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LATEST
COLLECTIONS OF 14K GOLD and DIAMOND DESIGNER JEWELRY!

ENTER THE CODE "CRG1005"
AT THE CHECKOUT FOR THE 5% DISCOUNT!





 
 
 
 
 
 
 
 
 
 
 

















 
















 




ENTER
OUR CRAIGSLIST SPECIAL OFFER CODE "CRG1005"
AT
THE CHECK OUT FOR THE 5% DISCOUNT!





















 
For
the past, the present, and
the future. View our Three-Stone
Diamond Ring collection.















 

Diamond accents add a dash
of sparkle to your engagement
ring.







 












 

View
wedding bands in 14K gold,
platinum, tungsten, titanium
and silver from $20.
















 

Classic
wedding bands for men. A great
choice.Starting at $30.

















 

Add
some sparkle with our diamond
wedding bands. Browse through
a stunning collection of Eternity
and Channel Set Bands.















 


 


 



Our
classic 14k white gold four-prong
diamond tennis bracelets are manufactured
with G-H color, SI-I clarity stones
and perfect examples of diamond
jewelry.
 




1
ct. tw $599.95


 
 




2
ct. tw $979.95




4
ct. tw $1999.95





6
ct. tw $2999.95




8
ct. tw $6999.95





 
















14k white gold four-prong settings
are set with a perfectly-matched
pair of diamonds of at least I-J
color, because a white metal accentuates
near-colorlessness in diamonds.
Also, these diamonds are graded
SI-I clarity.






1/4
ct. tw.
$219.95
view




1/3
ct. tw.
$299.95
view




1/2
ct. tw.
$389.95
view




3/4
ct. tw.
$689.95
view




1
ct. tw.
$979.95
view




1 1/2
ct. tw.
$1669.95
view


 





























 
 













 





 
 
 
 

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yellow


-Cr magma in volcanic pipes is usually one of two characteristic types, which
cool into igneous rock known as either kimberlite or lamproite.[6] The magma
itself does not contain diamond; instead, it acts as an elevator t pyroxene,
and amphibole minerals[6] which are often altered to serpentine by heat and
fluids during and after eruption. Certain indicator minerals typically occur
within diamondiferous kimberlites and are used hat carries deep-formed rocks
(xenoliths), minerals (xenocrysts), and fluids upward. These rocks are characteristically
rich in magnesium-bearing olivispinels, da mineralogic tracers by prospectors,
who follow the indicator trail back to the volcanic pipe which may contain diamonds.
These minerals are rich in chromium (Cr) or titanium (Ti), elements which impart
bright colors toccasionally green ugrandite-series garnets), eclrk chromite,
bright green Cr-diopside, glassy green olivine, black picroilmenite, and magnetite.[6]
Kimberlite deposits are known as blue ground for the deeper serpentinized part
of the deposits, or as yellow ground for the near surface smectite clay and
carbonate weathered and oxidized portion.







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