Diferentes tipos de Rubi

O rubi é o nome da variedade vermelho do mineral corindon e o corindon  pode ter várias cores mas sob o nome de safira, salvo o corindon de cor vermelho que é reservado exclusivamente ao rubi.
rubi bruto da Tanzânia foto de Rob Lavinsky, iRocks.com
Rubi bruto da Tanzânia foto de Rob Lavinsky, iRocks.com
Antes de conhecermos os diferentes tipos de Rubis, será preciso saber:
Como se forma o Rubi?
O Rubi e a Safira são duas gemas preciosas que são encontradas nas chamadas rochas metamórficas. Elas são formadas da seguinte maneira: o magma extravasa do manto, e então o vulcanismo coloca as rochas do local onde extravasou sob calor e pressão, o que pode causar mudanças na estrutura química de seus cristais. Daí o nome metamórfica, devido à transformação química que essas rochas sofrem.
É um processo que leva milhões de anos e poucos lugares no mundo têm minas desses raros cristais.
Os  tipos de Rubis são diferenciados dependendo de onde eles são extraídos. Rubis vêm em vários tons de vermelho, mas podem ir desde tons de vermelho a tons de cor de rosa, o que é determinado por diferentes elementos.
Além do rubi e da safira, gemas associadas a rochas metamórficas incluem berilo, jade, lápis-lazúli, turquesa, espinélio e zircão. Na maioria das vezes ocorrem junto com espinelas nas mesmas formações geológicas ocorrendo confusão entre as duas espécies: no entanto, também bons exemplares de espinelas vermelhas têm um valor próximo do rubi.

O Rubi é uma variedade do mineral corindo (óxido de alumínio) cuja cor é causada principalmente pela presença de crómio. O óxido crômico dá os tons de vermelho rubi, enquanto o óxido férrico dá um pouco de amarelo. Os rubis com altos níveis de titânio são os mais procurados devido a sua cor vermelha intenso. Se um rubi tiver tons rosa, roxo, laranja e marrom, é causado por cromo e ferro. A quantidade de cor depende da quantidade de metais. Porém nem todas as amostras de Rubi possuem as qualidades requeridas de tranparência e de cor para serem consideradas como gemas.

O Rubi tem dureza 9 na escala de Mohs, e entre as gemas naturais somente é ultrapassado pelo diamante em termos de dureza. As variedades de corindo não vermelhas são conhecidas como safiras.

O Rubi foi muito tempo dito "carbunculo" que era confundido com o espinélio vermelho e a granada piropo. Somente no ano 1800 que ele é associado, com a safira, no grupo do corindon.

Rubis artificiais
Os rubis naturais são excepcionalmente raros, mas como a procura é muito grande já são produzidos rubis artificialmente que são comparativamente baratos.
As gemas de rubi bruto são valorizadas de acordo com várias características incluindo tamanho, cor, claridade e corte. Todos os rubis naturais contêm imperfeições. Por outro lado, rubis artificiais podem não conter imperfeições. Alguns rubis manufaturados têm substâncias adicionadas a eles para que possam ser identificados como artificiais, mas a maioria requer testes gemológicos para determinar a sua origem.

Os diferentes tipos de rubis:
rubi lapidado com inclusões naturais
Existem diferentes tipos de pedras preciosas rubi existentes no mercado. Os vários tipos de rubi normalmente recebem o seu nome devido a área de mineração.

Rubi da Birmânia
Rubis birmaneses são um dos rubis de alta qualidade, bem como um dos mais procurados rubis birmaneses têm uma cor vermelho escuro devido à quantidade de cromo, embora às vezes eles podem ter dicas de azul ou rosa. Rubis birmaneses vêm de regiões específicas, nomeadamente Mogok no norte da Birmânia e Mong-Hsu a leste de Mandalay. Todos os rubis têm manchas; na verdade, todas as pedras naturais fazem. Se não há manchas, não é uma pedra natural. Os rubis birmaneses têm menos defeitos de todos.
Origem: Myanmar

Rubi da Tailândia (Thay Ruby)
Rubis tailandeses são perdem apenas para os rubis birmaneses, Eles têm tons mais escuros devido à combinação de ferro e cromo. Os rubis tailandeses também podem ter matizes que variam de marrom a vinho, que também são chamados de rubis de Sião, mas não são tão procurados quanto os birmaneses. Rubis tailandeses vêm da área a sudeste de Bangkok.
Origem: Banguecoque

Rubi da Tanzânia
Na Tanzânia, depósitos de rubi são encontrados em regiões próximas a Songea. A cor desses rubis se assemelha tanto à granada que até os joalheiros muitas vezes ficam desconcertados com sua proximidade. A aparência da pedra rubi da Tanzânia também é bastante semelhante à da pedra Hessonita devido à sua cor.
Foi notado que a intensidade da cor diminui com o tamanho. Portanto, quanto menor o tamanho das pedras de rubi da Tanzânia, mais valiosas elas são. Conforme o tamanho da pedra aumenta, a cor da pedra começa a desbotar.
Estes rubis são menos caros do que os rubis birmaneses e tailandeses.
Origem: Songea

Rubi de Madagascar
Madagascar é outra fonte de rubis top de linha, embora os rubis de Madagascar sejam relativamente novos no mercado. A área de mineração em Madagascar é nas regiões de Andilamena e Vatomandry, onde os rubis podem ser encontrados em uma grande variedade de rochas ígneas diferentes. Existem diferenças nos rubis de cada área. Os rubis da região de Andilamena são melhores quando recebem um tratamento térmico, os de Vatomandry não. Os rubis Vatomandry têm reflexos laranja, vermelho e rosa.
Origem: Andilamena e Vatomandry

Rubi do Afeganistão
Rubis foram extraídos no Afeganistão pelo menos desde o primeiro século. As minas estão nas regiões de Badakshan e Jagdalek. Sabe-se mais sobre os rubis que vêm de Jagdalek, que produz rubis que podem variar de um fraco ao vermelho profundo. Os rubis Jagdaled têm qualidades não encontradas em outros lugares. Eles podem ter um tom arroxeado e um brilho fluorescente.
Origem: Badakhshan e Jagdalek

Rubi Africano
Pedras de rubi africanas são geralmente arroxeadas a vermelho escuro. Rubis africanos vêm em variedades de tamanhos e qualidades. A melhor cor dos rubis africanos é a fina cor vermelha escura.
Origem: Moçambique e Quênia

Rubi de Moçambique:
Embora o Rubi de Moçambique não seja denominado como um Tipo, atualmente, os rubis de Moçambique é que estão dominando o mercado devido a sua alta qualidade. Os depósitos de rubis mais importantes e produtivos na África encontram-se no norte de Moçambique.

Relatos de rubis de alta qualidade no norte de Moçambique começaram a surgir entre 2008 e 2009, perto das aldeias de Maawize e Namahumbire, respectivamente. E quando a Gemfields Plc adquiriu uma participação no depósito de rubis de Montepuez em 2012, os rubis de Moçambique começaram a ter um impacto significativo no mercado global. A produção até hoje tem sido enorme se comparada a qualquer outro depósito de rubis, e algumas das pedras são comparáveis aos lendários rubis "sangue de pombo" da Birmânia.

