佩尼亞布蘭卡｜Peñas Blancas

佩尼亞布蘭卡位於哥倫比亞博亞卡省西部的 San Pablo de Borbur，是西博亞卡祖母綠帶北部的重要礦區。

雖然這片區域位於著名的哥倫比亞祖母綠產帶之中，佩尼亞布蘭卡在礦物收藏市場裡同樣以石英受到注意。

透明石英、晶簇、不同的生長紋理，以及晶體與熱液礦化環境之間的關係，共同構成這片產區具有辨識度的自然樣貌。

在 DIYU Reading System 中，佩尼亞布蘭卡也是我們閱讀哥倫比亞石英的重要入口之一。

Peñas Blancas, located in San Pablo de Borbur in western Boyacá, Colombia, lies toward the northern part of the Western Emerald-Bearing Belt.

Although the region belongs to Colombia’s celebrated emerald landscape, Peñas Blancas has also become notable among mineral collectors for its quartz specimens.

Clear quartz, crystal clusters, varied growth textures, and the relationship between crystals and hydrothermal mineralization together shape the distinctive mineral character of this locality.

Within the DIYU Reading System, Peñas Blancas is also one of our important entry points into Colombian quartz.

佩尼亞布蘭卡並不是單一礦坑，而是一片山區礦化地帶，其中分布著多個小型礦坑與探坑。

這裡位於哥倫比亞東科迪勒拉西部祖母綠帶，部分礦化發育於 Rosablanca Formation 的沉積岩中。當地研究記錄了黑色至深灰色石灰岩、含碳質泥岩，以及受到構造作用影響的熱液脈與礦化空間。

熱液沿著岩石中的裂隙與構造通道活動，使石英、方解石、白雲石、螢石及其他礦物得以在不同環境中形成。

Peñas Blancas is not a single mine, but a mineralized mountain area containing numerous small mines and prospects.

It lies within the Western Emerald-Bearing Belt of Colombia’s Eastern Cordillera. Parts of the mineralization occur within sedimentary rocks of the Rosablanca Formation, where dark limestones, carbonaceous mudstones, structural deformation, and hydrothermal veins form part of the geological setting.

Hydrothermal fluids moved through fractures and structural pathways, allowing quartz, calcite, dolomite, fluorite, and other minerals to form in different parts of the locality.

佩尼亞布蘭卡具有豐富的石英標本紀錄。常見的收藏特徵包括完整晶形、明顯柱面生長紋、透明至高透明晶體、晶簇與連生結構，以及蝕刻與不同階段留下的生長痕跡。

既有礦物資料記錄當地石英十分常見，可見自形柱狀、晶簇狀及平行生長等型態。不同礦坑與不同形成階段仍可能呈現明顯差異，因此這些特色適合作為收藏觀察，而不是單靠外觀判定產地的依據。

Quartz is well represented at Peñas Blancas. Collector specimens may show well-formed crystal outlines, distinct growth striations, clear to highly transparent crystals, clusters and intergrown crystals, as well as etching and varied growth textures.

Published locality records describe quartz as common in the area, including euhedral prismatic, drusy, and parallel-growth habits. Individual mines and stages of mineralization can nevertheless produce considerable variation, so these characteristics should be understood as collecting observations rather than diagnostic rules for provenance.

佩尼亞布蘭卡常見的收藏類型包括：

• 白水晶｜Clear Quartz
• 晶簇｜Crystal Clusters
• 平行生長晶體｜Parallel-Growth Quartz
• 礦物共生標本｜Mineral Associations
• 螢石｜Fluorite

Common collector material from Peñas Blancas includes:

• Clear Quartz
• Crystal Clusters
• Parallel-Growth Quartz
• Mineral Associations
• Fluorite

佩尼亞布蘭卡給人的印象，首先來自石英本身。

透明晶體、清晰的柱面、生長紋與彼此連生的晶簇，使許多標本呈現出明確而具有秩序的結晶感。

但這種清晰並不代表單純。蝕刻、附著、共生與不同階段留下的表面變化，又讓晶體保留了熱液活動與生長過程中的痕跡。

因此，佩尼亞布蘭卡的風土既可以被閱讀為晶體的完整，也可以被閱讀為生長留下的層次。

The character of Peñas Blancas begins with quartz itself.

Transparent crystals, defined prism faces, growth striations, and intergrown clusters give many specimens a strong sense of crystalline structure and order.

Yet this clarity does not necessarily mean simplicity. Etching, surface deposits, mineral associations, and traces left by different stages of growth preserve evidence of a more complex hydrothermal history.

The terroir of Peñas Blancas can therefore be read through both the definition of its crystals and the layers left by their growth.

在 DIYU Reading System 中，佩尼亞布蘭卡是博亞卡石英逐漸取得更精確產地資訊之後，變得越來越重要的一個名字。

我們所接觸的標本中，包括部分市場稱為黃金利姆的石英，以及具有明顯生長紋、蝕刻、晶簇與特殊晶體結構的標本，都可以在這片產區找到對應的收藏脈絡。

但對 DIYU 而言，佩尼亞布蘭卡真正值得閱讀的地方，不在於建立一套「只要長這樣就是 PB」的外觀公式，而是在產地從「哥倫比亞」、「博亞卡」逐漸縮小到 Peñas Blancas 之後，把手中的晶體重新放回一個更具體的地質環境裡。

晶體沒有因此改變。改變的是我們知道它來自哪裡之後，看見它的方式。

Within the DIYU Reading System, Peñas Blancas has become increasingly important as the provenance of our Boyacá quartz specimens has become more precise.

Among the specimens we encounter are quartz crystals sold under collector terms such as Golden Lemurian, together with pieces showing pronounced growth striations, etching, clustering, and distinctive crystal structures.

For DIYU, however, the value of Peñas Blancas is not in creating a visual formula that claims a specimen must come from PB simply because it looks a certain way. Instead, as provenance narrows from “Colombia,” to “Boyacá,” and finally to Peñas Blancas, the crystal can be placed back into a more specific geological landscape.

The crystal itself has not changed. What changes is the way we see it once we understand where it came from.