中國｜China

中國位於亞洲東部，面向西太平洋。廣大的陸地範圍，從世界最高的高原與山系，延伸到內陸盆地、北方草原、乾燥荒漠、東部平原，以及濕潤的東南丘陵與海岸。

這片土地最清楚的地形特徵，是高度由西向東逐步下降。

西部的青藏高原構成最高的一層，平均海拔超過四千公尺，並與喜馬拉雅、崑崙等大型山系相連。向東移動，地勢進入高原與盆地交錯的中間區域；再往東，土地逐漸下降為平原、丘陵、河口與沿海地帶。這種由高至低的階梯結構，使山脈、河流、氣候與人類活動，在廣大範圍內形成不同的方向與密度。

但中國並不是由幾個整齊排列的地形區塊組成。

高山與盆地彼此相鄰，乾燥荒漠之外仍有雪山與河谷；東南沿海雖然濕潤，也分布著大量丘陵與山地。高度、季風、水分與岩層的改變，使不同區域形成截然不同的自然條件。西北部較為乾燥，岩體與地表容易直接暴露；東部與南部水分較多，植物、土壤與河流則更深地參與地景的形成。

地形的差異，也對應著複雜的地質背景。

古老陸塊、活動山系、沉積盆地、岩漿作用與變質作用，在不同時期共同塑造這片土地。中國的礦物並非來自單一成礦環境，而是分布在多個地質單元與礦帶之中。青藏高原、東部中生代岩漿活動區與北方地質帶，便保存著不同類型的礦床與礦物組合。

因此，「中國礦物」並不存在一種可以代表全部的樣貌。

透明而完整的晶體、帶有包裹體與共生的標本、經過風化與暴露的礦物，以及形成於不同高度與岩層中的晶體，都可能被收進同一個國家名稱之下。真正需要閱讀的，是這個廣大名稱之內，究竟包含了哪些彼此不同的地方。

China lies in eastern Asia, facing the western Pacific. Its immense land area extends from the world’s highest plateau and mountain systems to inland basins, northern grasslands, arid deserts, eastern plains, and the humid hills and coastlines of the southeast.

The clearest structure of this landscape is its general descent from west to east.

The Tibetan Plateau forms the highest level, averaging more than four thousand meters above sea level and connecting with major mountain systems such as the Himalayas and the Kunlun Mountains. Moving eastward, the land enters an intermediate region of plateaus and basins before descending again toward plains, hills, river deltas, and coastal terrain. This stepped relief gives mountains, rivers, climate, and human settlement different directions and densities across the country.

Yet China is not composed of neatly separated geographical zones.

Mountains stand beside basins, while snow-covered ranges and river valleys appear beyond arid deserts. The humid southeast is not simply flat or tropical, but is also shaped by extensive hills and mountain terrain. Changes in elevation, monsoon influence, water, and underlying rock create sharply contrasting environments. In the drier northwest, rock bodies and land surfaces are often more directly exposed; in the east and south, vegetation, soil, and rivers participate more deeply in shaping the visible landscape.

This geographical variety is matched by an equally complex geological history.

Ancient continental blocks, active mountain systems, sedimentary basins, magmatism, and metamorphism have shaped different regions at different times. China’s minerals do not arise from one geological environment, but occur across numerous geological units and metallogenic belts. The Tibetan Plateau, the Mesozoic igneous regions of eastern China, and the geological belts of the north preserve different mineral deposits and associations.

For this reason, there is no single appearance that can represent “minerals from China.”

Transparent and well-formed crystals, specimens containing inclusions and mineral associations, weathered minerals exposed at the surface, and crystals formed under very different elevations and rock conditions may all be placed beneath the same country name. What deserves to be read is the range of distinct places contained within that broad label.