Então se você perguntar onde no mundo se produzem os melhores rubis?
Você provavelmente irá ouvir que são os rubis da Birmânia, mas isto só se reflete porque é a localidade mais famosa para os rubis. Aliás, os rubis birmaneses sempre foram conhecidos por sua fina cor vermelha fluorescente em qualquer tipo de luz e a cor das pedras birmanesas é muitas vezes dito ser "sangue de pombos". Os rubis birmaneses, com sua rica herança e história, comandam os preços mais altos em todos os leilões de pedras preciosas e jóias, e pedras acima de 3 quilates estão entre as mais raras e caras de gemas em qualquer lugar.
Mas a mineração de rubi birmanesa nunca foi suficiente e os altos preços das pedras refletem em parte isso.
Então um novo gigante na produção de rubis de qualidade surgiu, o Rubi de Moçambique e que o tal já deveria ter atingido o escalão como pertencendo há um novo Tipo de Rubi.

Rubis no Mundo:
Além das localidades e países já mencionados acima, Rubis também podem ser encontrados em:
Rubi de Goiás, Brasil foto de Rui Nunes por mindat.org
Rubi de Goiás, Brasil foto de Rui Nunes por mindat.org

Rubis também foram explorados na Tailândia, no distrito de Pailin e Samlout, no Camboja, Austrália em Queensland, Nova Galles do Sul, Brasil, Colômbia, Índia - Mysore, Namíbia, Japão, Escócia, Madagascar, Malawi na região de Chiradzulu, Nepal, Paquistão, Quênia região de Mangari, Tajiquistão, Vietnã nas províncias de Yen Bai e Nghe, no Sri Lanka os rubis tem os tons mais claros chamados de "safiras rosas", Zimbabue,na Macedônia na Europa continental eles podem ser encontrados principalmente em torno da cidade de Prilep. Os rubis macedónios têm uma cor framboesa única. O rubi também está incluído no brasão macedônio. Ainda na Europa foi encontrado rubis na Suiça (Tessin) e na Noruega. Já na europa insular é encontrado na Groelândia que pertence a Dinamarca. Alguns rubis foram encontrados nos estados norte-americanos de Montana, Carolina do Norte, Carolina do Sul e Wyoming.

Sobre a Espinela:
espinela na matriz de mármore e calcita
Espinela em matriz de mármore e calcita.
Espinela, é uma pedra preciosa vermelha, às vezes é encontrada junto com rubis no mesmo cascalho ou no mármore. Espinelas vermelhas podem ser confundidos com rubis por aqueles que não têm experiência com pedras preciosas. Alguns vendedores de pedras preciosas vendem espinelas com se tratando de Rubi, levando um comprador inexperiente a comprar sem ter o menor cuidado de mandar analisar em um laboratório de gemologia a fim de se ter uma certeza ou um certificado de garantia da pedra.
Porém, os melhores espinélios vermelhos de melhor qualidade podem ter valores próximos de um rubi médio.
Balas ruby é um nome antigo para uma variedade de espinélio de cor rosa.

Imagens de:
Rob Lavinsky, iRocks.com

Fontes:

Recursos Minerais de Timor-Leste

Recursos Minerais e pedras preciosas de Timor-Leste
spinel
A República Democrática de Timor-Leste, vulgarmente conhecida por Timor Leste, compreende a metade oriental da ilha de Timor, as ilhas vizinhas de Atauro e Jaco e Oecussi-Ambeno, um enclave no lado noroeste da ilha no Timor Ocidental indonésio.

Timor Leste é dividido em 13 distritos administrativos. Os distritos estão subdivididos em 65 subdistritos, 442 sucos (aldeias) e 2225 aldeias (aldeias).

Distribuição de minerais metálicos em Timor Leste
Recursos Minerais de Timor-Leste

Distribuição de minerais não metálicos em Timor-Leste
Recursos Minerais de Timor-Leste

Jade branco Timor Leste
Giok Putih Timor Leste - Jade branco de Timor Leste
(Giok Putih Timor Leste)

Dada a ausência de mais informações no Mindat sobre Timor Leste, aqui ficam alguns dados sobre a sua geologia.

Geologia de Timor Leste:
breve resumo por P. F. T. Kaul
Instituto Brasileiro de Geografia e Estatística (IBGE),
Florianópolis, SC, Brasil - Out/04.

As rochas e os sedimentos do Timor-Leste constituem dois domínios geológicos: um, chamado de Autóctone, constituído por rochas e sedimentos gerados “in situ” ; outro, designado de Alóctone, composto por rochas formadas alhures, porém transportadas às regiões onde atualmente se encontram como conseqüência de intensas movimentações tectônicas.
O Domínio Autóctone distribui-se por todo o país, inclusive no enclave de Oecussi. É predominante, entretanto, na metade leste do território timorense (região que se estende, aproximadamente, do meridiano que passa em Manatuto àquele do ilhéu Jaco), tendo presença expressiva no sudoeste deste território (áreas de Bononaro e Ainaro e respectivas vizinhanças). Ele consiste numa sucessão de diferentes tipos de rochas, formadas desde o Permiano Inferior, há aproximadamente 280 milhões de anos, até o Pleistoceno, há cerca de 2 milhões de anos, com lacuna provável de tal formação de rochas no período Cretáceo (intervalo aproximado dos 140 aos 70 milhões de anos). São folhelhos, intercalados por calcários e, eventualmente, por arenitos, conglomerados e lavas básicas. Integram-no, também, consistindo sua porção mais jovem, depósitos quaternários recentes: sedimentos fluviais e marinhos, além de recifes corálicos elevados. Os sedimentos marinhos correspondem às planícies costeiras, que dominam na costa sul do país. Os recifes corálicos elevados são construções calcárias constituídas principalmente por exoesqueletos de corais, que ocorrem nas áreas de Baucau e Los Palos, bem como no ilhéu Jacó.
O Domínio Alóctone corresponde a um “complexo carreado” que se estende, principal-mente, no noroeste do país – região de Balibo, Ermera, Dili, Aileu, Laclubar, etc., ocorrendo também no enclave de Oecussi. Ele é constituído por rochas metamórficas de baixo e médio grau de metamorfismo, além de rochas ígneas, formadas, todas elas, do Permiano Inferior, há cerca de 280 milhões de anos, ao Eoceno, há mais ou menos 50 milhões de anos. Trata-se de xistos sericíticos, micaxistos com biotita, anfibolitos, mármores, diversos tipos de calcário, margas, brechas vulcânicas e rochas eruptivas.
Os bens minerais do país ocorrem em todo o território nacional, correspondendo, em grande maioria, a ocorrências cuja potencialidade não está ainda definida:
- Minerais metálicos:
cobre, chumbo/zinco, ouro, prata, manganês.
- Minerais não-metálicos:
talco, magnesita, fosforita.
- Materiais de construção:
rochas carbonáticas (calcários, dolomitos e mármores), argilas, caulim, areia, cascalho.
- Combustíveis fósseis, na plataforma continental do mar de Timor:
petróleo e gás natural.

Minerál sira ne’ebé mak iha país nia laran
Minerais e pedras preciosas em Timor-Leste:
Calcopirite, Cromita, Cobre nativo, Dolomite, Enstatite var: Bronzite,
Fluorapatite, Galena, Ouro, Grafite, Gesso, Heazlewoodite,
Caolinite, Laurite, Milerite, Molibdenite, Nickeline, Opala var: Kalimaya, Pentlandite,
Platina nativa, Pirita, Pirrotita, Quartzo, Prata nativa, Espinel, Enxofre,
Talco, Talnakhite e Wollastonite.

