螢石｜Fluorite

螢石是世界上最具代表性的彩色礦物之一。

從紫色、綠色、藍色到黃色，甚至同一顆晶體中同時出現多種色帶，螢石展現了自然界豐富而細緻的色彩變化。

在 DIYU Reading System 中，螢石代表著色彩，也是閱讀礦物形成環境與元素變化的重要窗口。

────────────────

Fluorite is one of the world’s most colorful minerals.

From purple and green to blue and yellow, and often displaying multiple color zones within a single crystal, fluorite reveals the extraordinary beauty of natural color.

Within DIYU Reading System, fluorite represents color and offers an important window into the geological environments that shape minerals.

螢石的化學成分為氟化鈣（CaF₂），屬於鹵化物礦物。

它主要形成於熱液礦脈，也常與石英、方解石、重晶石及多種金屬礦物共生。

不同的微量元素、天然輻射與晶體缺陷，共同影響螢石的顏色，使其成為自然界色彩最豐富的礦物之一。

────────────────

Fluorite is composed of calcium fluoride (CaF₂) and belongs to the halide mineral group.

It commonly forms in hydrothermal veins and frequently occurs alongside quartz, calcite, barite, and metallic minerals.

Trace elements, natural radiation, and crystal defects together produce the remarkable range of colors found in fluorite.

在 DIYU Reading System 中，螢石代表的是色彩。

不同的元素、形成環境與地質條件，使同一種礦物呈現出截然不同的色澤與透明度。

對 DIYU 而言，我們閱讀的不只是顏色本身，而是色彩如何記錄礦物形成的環境，以及晶體如何在時間中保留這些自然留下的痕跡。

閱讀螢石，也是閱讀自然如何透過光與元素，創造出礦物世界最豐富的色彩。

────────────────

Within DIYU Reading System, fluorite represents color.

Different trace elements, geological environments, and formation conditions give rise to remarkable variations in color and transparency.

For DIYU, we read more than color itself—we explore how color preserves the history of mineral formation and how crystals record the environments in which they grew.

Reading fluorite means understanding how light, chemistry, and time together create one of nature’s most beautiful minerals.

※ DIYU Reading System 將持續建立各產地的獨立閱讀頁面。