wholesale jewelry

On Each grand awards ceremony, we not only focus on the music, art, film, but also the dressing and jewelry wearing by the superstars.

The 81st Academy Award Ceremony in Los Angeles was the usual parade of beautiful gowns, dresses and accessories worn on the red carpet. And let's be honest, there are many of us who watch the Oscars just to see the jewellery and fashions on display.

So what do this year's Oscars tell us about what's hot in jewellery? Here are some key jewellery trends for 2009 that emerge from the Oscars red carpet.

1. Using striking color to liven up outfits is one of the great jewellery trends of the season, as it's an affordable way of reviving an old outfit. For example, famous actress Angelina Jolie chose striking green dangling earrings to go with her elegant black gown. In fact, one commentator described her earrings as the most interesting part of her outfit.

2. Big, bold, “Statement jewellery” is still one of the most important jewellery trends for this season. Just check out the number of celebrities wearing Fred Leighton statement pieces. Big flower bracelets, chunky beads and big base metal are all great new statement ideas for 2009. This is a new trend, and is especially suitable in times of make public individual character.

3. Drop or dangling earrings remain a big hit. 'Slumdog Millionaire' actress Freida Pinto wore pretty drop earrings, as did Angeline Jolie (see above).

4. Charm bracelets were worn by quite a few on the red carpet. The stack of charms, watches and chains shows a revival of that famous eighties Madonna look, which is set to be big again in 2009.

Celebrity looks can inspire whole new jewellery trends, and breathe new life into old ones. We can get some inspiration from celebrities, and design new products on this basis, maybe there will be a new fashion arised.

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Olivine has also been called "peridot" which ranges in color from a yellowish green to pure green to a nearly olive green color.

The finest peridot, the Egyptian material, has a minimum of yellow in it and is a bright clear green. Unfortunately the Egyptian material is no longer mined and not readily available on the market.

You can find fine Burmese peridot, which is fairly rare, in sizes over ten carats, with a fairly dark clear green color with only a hint of yellow.

Norwegian peridot is yellowish green but it is much softer in color than the other sources.

Arizona material is readily available in sizes under five carats and is characteristically a bright yellowish green. It is mined on a Reservation by the San Carlos Indians.

Peridot is a fragile stone; it is brittle and will abrade easily around facet junctions. It should be set into protective mounting. Never put peridot in an ultrasonic cleaner: it may not break but the internal fracture may be massive.

Peridot over ten carats with a bright medium green color with a minimum of yellow and good transparency with no sleepiness or visible inclusions will command the highest price per carat. Fine stones will fall into a moderate price per carat category. Large peridot even of lesser quality will usually be in the lower end of the moderate per carat price range due to its rarity. Peridot under two carats will usually fall into the low price per carat category even for fine qualities. Fine quality stones in two to five carat sizes may be in the moderate price range but olive colored material or heavily included stones will fall into the low price per carat group.

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Garnets are a form of neosilicates and are created from the elements of calcium, manganese and iron. Besides these elements, other elements do occur including chromium and titanium. Garnets can be found in crystal form or in a grainy form.

Garnets are usually found as dodecahedral crystals, but are known also to form in trapezohedron habits. The crystalline structure is that of an isometric system, meaning they have three axes that are all equal in length and also considered perpendicular to one another.

Garnets are usually hard minerals with a hardness score of 7.5 to 8 on Moh’s hardness scale; however it should be noted, they can still crack easily and will break into sharp fragments.

Garnets are found in a wide variety of locations including Kenya, Sri Lanka, Thailand, Brazil, India, Madagascar, Canada and USA. In USA garnet has been obtained in Arizona, Colorado, Georgia, Idaho, New Hampshire, New Mexico, North Carolina, Pennsylvania, Utah, Florida, California and Virginia.

The majority of today's Garnet supplies come from Africa. Notable quantities of garnets have been also found in Czech Republic and Spain. The oranges and browns of Spessartite and Hessonite hail from Namibia and Sri Lanka.

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Agate is formed from mineral deposits and is considered by most to be a precious stone.

Agate usually occurs in cavities that have formed from volcanoes (especially ancient lavas). Agates are known to have bands that come in many colors and resemble the rings of a tree. Scientists say that agate is created when gas bubbles inside of cooling lava include saline water. These gas bubbles with saline water turn into a gel. Since there is salt in the water, it attacks the surrounding iron in the lava and creates bands. These bands are extremely intricate and beautiful.

It should be noted that no two stones are the same, making each Agate stone unique and more precious. Agate comes in many different colors and usually in its raw state is dull and rough. In order for Agate to show its true beauty it must be polished.

Agates are widely distributed, although the main deposits are in India, Brazil, Madagascar, China, Russia and Australia. According to Greek legend, Agate was found in the river Achates, which is now called the Drillo River, located in Sicily. However, there is evidence that Stone Age men used Agate more than 15,000 years ago. Today, you can easily find sources in the Western United States, Mexico, Germany, Italy, Brazil, China, India, Africa, etc.

The color of agates can vary significantly, depending on the distribution of minerals within each band. Minerals that contribute to the stone color include: iron oxides (red, brown, black, green), manganese (pink, violet, black), chromium (green, yellow, red), titanium (blue), cobalt (red), nickel (green), and copper (red, blue, and green). The shade of color is further modified when these minerals work in combination. The color can occur through an agate band, or it can form as small, dot-like inclusions. Color can also be influenced by temperature, radiation, pressure, and weathering.

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