Os 27 minerais em Timór-Leste descritos acima estão catalogados no banco de dados de minerais do mindat.org
Nickeline
Potencial Mineiro para Explorar em Timor-Leste:
https://www.pecc.org/resources/minerals

Um breve resumo da ocorrência dos principais minerais de Timor Leste

Cobre
A mineralização ocorre como sulfetos maciços, veios contendo calcopias e pirita em unidades ultra-básicas, com extensa alteração serpentina e evidência de diorito / diabásio intrusivo.
Na área de Ossual (distrito de Baucau) a amostragem da Allied Mining Company (Wittouck, 1937) retornou valores de 10% Cu, 3 g / t Au e 170 g / t Ag.

Ouro
A mineralização de ouro tem sido observada em várias formas como quartzo,
veios calcite de quartzo e calcite hospedados por xisto/ardósia ou xisto. O veio é purificado e mineralizado com ouro. Na área de Hilimanu a mineralização ocorre na rocha ígnea metamorfoseada. A mineralização estão associadas a veios de quartzo (0,5 - 12 m de largura) contendo calcopirita, limonita e calcedônia. Amostras de análise indicam o teor médio de 0,5 g / t Au e 50 g / t Ag.

Cromita
Os depósitos de cromita foram reportados em Baucau, Hili Manu
(Distritos de Manatuto) e Manufahi. Os depósitos foram encontrados como mineralização primária nos hospedeiros serpentinitos. A cromita nos distritos de Manatuto é semelhante à mineralização de cromita nos corpos ofiolíticos de allochtone encontrados no cinturão Circum Pacific nas Filipinas, Nova Caledônia e Kalimantan, na Indonésia. A qualidade da cromita é boa, com notas entre 36% e 51% de Cr2O3. Quanto ao grau, 80% dos principais depósitos do mundo têm entre 33% e 52% de Cr2O3.

Manganês
Os depósitos de manganês foram descobertos em vários locais, como
Vemmasse, Talamata, Venilale (distrito de Baucau), Uato Carabau
(Distrito de Viqueque). Os depósitos são intercalados dentro do vermelho
xisto e associado com o calcário da Formação Bobonaro.
Os depósitos de manganês são compostos principalmente de minerais pirolusite
a faixa de notas entre 84 - 94,5% MnO2.

Fosfato
Os depósitos estão localizados em Daemena, Abo (distrito de Quelica e Baucau),
e Laleia (distrito de Manatuto). Os depósitos de fosfato ocorrem no
cascalho não consolidado - material pedregoso semelhante ao
Ainaro Gravel. A análise dos resultados obtidos na área de Abo
revelou o ensaio significativo variando de 9,97% a 31% de P2O5.

Bentonita
Os depósitos de argila estão intertravados da argila de Bobonaro
Formação de argila escamosa e localizada em Venilale (distrito de Baucau),
Bobonaro (distrito de Bobonaro). Na aldeia de Mulia-Quelicai (Baucau
distrito), o valor do inchaço foi registrado entre 371 até 1829 x
volume seco. O potencial da reserva de minerais é de aproximadamente
115.570.000 metros cúbicos.

Mármore
O depósito foi registrado em Cablaci-Same (Manufahi District),
Laclo (distrito de Manatuto) e Builale (distrito de Viqueque). Em Laclo,
a reserva mineral é estimada em pelo menos 5.000.000 metros cúbicos.

Gesso
Os depósitos de gesso estão associados a argilitos de
Formação Bobonaro Scaly Clay. O depósito está localizado em Laleia-Obrato (distrito de Manatuto), o resultado de uma área investigada de 50 ha de poço revelou que a reserva mineral é de aproximadamente 400 toneladas.

Conclusões
1. Geologicamente, o potencial mineral de Timor-Leste é muito
atraente para futura exploração mineral e desenvolvimento
atividades.
2. Os mais atraentes potenciais minerais metálicos de Timor são o cobre, o ouro e a prata.
3. O negócio de mineração de minerais metálicos é de alto risco e
alto capital, por isso é melhor feito pelo setor privado como é
precisa de recursos financeiros e técnicos sólidos.
4. Minerais não-metálicos, como mármore, argila, areia, cascalho,
etc, têm um grande potencial em Timor-Leste.
5. O crescimento e desenvolvimento da mineração de um país
a indústria é determinada não só pelo seu potencial mineral
sozinho, mas sim, pelas políticas do governo na criação de
clima de negócios para incentivar o investimento.

Fontes:

Comment et où trouver de l'or en Suisse

Gisements d'or en Suisse
La Suisse est un pays riche en mines pauvres!
gold in Suisse
Dans le Sud, vers 1890 on a pu croire à « une nouvelle Californie au
Tessin ». L'exploitation aurifère industrielle a toutefois cessé en 1897.
Tous les cours d'eau entourant le Lac Léman ont aussi été fouillés.
La région de Disentis, vallée supérieure du Rhin (Canton des
Grisons) est riche en minéraux. Les gisements d'or de Disentis sont connus depuis 1672.
En 1990, on a redécouvert une région aurifère de 30 km2 dans le
secteur de Disentis.
La plus grande pépite d'or suisse (123 g) y a été trouvée en 1997
mais déjà, une pépite de 48,77g en 1996 et une autre de 20 g avaient été découvertes.
Les « filons d'or » de Disentis se trouvent à l'état de minerai microscopique dans l'ardoise.
La teneur en or des sédiments du Rhin est comprise entre 0,7 et 3 g par tonne.

Carte d'or de la Suisse
Comment et où trouver de l'or en Suisse - Carte d'or de la Suisse
 Gisement de filon d'or - Concentration d'or alluvial - Terrain d'altitude inférieure à 2000m

L'extraction de l'or du Rhin remonte à une époque ancienne car on connait en 776, une charte où le droit de faire le lavage d'or est accordé à un monastère. Il est probable que le Rhin faisait partie des rivières desquelles les gaulois extrayaient l'or (cité par Diodore de Sicile, au 1°s av JC).
Dans la vallée du Rhin moyen, c'est entre Bâle et Mannheim qu'il est le plus aurifère. L'or s'y rencontre sous forme de paillettes très minces, aux contours arrondis dont le diamètre n'excède pas 1 mm.
La richesse en or est comprise entre 0,23 et 1 g par tonne de sédiments.
En pays de Bade, 366 kg d'or auraient été recueillis entre 1748 et 1874.
Les livraisons d'or auraient permis de frapper entre 1807 et 1841, 27987 ducats d'un poids moyen de 3,6 g.
En 1831, une des années les plus productives, on a récolté 12,523 kg d'or des deux cotés du Rhin.
L'origine de l'or alluvionnaire peut être rapporté à trois catégories : filons d'or, or engagé dans des roches massives magmatiques et amphibolites,
or disséminé dans des roches de type schistes. La forme en lamelles très minces de l'or du Rhin est un argument en faveur d'une origine en terrains
schisteux et quartzeux, ce qui correspond à la région de Disentis (Rhin antérieur).
On trouve aussi de l'or dans des cailloux de quartzite comme en témoigne le galet de quartzite aurifère découvert en 1849 dans le cours de l'Ill et
exposé au musée de minéralogie de Strasbourg.
L'or du Rhin proviendrait essentiellement du massif cristallin de l'Aar, affluent du Rhin qui s'y jette à Koblentz.
Lors de la formation de molasse par érosion des Alpes (-50Ma, Miocène), l'or y est stocké secondairement dans des conglomérats, grès et bancs
marneux (formation de molasse de Napf) puis emporté par le cours d'eau.
La fragmentation des galets et des graviers libère peu à peu de nouvelles quantités d'or. Le fleuve transporte des particules de taille de plus en plus
réduites dont la sédimentation est favorisée par le ralentissement du courant.
Au cours de la seconde moitié du 19°s, la correction du cours du Rhin entraina la suppression des méandres et l'accélération du courant,
défavorisant les atterrissements aurifères susceptibles d'exploitation.

