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Fake Diamond
Fake Diamond
Fake Diamond
Fake Diamond

Fake Diamond

Fake Diamond

A species of Diamond, Also known as Imitation Diamond, Rhinestone

Fake Diamond, also known as a Diamond Imitation, is a man-made or natural material designed to mimic the appearance of a genuine Diamond, without being composed of carbon atoms arranged in a crystalline structure. A common type of fake Diamond includes Cubic Zirconia, Moissanite, and Glass. Although a fake Diamond may visually resemble a real Diamond, it typically lacks the distinct physical properties, such as hardness, refractive index, and thermal conductivity, that make Diamonds unique and valuable.

General Info About Fake Diamond

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Snap a photo for instant rock/gemstone/mineral ID and properties analysis, gaining quick insights on characteristics, market value, collecting tips, care, real vs fake, and health risks, etc.
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Physical Properties of Fake Diamond

Luster
Adamantine, Vitreous
Diaphaneity
Transparent to translucent
Colors
Colorless, white, yellow, brown, pink, black, blue, red
Streak
none
qrcode
Img download isoImg download android

Chemical Properties of Fake Diamond

Formula
C
Elements listed
C

Optical Properties of Fake Diamond

Refractive Index
2.417-2.419
Pleochroism
None
Dispersion
0.044
Optical Character
Isotropic

Characteristics of Fake Diamond

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In-depth exploration of rock types, features, and formation aspects
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Cultural Significance of Fake Diamond

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Unveiling the mysteries of rock culture - exploring uses, history, and healing properties, etc
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Healing Properties of Fake Diamond

Fake Diamond is believed to be one of the most powerful of stones. Said to offer access to Divine energy, the stone is often used to attract love, respect, and emotional growth while cleansing the aura from negativity. It is often worn on the Third Eye chakra to improve mental clarity and provide healing energy to the physical body.

Common Questions People Also Ask

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Arkose
Arkose ( /ˈɑːrkoʊz/) is a detrital sedimentary rock, specifically a type of sandstone containing at least 25% feldspar. Arkosic sand is sand that is similarly rich in feldspar, and thus the potential precursor of arkose. Quartz is commonly the dominant mineral component, and some mica is often present. Apart from the mineral content, rock fragments may also be a significant component. Arkose usually contains small amounts of calcite cement, which causes it to effervesce (fizz) slightly in dilute hydrochloric acid; sometimes the cement also contains iron oxide. Arkose is typically grey to reddish in colour. The sand grains making up an arkose may range from fine to very coarse, but tend toward the coarser end of the scale. Fossils are rare in arkose, due to the depositional processes that form it, although bedding is frequently visible. Arkose is generally formed from the weathering of feldspar-rich igneous or metamorphic, most commonly granitic, rocks, which are primarily composed of quartz and feldspar (called 'grus' as a sand). These sediments must be deposited rapidly and/or in a cold or arid environment such that the feldspar does not undergo significant chemical weathering and decomposition; therefore arkose is designated a texturally immature sedimentary rock. Arkose is often associated with conglomerate deposits sourced from granitic terrain and is often found above unconformities in the immediate vicinity of granite terrains. The central Australian inselberg Uluru (Ayers Rock) is composed of late Neoproterozoic/Cambrian arkose, deposited in the Amadeus Basin.
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Regarded for its beauty and delicate look, blue Lace Agate tumbled is a rare agate with beautiful lacy bands of gray, white, light blue, or sometimes brown. It is mined in Namibia, as well as in USA, India, China, and Brazil. It can be seen in beads and cabochons, and it's often used for jewelry making.
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