中國位於多個重要地質構造帶交會的位置，擁有極為完整且多樣的地質環境。

自前寒武紀以來，歷經板塊碰撞、海洋閉合、火山活動、花崗岩侵入與變質作用，不同年代所形成的岩石共同構成今日複雜的地質景觀。

這些漫長的自然作用，不僅塑造了山脈與地形，也提供了晶體形成所需的溫度、壓力、流體與化學環境，使中國成為世界重要的礦物產區之一。

China lies across several major geological provinces, making it one of the most geologically diverse regions on Earth.

Since the Precambrian, tectonic collisions, ocean closures, volcanism, granitic intrusions, and metamorphic events have shaped a remarkably complex geological framework.

These long geological processes created the temperatures, pressures, fluids, and chemical environments necessary for crystal formation, making China one of the world’s most significant mineral-producing regions.

前面我們展示了中國的風土與地質條件，接下來，讓我們以不同的角度閱讀這片土地。

對底域而言，中國首先呈現的是一種「尺度」。

國家的名稱將遼闊的土地收進同一個範圍。然而，當視線從沿海往內陸移動，這個整體便逐漸展開。氣候、地貌與生活方式不斷改變，土地呈現出截然不同的距離、表面與方向。

中國的廣大，不只存在於地圖之上。

長久以來，人也透過繪畫、園林與石頭，嘗試讓那些無法被完整帶走的山河，進入可以觀看、行走與相處的尺度。

山河進入畫卷之後，便不再需要一次出現在眼前。

長卷被放在案上，隨著雙手緩慢展開。觀看者一次只能看見其中一段，卻也因此獲得了穿越畫面的時間。山峰、河流、樹木與路徑依序出現，視線沿著畫卷向前，如同身體正在一片無法真正走入的地景中移動。

原本屬於空間的距離，被轉換成觀看所經過的時間。

園林則以另一種方式重新安排自然。

山石、水體、植物、建築與路徑被放入有限的範圍。人穿過門洞、轉過牆面、走近水邊，景物才一層一層顯現。同一座園林不會在入口處完全展開，它需要身體進入其中，讓方向、光線與季節逐漸改變眼前的世界。

而當天然石頭進入書齋，尺度再次縮小。

供石的孔洞、皺褶、表面、方向與重心，使一塊可以放置於案頭的石頭，保留了足以讓視線長久停留的深度。觀看者可以沿著它的起伏移動，在有限的物質之中，感受到更大的空間。

畫卷、園林與供石並沒有等比例複製自然。

它們改變了媒介，也改變了人與山河之間的距離。原本無法完整進入生活的土地，因此轉換成視線、身體與記憶可以抵達的形式。

一件晶體，也讓相似的尺度轉換再次發生。

它可以被托在掌心，卻仍保留著來自土地的方向、結構與生長痕跡。晶尖的指向、裂隙的延伸、母岩的承載與礦物之間的共生，讓視線在一件微小的自然之物中不斷移動。

晶體仍然是晶體，地景也仍然是地景。

兩者相遇的地方，不在於外形是否相似，而在於觀看如何重新安排尺度。當物質留下的線索與人的經驗相遇，一處無法被完整帶走的土地，便可能以另一種比例進入眼前。

人也可能因此對一件晶體產生感情。

那份感情不需要晶體替整片土地發言。它可能只是對漫長形成時間的敬意，對遙遠來處的想像，或是一件自然之物跨越土地，最終在日常生活裡獲得位置時，逐漸形成的珍惜。

收藏在此並不是占有一片山河。

更像是保存一次相遇，讓原本遙遠的土地，在人的空間與記憶中留下可以反覆靠近的入口。

從中國進入具體地區與產地，國家的名稱逐漸退到背景；從產地進入一件晶體，廣大的風土又收束成可以觀察的結構、表面與生長關係。

尺度每收束一次，既有的想像便退後一步，物質則向前一步。

而從這件晶體出發，視線仍然可以再次向外展開。

回到地層如何形成，回到山河如何被觀看，也回到人如何透過繪畫、園林、石頭與收藏，理解比自身更加廣大的世界。

中國在底域之中，因此呈現為一種不斷改變距離的觀看。

山河可以進入畫卷，世界可以進入園林，遠方也可以經由一件晶體，進入人的掌心與生活。

每一次尺度的轉換，都重新排列了土地、物質與人之間的關係。

願你在閱讀中，找到一種能從掌心重新望向山河，也能在廣大世界裡珍惜一件微小之物的目光。

—

The preceding sections introduced the terroir and geological conditions of China. Now, let us read this land from another perspective.