Gisements d'or alluvionnaire en Suisse
En Suisse, l'or se trouve en de nombreux endroits, comme le montre la carte ci-dessous. Souvent, cependant, on ne rencontre l'or seulement sous la forme de quelques infimes traces.
Gisements d'or alluvionnaire en Suisse
Les emplacements décrits dessous fournissent les meilleures chances pour l'orpailleur amateur déterrer des paillettes de l'or avec les outils simples, tel qu'un goldpan et une pelle. Le livre "Gold in der Schweiz" (en allemand seulement) fournit une description beaucoup plus détaillée de ces emplacements plus beaucoup plus. En outre, une introduction aux types géologiques de gisements d'or suisses et les techniqes de prospection est fournie.

La région du Napf
Historiquement, l'or dans la région Napf en Suisse Centrale est supposé être le premier gisement d'or connu en Suisse. Les "Napfgold" ont pu être connus par le Helvets (une tribu Celtique qui vit dans le territoire de la Suisse d'aujourd'hui avant Le Christ) et les Romains. Aujourd'hui, les ruisseaux et rivières de la région Napf sont aussi bien connues aux orpailleurs amateurs. Le décor naturel non touché du Prealps suisse et la possibilité de trouver une paillette d'or dans les graviers de ruisseau rapidement fait la région Napf une parfaite localité de l'or. À cause de l'histoire de l'or intense et les gens de l'affection tiennent pour les prospecteurs, nous avons consacré la région Napf sa propre site (L'or alluvionnaire en Suisse).

La Suisse de l'est
La Suisse de l'est représente une grande région avec alluvions fluviales et glaciaires. Les alluvions aurifères des Cantons d'Appenzell, Saint Gall, Thurgau, et Zurich étaitent inconnues avant le géologue Franz Hofmann de Schaffhausen a fait travail de champ intensif entre 1965 et 1985 là. Il a goûté beaucoup de rivières et le gravier dénoyaute scientifiquement et a découvert cet or alluvionnaire s'est été étendu sur la Suisse de l'est. Il a identifié trois types de sources de l'or alluvionnaire:

Les glaciers qui couvraient complètement la Suisse de l'est pendant les époques glaciaires ont déplacé l'or des Alpes.
Les deltas de la rivière tertiaires ont formé la région Napf mais les paillettes d'or aussi apportés de la Suisse Central à la Suisse de l'est pas seul et d'Autriche à la Suisse de l'est.
Les alluvions récentes ont été formées après que les dépôts glaciaires aient érodé.
Quelques localités prometteuses pour les orpailleurs amateurs sont trouvées dans la rivière de Rhin proche de Schaffhausen, les ruisseaux autour Saint Gall (Glatt, Sitter, Steinach, Goldach), et quelques rivières dans le Canton de Zurich (Töss, Kemptnertobel).

C'est aussi M. Hofmann qui était le premier chercher d'or qui suit de vieux contes et des sagas. Les sagas qui disent des dépôts d'or déterrés presque riches ont existé sur la Suisse pour beaucoup de cent années. Leurs sources sont inconnues. M. Hofmann était capable de montrer que quelques-unes de ces sagas contiennent un morceau de vérité, cependant. L'or existe dans quelques-uns de ces emplacements vraiment.

Bâle
Le Rhin entre Bâle et Mayence (Allemagne) a été une source bien connue pour l'or alluvionnaire depuis le Moyen Âge. Les orpailleurs professionnels vivaient fermé de l'or du Rhin entre les 14e et le 19e siècle sur le territoire allemand et français. Il n'y a aucune évidence historique pour l'orpaillage dans ou autour de la ville de Bâle (territoire suisse). Cependant, l'or alluvial se trouve dans les petits ruisseaux autour de la ville. Ces petites traces de l'or reviennent aussi à matière du glacier déposée pendant les Âges glaciaires.

La Suisse de l'ouest
Goldnuget, Schweiz - Gold Nugget, Switzerland
Goldnuget, Schweiz - Gold Nugget, Swizerland
La Suisse de l'ouest, semblable à la Suisse de l'est, est une grande région d'or alluviale. L'or vient encore de sources glaciaires de la période glaciaire. Ce temps c'était le glacier de Rhône qui a érodé des filons d'or dans le Canton de Valais et l'a transporté à Genève et Fribourg.

En plus du vieil or bien connu mine de Salanfe et Gondo, l'or se trouve dans les petites veines proche de Verbier, Nendaz, Iserables, Naters, et dans les vallées d'Anniviers et Binn. Les géologues (Nicolas Meisser de Lausanne, Stephan Ansermez de La Tour de Peilz, G. Della Valle de Genève et autres) ont découvert et récemment décrit beaucoup de ces petits gisements.

Autre que la région Napf, l'or alluvionnaire autour de la ville de Genève est le meilleur gisement d'or connu en Suisse. Son histoire revient à 1397 quand un orpailleur a sollicité à la ville de Genève une concession pour creuser pour l'or. Beaucoup de concessions ont été accordées dans le 15e et 16e siècle. Dans les 1930s, J.J. Pittard a fait des recherches sur les gisements d'or de la région de Genève scientifiquement.
Les localités renommées sont:
La rivière Allondon: Un emplacement de grand décor mais en été chanté par weekenders de la ville proche de Genève.
La rivière Arve: La rivière a ses sources en France. L'or n'est pas comme facile de trouver comme dans l'Allondon, probablement à cause du sable fin et normalement haut montant d'eau.
La rivière Versoix: Le décor est semblable à l'Allondon, mais plus petit et plus sauvage. Quelquefois le soubassement du grès est exposé.
Pittard indique que les paillettes d'or de la région de Genève sont 2 à 3 mm dans dimension approximativement. Le contenu de l'or des rivières de Genève varie de 0.1 à 0.4 g/m3.

Disentis et la Surselva
La région Surselva autour de Disentis dans le Canton Grisons est riche dans les minéraux. Les gisements d'or de Disentis ont été sus depuis 1672 mais ne jamais considérés important. En 1982, le géologue David Knopf suisse a proposé qu'une compagnie de l'exploration canadienne, Narex Inc International, entreprend drillings de l'épreuve dans la région parce qu'il a observé une ressemblance de la région au Hemlo district d'or riche. Les drillings ont identifié une région aurifère de 30 km2 le long de la rivière de Rhin Supérieure. L'or satisfait de 0,7 à 3 g/t a été trouvé mais aucune opération minière commerciale n'a été commencée. Les activités des entreprises minières ont attiré les orpailleurs amateurs et quelques pépites exceptionnelles agréables ont été trouvées dans les rivières depuis lors.

Peter Bölsterli mit dem 123 g-GoldnuggetLa plus grande pépite de l'or suisse a été trouvée en 1997 par Peter Bölsterli proche de Disentis (voyez l'image). Il pèse 123 grammes. Précédemment, une 48.77 pépite g (trouvez par August Brändle, 1996) et une 20 g pépite a été trouvée. Plusieurs pépites de 1 à 10 g sont sues. Les filons d'or de Disentis se trouvent comme minerai microscopique dans l'ardoise non plus, comme or natif dans quarz veine, ou très rarement comme cristaux de l'or. 

L'orpailleur amateur René Reichmuth a trouvé un grand filon d'or en automne 2000, le plus extraordinaires su en Suisse jusqu'à maintenant. La découverte de 15 morceaux hors de ce filon du quartz inclut 1.0 à 1.4 kg d'or approximativement.

