Sometimees the return to basics becomes a great idea, likewise returning to basic black and white in jewelry can be called a real "Return to Basics".
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In this "return to basics" design, two old gemstones are also used. White Agate, sometimes called Greek Agate, flat nuggets are combines with two sizes of Black Agate (Onyx) round beads and pewter accents with silver plated hammered chain and a lobster clasp to complete the necklace. Matching Black Agate (Onyx) round beads and pewter accents on French Hook earrings complete the set.
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Black Agate (Onyx) which is truely a died black Agate, is more common and perhaps the most famous variety, but not as common as natural Onyx. Onyx is a crypyocrystalline form of Quartz. The colors of its bands range from white to almost every color (save some shades, such as purple or blue).
A picture of a true Black Onyx specimum is seen at the left. True specimens of Onyx contain bands of colors of white, tan, and brown. As stated, the pure black form which most people know as Onyx, is not a naturally occuring variety. Black Agate or poorly colored Onyx is heated and dyed black to come up with the pure black form so well liked within the jewelry industry.
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Agate is a microcrystalline variety of quartz, chiefly Chalcedony, characterised by its fineness of grain and brightness of color. Although agates may be found in various kinds of rock, they are classically associated with volcanic rocks but can be common in certain metamorphic rocks.
White Agate or probably better known as Greek agate, is a name given to pale white to tan colored Agate originally found in Sicily back to 400 B.C. The Greeks used it for making jewelry and beads. Today almost any agate of this white color is called Greek agate. Yet the stone had been around centuries before that and was known to both the Sumerians and the Egyptians, who used the gem for decoration and religious ceremony. True White Greek Agate comes only from Sicily, once a Greek Colony.
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Pewter is a metaln alloy, traditionally between 85 and 99 percent tin
n, with the remainder consisting of 1-4 percent copper, acting as a hardener, with the addition of lead for the lower grades of pewter and a bluish tint. Traditionally, there were three grades of pewter: fine, for eatingware, with 96-99 percent tin, and 1-4 percent copper; trifle, also for eating and drinking utensils but duller in appearance, with 92 percent tin, 1-6 percent copper, and up to 4 percent lead; and lay or ley metal, not for eating or drinking utensils, which could contain up to 15 percent lead. Modern pewter mixes the tin with copper, antimony and/or bismuth as opposed to lead. Physically, pewter is a bright, shiny metal that is very similar in appearance to silver. Like silver, pewter will also oxidize to a dull gray over time if left untreated. Pewter is a very malleable alloy, being soft enough to work with hand tools, and it also takes good impressions from punches or presses. Because of this inherent softness and malleability, however, pewter cannot be used to make tools itself. Some types of pewter pieces, such as candlesticks, would be turned on a metal lathe. Pieces produced through this technique are sometimes referred to as "holloware." Pewter has a low melting point of around 225-240°C (437-464°F) depending on the exact mixture of metals. Duplication by casting will give excellent results especially in jewelry making. Pewter is many times the base metal for Silver or Gold plating.
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With this particular set one can go from Day to Night and not have to change.
This 18 inch necklace is made of blue Ceramic beads, fossil Coral barrel beads and polished Pewter accents.
The necklace is finished with a silver plated Toggle Clasp.
Matching circular hook dangle earrings complete the set.
Fossil Coral is a natural stone that is formed when ancient coral is gradually replaced with agate. The proper name for this material is agatized coral or agatized fossil coral. The fossilized coral typically appears as small flower-like patterns in the stone. Agatized fossil coral can exhibit a wide range of natural colors, ranging from white and pink to brown, gray, black, yellow and red. Corals may vary widely within a single stone depending on weathering and oxidation and the original mineral content. In some cases corals were buried in sediment as the land surface was affected by crustal plate movements or the oceans rose and fell. Temperature and pressure from compaction during burial resulted in those deposits becoming rock and part of the present day geological record.