For DIYU, China first presents itself as a question of scale.

The name of a country gathers an immense territory into a single frame. Yet as the gaze moves from the coast toward the interior, that apparent whole gradually unfolds. Climate, terrain, and ways of life continue to change, and the land reveals profoundly different distances, surfaces, and directions.

China’s vastness exists not only on the map.

For generations, people have also turned to painting, gardens, and stone, seeking ways for mountains and rivers that cannot be carried away in their entirety to enter a scale that can be seen, traversed, and lived with.

When mountains and rivers enter a painted scroll, they no longer need to appear all at once.

A handscroll rests upon a table and is slowly opened by hand. The viewer sees only one section at a time, yet this limitation gives the image duration. Peaks, rivers, trees, and paths appear in sequence. The gaze travels through the scroll as though the body were moving across a landscape it could not otherwise enter.

Distance, originally belonging to space, is transformed into time experienced through seeing.

The garden rearranges nature in another way.

Rocks, water, plants, architecture, and paths are brought together within a bounded space. Scenery appears layer by layer as a person passes through a doorway, turns around a wall, or approaches the water. A garden never reveals itself completely at its entrance. The body must enter, allowing direction, light, and season to gradually change the world before the eye.

When a natural stone enters the scholar’s studio, the scale narrows once again.

The cavities, folds, surfaces, orientation, and balance of a scholar’s rock give an object placed upon a desk enough depth to sustain prolonged observation. The gaze can travel along its contours, sensing a larger space within a limited body of matter.

The handscroll, the garden, and the scholar’s rock do not reproduce nature at the same scale.

They change the medium and the distance between people and the landscape. Land that cannot fully enter daily life is transformed into a form accessible to sight, the body, and memory.

A crystal allows a similar shift of scale to occur.

It can be held in the palm while retaining directions, structures, and traces of growth carried from the land. The orientation of its terminations, the extension of its fractures, the support of its matrix, and its relationships with other minerals allow the eye to keep moving through a small natural object.

The crystal remains a crystal, and the landscape remains a landscape.

Their meeting does not depend on a resemblance of form. It occurs through the way seeing rearranges scale. When the traces preserved in matter encounter human experience, a place that cannot be carried away in its entirety may enter the present at another proportion.

A person may therefore develop an emotional connection with a crystal.

The crystal does not need to speak for the whole land. The feeling may arise from respect for the time required for its formation, imagination directed toward its distant origin, or the care that gradually develops when a natural object crosses the land and finds a place within everyday life.

To collect, in this sense, is not to possess an entire landscape.

It is closer to preserving an encounter: allowing a distant place to leave an entrance within human space and memory, one that can be approached again and again.

As we move from China into a particular region or locality, the name of the country gradually recedes. As we move from the locality into an individual crystal, the breadth of terroir narrows into observable structures, surfaces, and relationships of growth.

With each narrowing of scale, prior imagination recedes by one step and matter moves one step forward.

From the crystal, the gaze can open outward once again.

It may return to the formation of geological layers, to the ways mountains and rivers have been seen, and to the ways people use painting, gardens, stones, and collecting to understand a world larger than themselves.

Within DIYU, China therefore becomes a way of seeing in which distance continually changes.

Mountains and rivers may enter a scroll. A world may enter a garden. A distant place may enter the palm and daily life through a crystal.

Each transformation of scale rearranges the relationship between land, matter, and the human observer.

May you find, through this reading, a gaze that can look from the palm toward mountains and rivers—and cherish a small natural object within the immensity of the world.