Présence de filons d'or en Suisse
filons d'or en Suisse
"La Suisse est riche dans mines pauvres" qu'un géologue suisse célèbre a affirmé une fois. L'or a été miné dans quatre emplacements en Suisse. Toutes ces mines sont abandonnés aujourd'hui. Galeries, arbres, et ruines des bâtiments des mineurs restent encore et sont un héritage culturel intéressant d'histoire de l'or suisse.

Salanfe (Valais)
Les arsenopyrites aurifères déposés de la montagne Luisin proche de Martigny  (Valais) ont été minés entre 1904 et 1928. La mine est haute dans les montagnes (2157 m) et souvent couverte par la neige.

Gondo (Valais)
La principale période minière dans Gondo (Valais) était entre 1890 et 1897. Un total de 73 or invente ("Goldvreneli") a été fabriqué de son or. L'or se toruve comme inclusions microscopiques dans la pyrite du granite qui appartient au Monte district Rosa.

Astano (Ticino)
L'or se trouve dans la région Malcantone dans les minerais de l'arsenopyrite. Beaucoup de petite datation des noyaux est trouvée dans cette région en arrière au Moyen Âge. La mine d'or d'Astano a opéré entre 1937 et 1961.

Calanda (Grisons)
La mine dl'or appelée "le Soleil d'Or" proche de Chur dans la montagne Calanda a été opérée entre 1809 et 1856. Un total de 70 or invente ("Bündner Dublonen") a été fabriqué de cet or.

Tourisme d'or en Suisse
Orpaillage dans le Rhin
How and Where to Find Gold in Switzerland
Ruée vers l'or et aventure dans la nature sauvage près de la source du Rhin.

Les gorges du Rhin, également connues sous le nom de «Grand Canyon suisse», fascinent les randonneurs et les chevrons du monde entier.
Avec une bassine dorée, une pelle à main, des bottes à genou et un verre pour l'or, vous serez guidé vers les sites où se trouvent les plus grandes pépites d'or suisses. Programme d'une demi-journée ou d'une journée avec ou sans barbecue suisse de la ruée vers l'or.
A plus dans:

L'or résiduel de la Suisse
Des millions d'euros d'or et d'argent évacués dans les eaux usées
gold particles in water
Une étude pour le moins surprenante révèle la présence de kilos d'or et de tonnes d'argent dans les eaux usées de Suisse.

Des millions d’euros d’or et d’argent évacués dans les eaux usées ? L’histoire est digne d’un scénario hollywoodien et, pourtant, c’est en Suisse que cela se déroule. Selon une étude, des kilos d’or et des tonnes d’argent seraient rejetés dans les eaux usées helvètes chaque année. Explications.
C’est une info pour le moins insolite révélée par des chercheurs de l’institut de l’eau Eawag. D’après leurs calculs, chaque année, 43 kilos d’or et 3 tonnes d’argent disparaissent dans les effluents et les boues d’épuration de Suisse ; une valeur totale qui s’élève à 2,6 millions d’euros.
Ces résidus proviennent pour la plupart des raffineries d’or de la région du Tessin tandis que les particules d’argent sont issues de l’industrie chimique et médicale. L’étude affirme que :

« Dans certaines zones du Tessin, la concentration d’or est tellement importante qu’il serait opportun de la recycler. »

Pour l’heure, le recyclage n’est pas encore rentable. Les chercheurs affirment également que les concentrations ne représentent pas de danger pour l’environnement.
La Suisse abrite en effet les plus grandes raffineries d’or au monde, un or qui représente plus d’un quart de toutes les exportations du pays.

De quoi donner envie de revêtir sa panoplie de chercheur d’or…

Musée de la mine d'or de Sessa
La dernière mine d’or de Suisse ser ouverte au public
Dans le Malcantone, région à l’ouest de Lugano, un des plus importants districts miniers de Suisse, on y extrayait de l’or jusqu’en 1954. La mine de Sessa, après un demi-siècle dans l’oubli, ser ouverte au public.
Au cœur du Malcantone, le village de Sessa est un petit joyau de par son architecture et son paysage. Juste au-dessus du village se trouve un ancien gisement aurifère, le plus important de la région. En 1856, après des décennies d’extraction «sauvage», un ingénieur italien de Sion obtenait une concession d’exploitation du Conseil d’Etat tessinois et ouvrait la mine «La Costa». Pendant près d’un siècle, jusqu’à sa fermeture définitive en 1954, des tonnes de métaux (or, argent et plomb notamment) en ont été extraits et jusqu’à 400 mineurs y ont travaillé. Voilà qu’elle va connaître une nouvelle vie, puisqu’elle sera ouverte au public en 2017.

L´or en France

Rivieres qui ont l´or en France

L´or en Belgium

Sources d'information:

Gold International Day

The International Gold Day
(Domain for sale: goldinternationalday.com)
gold price, gold exchange, money exchange, NYSE American, The New York Stock Exchange
Gold International Day
Did you know that there is a day dedicated to gold?
Gold Day is celebrated on September 7 (7.9).
This is the atomic number of gold on the periodic table.
gold simbol in periodic table
Symbol: Au
Boiling point: 2700 ° C
Melting point: 1064 ° C
Atomic mass: 196.96657 or ± 0.000004 u
Relative Density: 19.33 g / cm3
Electron configuration: [Xe] 4f14 5d10 6s1

Gold is a chemical element with the symbol Au (from the Latin: aurum) and the atomic number 79, which makes it one of the elements of greater atomic number that occurs naturally. In its purest form, it is a shiny, slightly reddish, dense, soft, malleable and ductile metal. Chemically, gold is a transition metal and a member of group 11. It is one of the least reactive chemical elements and is solid under standard conditions. Gold usually occurs in free (native) elemental form, such as nuggets or grains, in rocks, veins and alluvial deposits. It occurs in a number of solid solutions with the native silver element (like electrum) and also naturally bound with copper and palladium. Less commonly, it occurs in minerals as compounds of gold, often with tellurium (gold tellurides).

Gold is resistant to most acids, although it dissolves in water, a mixture of nitric acid and hydrochloric acid, which forms a soluble tetrachlorourate anion. Gold is insoluble in nitric acid, which dissolves silver and base metals, a property that has long been used to refine gold and confirm the presence of gold in metallic objects, giving rise to the term acid test. Gold also dissolves in alkaline cyanide solutions, which are used in mining and electroplating.

Gold is attacked and dissolves in alkaline solutions of potassium or sodium cyanide, forming gold-cyanide saline - a technique that has been used in the extraction of metallic gold from ores in the cyanide process. Gold cyanide is the electrolyte used in the commercial electrodeposition of gold into basic metals and electroforming.
Gold dissolves in mercury, forming amalgam alloys, but this is not a chemical reaction.

Gold is a relatively rare element, it is a precious metal that has been used for minting coins, jewelry and other arts throughout recorded history. In the past, a gold standard was often implemented as a monetary policy, but gold coins were no longer minted as currency in the 1930s, and the world gold standard was abandoned by a fiduciary monetary system after 1976.

The worldwide consumption of new gold produced is used in about 50% for jewelry, 40% is used for investments and 10% is used in the industry. The high malleability of gold, ductility, corrosion resistance and most of the chemical reactions and conductivity of the electricity led to its continuous use in corrosion resistant electrical connectors in all types of computerized devices (its main industrial use). Gold is also used in infrared protection, colored glass production, gold foil and tooth restoration. Certain gold salts are still used as anti-inflammatories in medicine.

