Diamond Stocks List

Recent Signals

Date Stock Signal Type
2019-10-11 DFR Narrow Range Bar Range Contraction
2019-10-11 DMI MACD Bullish Signal Line Cross Bullish
2019-10-11 DMI Pocket Pivot Bullish Swing Setup
2019-10-11 DMI Crossed Above 20 DMA Bullish
2019-10-11 NAR MACD Bullish Signal Line Cross Bullish
2019-10-11 NAR Non-ADX 1,2,3,4 Bearish Bearish Swing Setup
2019-10-11 NAR Pocket Pivot Bullish Swing Setup
2019-10-11 NAR Crossed Above 20 DMA Bullish
2019-10-11 NAR Narrow Range Bar Range Contraction
2019-10-11 NAR Stochastic Buy Signal Bullish
2019-10-11 NAR Bollinger Band Squeeze Range Contraction
2019-10-11 TUF Narrow Range Bar Range Contraction
2019-10-11 TUF Stochastic Sell Signal Bearish
2019-10-11 TUF MACD Bearish Signal Line Cross Bearish
2019-10-11 TUF New Downtrend Bearish

Diamond is a solid form of the element carbon with its atoms arranged in a crystal structure called diamond cubic. At room temperature and pressure, another solid form of carbon known as graphite is the chemically stable form, but diamond almost never converts to it. Diamond has the highest hardness and thermal conductivity of any natural material, properties that are utilized in major industrial applications such as cutting and polishing tools. They are also the reason that diamond anvil cells can subject materials to pressures found deep in the Earth.
Because the arrangement of atoms in diamond is extremely rigid, few types of impurity can contaminate it (two exceptions being boron and nitrogen). Small numbers of defects or impurities (about one per million of lattice atoms) color diamond blue (boron), yellow (nitrogen), brown (defects), green (radiation exposure), purple, pink, orange or red. Diamond also has relatively high optical dispersion (ability to disperse light of different colors).
Most natural diamonds have ages between 1 billion and 3.5 billion years. Most were formed at depths between 150 and 250 kilometers (93 and 155 mi) in the Earth's mantle, although a few have come from as deep as 800 kilometers (500 mi). Under high pressure and temperature, carbon-containing fluids dissolved minerals and replaced them with diamonds. Much more recently (tens to hundreds of million years ago), they were carried to the surface in volcanic eruptions and deposited in igneous rocks known as kimberlites and lamproites.
Synthetic diamonds can be grown from high-purity carbon under high pressures and temperatures or from hydrocarbon gas by chemical vapor deposition (CVD). Imitation diamonds can also be made out of materials such as cubic zirconia and silicon carbide. Natural, synthetic and imitation diamonds are most commonly distinguished using optical techniques or thermal conductivity measurements.

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