Hexagonal
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6/m 2/m 2/m (D6h)
4개의 축: 120도로 교차하는 동일한 수평 3축과 수직 1축 (a1 = a2 = a3 ≠ c)
육방정계는 4개의 결정축을 가집니다. 120도로 교차하는 동일한 길이의 수평 3축과 길이가 다른 수직 1축으로 구성됩니다. 결정은 흔히 육각형 기둥과 피라미드 형태를 나타냅니다. 대표 광물로는 녹주석(에메랄드, 아쿠아마린), 인회석, 흑연 등이 있습니다.
The hexagonal crystal system features four axes — three equal axes in a plane at 120° to each other, plus one unique axis perpendicular to them. This six-fold symmetry produces the characteristic hexagonal prisms and bipyramids seen in many well-known minerals. The hexagonal system is home to some of the most valuable gemstones on Earth, including beryl (emerald, aquamarine) and corundum (ruby, sapphire).
Symmetry
Hexagonal crystals have a principal six-fold rotation axis (a₁ = a₂ = a₃ ≠ c, with a-axes at 120°). Looking down the c-axis, the crystal appears to have six-fold symmetry. The system contains 7 crystal classes, from the fully symmetric dihexagonal dipyramidal class to the less symmetric hexagonal pyramidal class. The Miller-Bravais index system uses four indices (hkil) rather than three, where i = -(h+k), reflecting the three equivalent a-axes. This system is sometimes confused with the trigonal system, which has three-fold rather than six-fold symmetry and is treated as a subdivision by some crystallographers.
주요 광물
Beryl is the signature hexagonal mineral, forming the prismatic hexagonal crystals that yield emerald (green, chromium-colored), aquamarine (blue), morganite (pink), and heliodor (yellow). The largest single crystal ever found — an 18-meter beryl from Madagascar — crystallized in this system. Apatite, the mineral that forms our bones and teeth, is hexagonal and occurs in a remarkable range of colors. Molybdenite (MoS₂), the chief ore of molybdenum, forms distinctive hexagonal plates with a metallic luster. Ice itself crystallizes in the hexagonal system, explaining the six-fold symmetry of snowflakes.
광물 (2)
Beryl (Emerald)
Be3Al2(SiO3)6
09 Silicates
Apatite
Ca5(PO4)3(F,Cl,OH)
08 Phosphates, Arsenates, and Vanadates