The origin of gold
native gold nugget
Theories of celestial origin
It is believed that gold was produced in the nucleosynthesis of supernovae from the collision of neutron stars and has been present in the dust from which the solar system formed. As the Earth was melted when it was formed, almost all the gold present on the early Earth probably sank into the planetary core. Therefore, it is believed that most of the gold that is in the Earth's crust and mantle has been delivered to Earth later because of the impact of asteroids during the last heavy bombardment about 4 billion years ago.

Traditionally, gold is believed to have formed by the rapid neutron capture process in supernova nucleosynthesis, but more recently it has been suggested that gold and other elements heavier than iron can also be produced in quantity by the process in the collision of neutron stars. In both cases, the satellite spectrometers only indirectly detected the resulting gold: "we have no spectroscopic evidence of what [such] elements actually were produced," wrote author Stephan Rosswog. However, in August 2017, signatures of heavy elements, including gold, were observed by gravitational wave detectors and other electromagnetic observatories in the event of neutron star fusion GW170817. Current astrophysical models suggest that a single fusion event of neutron stars generated between 3 and 13 terrestrial gold masses.

The asteroid that formed the Vredefort crater 2,020 billion years ago is often credited with sowing the Witwatersrand basin in South Africa with the richest gold deposits on Earth. However, the gold rocks of the Witwatersrand were established between 700 and 950 million years before the Vredefort impact. These gold-bearing rocks had been covered by a thick layer of Ventersdorp lavas and the Transvaal Rocks Supergroup before the meteor was struck. What the Vredefort impact did, however, was to distort the Witwatersrand basin in such a way that the gold-bearing rocks were brought to the present erosion surface at Johannesburg in the Witwatersrand within the original 300-km-diameter crater rim by the meteor attack. The discovery of the depot in 1886 launched the Witwatersrand Gold Rush. About 22% of all the gold that exists today on Earth was extracted from these Witwatersrand rocks.

The Alchemy of Gold
alchemy gold symbol
Is it possible to make gold?
Gold is only found in nature, yet alchemists all over the world and for several centuries have tried and still try to transmute lower metals into gold. It has now been possible to transmute bismuth and lead into gold, but the processes for this transmutation are very costly to exceed the large hundreds of dollars the gram of gold, and a large investment is not compensatory.
Alchemists have tried to transmute gold for centuries, but it seems that modern alchemists have succeeded through current technologies.

The Gold Microbial Alchemy
Gold Microbial Alchemy
Bacteria that can produce gold
Scientists at Michigan State University have identified a bacterium capable of secreting gold. Cupriavidus metalliduran not only survives toxic concentrations of gold chloride but thrives. By feeding a colony, Kazem Kashefi and Adam Brown led the microbes to create 24-carat gold nuggets - that is, pure gold.
But bacteria do not act alone
Cupriavidus metalliduran acts together with the species Delftia acidovorans, acts on the formation of gold nuggets, by precipitation of metallic gold from the solution of gold chloride (III), a compound highly toxic to most other microorganisms.

Delftia acidovorans is a gram-negative, non-spore, aerobic, rod-shaped bacterium known for its ability, in conjunction with Cupriavidus metallidurans, to produce pure gold nuggets.

Gold Characteristics
Gold is the most malleable of all metals; a single gram can be beaten until it is turned into a 1-square-meter sheet. A gold leaf can be beaten sufficiently to become a semi-transparent sheet. The transmitted light appears in blue-green because the gold reflects strongly yellow and red. These semi-transparent sheets also strongly reflect infrared light, making them useful as infrared shields (radiant heat) on visors of heat-resistant clothing, and visors for space suits. Gold is a good conductor of heat and electricity.

Gold has a density of 19.3 g / cm 3, almost identical to that of tungsten at 19.25 g / cm 3; As such, tungsten has been used in forging gold bars, for example, by plating a tungsten bar with gold, or by picking up an existing gold bar, by sticking and replacing the gold removed with tungsten rods. In comparison, the density of the lead is 11.34 g / cm 3 and that of the denser element, the osmium, is 22.588 ± 0.015 g / cm 3.

Abundance and Attainment in its Native State
On Earth, gold is found in ores on rock formed from pre-Cambrian times.
Because it is relatively inert, it can be found as metal, sometimes as large nuggets, but is usually found in small inclusions in some minerals, such as quartz, metamorphic rocks and alluvial deposits originating from these sources.
gold in quartz
Gold is widely distributed, and is often associated with quartz and pyrite. It is common as impurity in many ores, from where it is extracted as a by-product.

Gold sometimes occurs in conjunction with tellurium (gold telluride) as the minerals calaverite, krennerite, nagyagite, petzite and silvanite, and as the rare maldonite bernutida (Au2Bi) and the antimonide aurostibito (AuSb2). Gold also occurs in rare alloys with copper, lead and mercury: the minerals auricupride (Cu3Au), novodneprite (AuPb3) and weishanite ((Au, Ag) 3Hg2).

The gold is extracted by a process called cyanide leaching. The use of the cyanide facilitates the oxidation of the gold forming (CN) 22- in dissolution. To separate the gold from the solution, the reduction is carried out using, for example, zinc. It has been tried to replace the cyanide with another binder due to the environmental problems it generates, but they are not profitable or they are also toxic.

Recent research suggests that microbes can sometimes play an important role in the formation of gold deposits, transporting and precipitating gold to form grains and nuggets that accumulate in alluvial deposits.

Another recent study said that water failures evaporate during an earthquake, depositing gold. When an earthquake strikes, it moves along a fault. Water often lubricates faults, filling fractures and movements. About 10 km below the surface, under incredible temperatures and pressures, the water carries high concentrations of carbon dioxide, silica and gold. During an earthquake, the failed race suddenly opens more. The water inside the emptiness vaporizes instantly, making the steam flow and forcing the silica, which forms the quartz mineral, and the gold of the fluids to the nearby surfaces.

Gold in the oceans
All the world's oceans contain gold
gold in ocean
Gold is scattered throughout the earth's crust in a very low average concentration (5 grams in 1000 tonnes), and still lower in the oceans (from 0.1 μg / kg to 2 μg / kg), where it is estimated that there are billions of tons of gold, but of exploitation economically unfeasible by the current methods (a trillion liters of sea water contain 120 kg, or 1 kilo in more than 8.3 billion liters. usually above 3 grams per ton, if the same content were found in the sea, 1 trillion liters could supply 3,000 tons of gold.
sea gold extration plant test
The deep waters of the Mediterranean contain slightly higher concentrations of gold (100-150 femtomol / L) attributed to dust and / or rivers or blown by the wind.

Different Colors of Gold in Gold Alloys
gold alloys table
The following gold medals are recognized worldwide: 375, 500, 583, 585, 750, 958, 996, 999.9 (used in the aerospace industry). The gold (alloyed) blend is most often found under No. 583. The alloys of this test may have different colors, depending on the amount and composition of the metals. For example, if the gold alloy of test nº 583 (58.3% gold) contains about 36% silver and copper 5.7%. This alloy has a slightly green hue if it is 18.3% silver and 23.4% copper - it turns pink if it is 8.3% silver and 33.4% copper - one color reddish. Gold with Proof # 958 is three components, plus gold contains silver and copper and is usually used to make wedding rings.

