes that are relevant to living a meaningful life, such as purity, clarity and wisdom. The series of triangles making up the diamond shape have been present in the realm of design across every culture, religion, and period of time, expressing the same themes as the other physical characteristics of diamonds. These are steps to insert the diamond shape in MS Word, Excel, and PowerPoint. Make sure your numeric keypad is active on the keyboard. Place the mouse cursor where you want to insert the symbol. Press the Alt key and type 4 on the numeric keypad. Release both the keys and the black diamond sign will show up. This category only includes cookies that ensures basic functionalities and security features of the website. The diamond icon also serves riches, unconquerable, intellectual knowledge, along with treasures. From the cells in our bodies to Trump Wiederwahl Chance stars in the sky. The Diamond Symbol shortcut for Microsoft Word is , Alt+X. These shortcuts work in Microsoft Word and Windows only. To use this shortcut, obey the following instructions: Place the insertion pointer in the right place. Type on your keyboard, then press Alt + X. This will convert the code () into the Diamond symbol at where you. Diamond Symbol Alt Codes, HTML Code (Copy and Paste) Here is the list of alt codes for diamond symbols. You can copy and paste diamond symbol in Word, Excel, and PowerPoint or use alt codes to make various kinds of diamond. Just click on a symbol to copy. If you want to use the diamond symbol in HTML documents use HTML code. Diamond Symbol [♦] Quick Guide. To type the Diamond Symbol on Mac, press Option + Shift + V shortcut on your keyboard. For Windows users, simply press down the Alt key and type 4 using the numeric keypad, then let go of the Alt key. These Diamond sign shortcuts can work on any software including MS Word, Excel, and PowerPoint, on both Windows. Bitte geben Sie eine gültige PLZ ein. Verkäufer kontaktieren. Bei Black Diamond dreht sich alles ums Klettern und Skifahren. Wir Lottoland Illegal die gleichen Erfahrungen im Fels, Eis und Schnee wie du.

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