This alloy has a yellow-strong color and is close to pure gold color. In alloy # 750 there is also copper and silver, but sometimes palladium, nickel or zinc can be used. It has a yellowish-green color, also reddish tones to white. This alloy is easily diffused, but if it contains more than 16% copper the color gradually loses its brightness. Test No. 375 usually contains: 37.5% gold, 10.0% silver, 48.7% copper, 3.8% palladium and is used to make alliances. There is also extensive use of "white gold" which contains:
a) gold alloy No. 583: silver 23.7-28.7%, palladium 13.0-18% or nickel 17%, zinc 8.7%, copper 16%;
b) in gold alloy No. 750: silver 7.0-15.0%, palladium up to 14%, nickel up to 4%, zinc up to 2.4% or nickel 7.5-16.5%, zinc 2.0 -5.0% and copper up to 15%.

The Gold in the jewelry
Because of the softness of pure gold (24k), it is usually bonded with basic metals for use in jewelry, changing its hardness and ductility, melting point, color and other properties. Lower carat alloys, typically 22k, 18k, 14k or 10k, contain higher percentages of copper or other base metals or silver or palladium in the alloy. Nickel is toxic and its release of white gold from nickel is controlled by legislation in Europe. Palladium-gold alloys are more expensive than nickel alloys. High-carat white gold alloys are more resistant to corrosion than pure silver or sterling silver.
japan traditional art in jewelry
Mokume-gane is a Japanese machining procedure that exploits the color contrasts of gold between colored gold-plated alloys to produce decorative grain-wood effects.
Mokume-gane translates closely to "wood grain metal" or "wooden eye metal" and describes the way the metal takes on the appearance of the natural wood grain.

About Soldering Gold in Jewelry
Gold welding is used to join gold jewelry components by high temperature brazing or brazing. If the work should be of branded quality, the gold solder alloy should match the fineness (purity) of the work, and the alloy formulas are manufactured to match yellow and white gold color. Gold welding is usually done in at least three bands of melting point referred to as Easy, Medium and Hard. Using high melting solder followed by progressively lower melting welds, goldsmiths can assemble complex items with several separate welded joints. Gold can also be made online and used in embroidery.

Gold in Electronics
intel c4004
Only 10% of the world's new gold consumption is intended for industry, but by far the most important industrial use for new gold is in the manufacture of corrosion-free electrical connectors in computers and other electrical devices. For example, according to the World Gold Council, a typical cell phone may contain 50 mg of gold.

Although gold is attacked by free chlorine, its good conductivity and general resistance to oxidation and corrosion in other environments (including resistance to non-chlorinated acids) have led to its widespread industrial use in the electronic age as a thin layer coating on electrical connectors , thus ensuring a good connection. For example, gold is used in the most expensive electronic cable connectors such as audio, video and USB cables. The benefit of using gold over other metal connectors, such as tin in such applications, has been debated; gold connectors are often criticized by audio-visual experts as unnecessary to most consumers and viewed simply as a marketing trick. However, the use of gold in other applications in sliding electronic contacts in highly humid or corrosive atmospheres, and in use for contacts with high cost of failure (certain computers, communication equipment, spacecraft, jet engines) is very common.
motorola vintage transistor gold wire
In addition to sliding the electrical contacts, gold is also used in electrical contacts due to its resistance to corrosion, electrical conductivity, ductility and lack of toxicity. The key contacts are usually subjected to a stronger corrosion stress than the sliding contacts. Thin gold wires are used to connect semiconductor devices to their housings by a process known as wiring.

The concentration of free electrons in gold metal is 5.91 × 1022 cm3. Gold is highly conductive of electricity and has been used for electrical wiring in some high energy applications (only silver and copper are more conductive by volume, but gold has the advantage of corrosion resistance). For example, gold electrical wires were used during some of the Manhattan Project atomic experiments, but large high-current silver wires were used in the boiler isotope separator magnets in the design.

It is estimated that 16% of the world's gold and 22% of the world's silver are contained in electronic technology in Japan.

The gold in the Bible
Gold is often mentioned in the Old Testament, beginning with Genesis 2:11 (in Havilah), the story of the Golden Calf and many parts of the temple, including the Menorah and the golden altar. In the New Testament, it is included in the gifts of the magicians in the early chapters of Matthew. The book of Revelation 21:21 describes the city of New Jerusalem as having streets "made of pure gold, crystal clear." It is said that gold exploration in the southeast corner of the Black Sea dates back to the time of Midas, and this gold was important in establishing what is probably the oldest coinage in the world in Lydia around 610 BC.

Gold in Popular Culture
Great human achievements are often rewarded with gold, in the form of gold medals, gold trophies and other decorations. Winners of sporting events and other classified competitions generally receive a gold medal, such as the Olympic Games. Many prizes such as the Nobel Prize are also made of gold.
Other statues and awards are represented in gold or gold-plated (such as the Oscars, the Golden Globes, the Emmy Awards, the Palme d'Or, the British Academy Film Awards among many others).

Aristotle, in his ethics, used the symbolism of gold by referring to what is now known as the golden mean. In the same way, gold is associated with perfect or divine principles, as in the case of golden proportion and the golden rule.

Gold is still associated with the wisdom of aging and fruition. The 50th wedding anniversary is golden. The most valued or most successful years of a person are sometimes considered "golden years." The most prosperous years of a nation or a civilization is referred to as a golden age.

In some forms of Christianity and Judaism, gold has been associated with both holiness and evil. In the Book of Exodus, the Golden Calf is a symbol of idolatry, while in the Book of Genesis, Abraham was said to be rich in gold and silver, and Moses was instructed to cover the mercy seat of the Ark of the Covenant with pure gold. In Byzantine iconography, the halos of Christ, Mary and the Christian saints are often gold.

According to Christopher Columbus, those who possessed something of gold possessed something of great value on Earth and a substance that even helps souls to reach paradise.
wedding ring in gold
Wedding rings are made of gold as it is long lasting and unaffected by the passage of time and can aid in the symbolism of the ring of eternal vows before God and the perfection that marriage means. In the Orthodox Christian wedding ceremonies, the couple is adorned with a golden crown during the ceremony, a fusion of symbolic rites.
gold card by credicard
Credit cards or customer loyalty cards are described as "gold card" or "gold card", are some of other examples.

The Gold in Guinness World Records
Golden Buddha - Phra Maha Suwan Phuttha Patimakon
The largest gold piece in the world is the Golden Buddha of Wat Traimit in Thailand and weighs no less than 5 tonnes of pure gold.

Mythology and Legends
Midas is a character from Greek mythology and was King of a region whose name was Phrygia.

The main myth attributed to Midas, that of transforming into gold everything he touched, acquired a symbolic and metaphorical character in contemporary society, and symbolic analogies such as that of a "Midas complex" are easily understood in our culture, or it is attributed that an individual who possesses the "Midas touch" is one who has the ability to make something thrive, multiplying profits.

Medicinal Uses of Gold
Metallic gold compounds have long been used for medicinal purposes. Gold, usually as the metal, is perhaps the oldest medicine administered (apparently by shamanic practitioners) and known to the Dioscorides. In medieval times, gold was often seen as beneficial to health, in the belief that something so rare and beautiful could not be anything but healthy. Even some modern esotericists and forms of alternative medicine ascribe to metal gold a healing power.

In the nineteenth century, gold had the reputation of "nervine," a therapy for nervous disorders. Depression, epilepsy, migraine and glandular problems, such as amenorrhea and impotence, were treated and, mainly, alcoholism (Keeley, 1897).

The apparent paradox of the substance's actual toxicology suggests the possibility of serious gaps in the understanding of the action of gold in physiology. Only gold salts and radioisotopes are of pharmacological value, since elemental (metallic) gold is inert to all chemicals found in the body (ie gold ingested can not be attacked by gastric acid). Some gold salts have anti-inflammatory properties and currently two are still used as pharmaceuticals in the treatment of arthritis and other similar conditions in the US (sodium aurothiomalate and auranofin). These drugs have been explored as a means of helping to reduce the pain and swelling of rheumatoid arthritis, and also (historically) against tuberculosis and some parasites.

Gold alloys are used in restorative dentistry, especially in dental restorations such as crowns and permanent bridges. The slight malleability of gold alloys facilitates the creation of a superior molar coupling surface with other teeth and produces generally more satisfactory results than those produced by the creation of porcelain crowns. The use of gold crowns on more prominent teeth, such as the incisors, is favored in some cultures and discouraged in others.

Solutions of gold chloride (chloruric acid) are used to make colloidal gold by reducing with citrate or ascorbate ions. Gold chloride and gold oxide are used to produce crystals or red glasses, which, like colloidal gold suspensions, contain spherical gold nanoparticles of uniform size.

Gold colloidal preparations (suspensions of gold nanoparticles) in water are intensely red, and can be made with rigidly controlled particle sizes up to a few tens of nanometers by reducing gold chloride with citrate or ascorbate ions.

Colloidal gold is used in research applications in medicine, biology and materials science. The immunogold labeling technique explores the ability of gold particles to adsorb protein molecules on their surfaces. Colloidal gold particles coated with specific antibodies can be used as probes for the presence and position of antigens on the cell surfaces. In ultra-thin sections of tissues seen by electron microscopy, immunogold labels appear as extremely dense round spots at the antigen position.

Gold, or gold and palladium alloys, are applied as conductive coating to biological specimens and other nonconductive materials, such as plastics and glass, to be seen in a scanning electron microscope. The coating, which is usually applied by cathodic spray with argon plasma, has a triple role in this application. The very high electrical conductivity of gold drains the electric charge to Earth, and its very high density provides stopping energy for the electrons in the electron beam, helping to limit the depth at which the electron beam penetrates the test body. This improves the definition of the position and topography of the sample surface and increases the spatial resolution of the image. Gold also produces a high output of secondary electrons when irradiated by a beam of electrons, and these low energy electrons are the most commonly used signal source in the scanning electron microscope.

The gold isotope-198 (half-life of 2.7 days) is used in nuclear medicine, in some cancer treatments and for the treatment of other diseases.

The Gold in the Kitchen
Gold can be used in food and has the E 175 number. In 2016, the European Food Safety Authority published an opinion on the reassessment of gold as a food additive. Concerns included the possible presence of minimal amounts of gold nanoparticles in the feed additive and that the gold nanoparticles showed to be genotoxic in mammalian cells in vitro.
Gold leaf, flake or powder are widely used in some gourmet foods, especially sweets and beverages as a decorative ingredient. The gold flake was used by the nobility in medieval Europe as decoration in food and drink, in the form of leaves, flakes or powder, both to demonstrate the wealth of the host and the belief that something valuable and rare should be beneficial to health. A little all over the world we've heard of some international cuisine menu that may contain gold leaf.
Vark is a sheet made up of pure metal that is sometimes gold, and is used to garnish sweets in South Asian cuisine.

Alcoholic Beverages Containing Gold
Danziger Goldwasser (German: Gold gold of Danzig) or Goldwasser (in English: Goldwater) is a traditional German herbal liqueur produced in what is now Gdańsk, Poland, and Schwabach, Germany, and contains gold leaf flakes. Smirnoff Gold Collection was a limited edition of the famous Gold Leaf Vodka.
Gold Strike - alcoholic beverages containing gold
Gold Strike is a cinnamon liqueur drink with gold leaves. Goldschläger is a Swiss cinnamon schnapps, a liqueur with gold flakes. Some wines Portuguese and Spanish, non-current, are produced with small gold flakes.
There are also some expensive cocktails that contain flakes of gold leaf.

However, because metallic gold is inert to all body chemistry, it has no taste, does not provide nutrition, and leaves the body unchanged.

Gold in High Technology
James Webb Space Telescope Mirror Coated in Gold to Reflect Infrared Light
James Webb Space Telescope Mirror Coated in Gold to Reflect Infrared Light

Gold produces a deep deep red color when used as a dye in blackberry glass.
In photography, gold toners are used to change the color of black-and-white prints with silver bromide to brown or blue tones, or to increase their stability. Used in sepia prints, gold toners produce red tones. Kodak has published formulas for various types of gold toners, which use gold as chloride.

Gold is a good reflector of electromagnetic radiation, such as visible and infrared light as well as radio waves. It is used for protective coatings on many artificial satellites, infrared protection plates in thermal protection clothing and astronaut helmets, and on electronic warplanes such as the EA-6B Prowler.
Gold is used as a reflective layer on some high-end CDs.
Cars can use gold for heat shielding. McLaren uses gold leaf in the engine compartment of its F1 model.

Gold can be made so thin that it looks semitransparent. It is used in some aircraft cockpit windows to defrost or anti-ice by passing electricity through it. The heat produced by the gold resistance is sufficient to prevent the formation of ice.

Toxicity of Gold
Pure metallic (elemental) gold is non-toxic and non-irritating when ingested and is sometimes used as food decoration in the form of gold leaf. Metallic gold is also a component of the Goldschläger, Gold Strike and Goldwasser alcoholic beverages. Metallic gold is approved as a food additive in the EU (E175 in the Codex Alimentarius). Although the gold ion is toxic, the acceptance of metallic gold as a food additive is due to its relative chemical inertia and resistance to corrosion or transformation into soluble salts (gold compounds) by any known chemical process that is found in the body of the human being.

Soluble compounds (gold salts), such as gold chloride, are toxic to the liver and kidneys. Common gold cyanide salts, such as potassium cyanide and gold, used in gold electroplating are toxic because of their cyanide and gold content. There are rare cases of lethal gold poisoning from gold and potassium cyanide. The toxicity of gold can be improved with chelation therapy with an agent such as dimercaprol.
Symptoms_of_gold_toxicity
The gold metal was elected the Allergen of the Year in 2001 by the American Contact Dermatitis Society, contact allergies with gold primarily affect women. Despite this, gold is a relatively non-potent contact allergen compared to metals such as nickel.

Generally an allergy to an alliance is not an allergy to gold but an allergy to some other metal contained in the gold alloy of this alliance.

A sample of the Aspergillus niger fungus was found growing from the gold mining solution, and found to contain cyano-metal complexes; such as gold, silver, copper and zinc. The fungus also plays a role in the solubilisation of heavy metal sulphides.

Gold Reserves
The reserve gold bullion in physical bars give an important economic factor to the country.
Countries with the largest gold reserves in solid bars, see table on Wikipedia. https://en.wikipedia.org/wiki/Gold_reserve

September 7
HAPPY GOLD DAY

Gold International Day
Gold International Day

Dia del Oro
Dia del Oro

Jour de l'or
Jour de l'or

黃金國際日
黃金國際日
黃金國際日.com

Internationaler Goldtag
Internationaler Goldtag

اليوم العالمي للذهب
اليوم العالمي للذهب

국제 금의 날
국제 금의 날

Guld dag
Guld dag

Araw ng Ginto
Araw ng Ginto

ゴールドインターナショナルデー
ゴールドインターナショナルデー

Διεθνής Ημέρα του Χρυσού
Διεθνής Ημέρα του Χρυσού

Hari Emas Internasional
Hari Emas Internasional

Giorno Internazionale dell'oro
Giorno Internazionale dell'oro

Международный день золота
Международный день золота

Dia do Ouro
Dia Internacional do Ouro

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