蒙古｜Mongolia

蒙古位於亞洲內陸，北接俄羅斯，南接中國，國土大部分分布在蒙古高原之上。它沒有海岸，山脈、河流與水分也不以流向海洋作為唯一方向，而是在高原、盆地與廣大內陸之間，形成彼此不同的地景系統。

蒙古的地勢並不是一片平坦而連續的草原。

西部由蒙古阿爾泰山脈構成最鮮明的高山區域，冰雪峰頂、裸露岩壁與高山河谷，使地表呈現強烈的高度差異。蒙古最高點友誼峰位於西部阿爾泰山區，海拔四千三百七十四公尺；向東移動，杭愛山、肯特山與其間的高原和盆地，繼續構成蒙古中部與北部的地形骨架。

北部部分地區接近西伯利亞森林帶，山坡、河谷與湖泊周圍可以出現針葉林和森林草原。向中部與東部移動，森林逐漸稀疏，土地展開為更連續的草原；再向南，水分減少，植被轉為乾草原、半荒漠與戈壁。蒙古由北向南大致跨越森林草原、草原、半荒漠與荒漠等自然地帶，高山地區又因海拔差異形成自己的垂直分帶。

東部的地景較為低緩而開闊。

廣大的平原與草地讓水平線成為主要方向，地表的起伏不一定劇烈，距離卻被拉得很長。山體、河谷與聚落之間往往隔著大面積草原，使空間不是由密集物件填滿，而是由風、天空與可以持續延伸的視線共同構成。

南部則逐漸進入戈壁。

戈壁並不等於一片完全由沙丘組成的沙海。它同時包含礫石平原、乾燥盆地、低山、裸露岩體、稀疏草地與局部沙丘。不同地表彼此交錯，使戈壁既具有荒漠的乾燥，也保存草原、山地與季節性水分留下的痕跡。

在蒙古，氣候與地景之間的關係尤其直接。

深居內陸、距離海洋遙遠，使大部分區域降水有限，季節與日夜之間的溫度差異也十分明顯。水分的多寡，決定森林能否延伸、草原能維持到什麼程度，也影響土地何時轉向半荒漠與荒漠。看似遼闊而穩定的地表，實際上對降雪、乾旱、風與季節變化極為敏感。

這些自然地帶也並非沒有人的土地。

草原上的生活長期依賴牧草、水源與季節，人與牲畜的移動使場所不只由固定建築界定，也由行進路線、營地與反覆返回的土地構成。在較乾燥的區域，能夠支持不同季節放牧的範圍往往更加廣大，移動也成為回應環境變化的方法。

蒙古的地質背景同樣複雜。

它位於中亞造山帶的重要範圍內，不同地質單元在漫長時間裡經歷增生、碰撞、岩漿活動、變質作用與斷裂。這些過程形成多樣的岩體、礦帶與成礦環境，也使蒙古保存煤、銅、螢石、金、鐵、鎢、稀土與其他礦產資源。

因此，「蒙古礦物」並不存在一種可以概括全部的外觀。

礦物可能來自西部山地、北方岩體、中東部草原之下的礦帶，也可能來自南部戈壁的盆地與裸露岩層。相同的國家名稱，可以包含完全不同的母岩、形成條件、晶體結構與採集環境。

蒙古首先提供的是一片廣大的內陸高原。

真正的礦物風土，仍要繼續走進阿爾泰、杭愛、東部草原、戈壁，以及更具體的山體、礦區與採集地點，才能逐漸形成。

Mongolia is a landlocked country in the interior of Asia, bordered by Russia to the north and China to the south. Most of its territory lies within the Mongolian Plateau. Without a coastline, its mountains, rivers, and water systems do not all move toward a nearby sea, but form different landscapes across highlands, basins, and vast continental interiors.

Mongolia is not a single, continuous grassland.

The Mongolian Altai forms the country’s most prominent high-mountain region in the west. Snow-covered summits, exposed rock walls, and alpine valleys create dramatic changes in elevation. Mongolia’s highest point, Khüiten Peak, rises to 4,374 metres in the western Altai. Farther east, the Khangai and Khentii mountains, together with surrounding plateaus and basins, continue to shape the central and northern terrain.

Parts of northern Mongolia approach the southern edge of the Siberian forest zone, where coniferous woodland and forest steppe occur along mountain slopes, rivers, and lakes. Moving toward the center and east, forests become less continuous and the land opens into broader steppe. Farther south, declining moisture produces dry steppe, semi-desert, and desert environments. From north to south, Mongolia broadly crosses forest-steppe, steppe, semi-desert, and desert zones, while high mountains form their own vertical belts.

The eastern landscape is generally lower and more open.

Broad plains and grasslands make the horizon a dominant direction. Relief may appear gentle, yet distances become immense. Mountains, rivers, and settlements are often separated by large expanses of steppe, creating a space shaped not by dense objects, but by wind, sky, and the long movement of the gaze.

Toward the south, the land gradually enters the Gobi.

The Gobi is not a continuous sea of sand dunes. It also contains gravel plains, dry basins, low mountains, exposed rock, sparse grassland, and localized dune fields. These surfaces overlap, allowing the Gobi to combine extreme aridity with traces of steppe, mountain environments, and seasonal moisture.

In Mongolia, the relationship between climate and landscape is especially direct.

Its deep continental position and great distance from the ocean limit precipitation across much of the country, while seasonal and daily temperature changes can be severe. The availability of moisture determines how far forests extend, how grasslands are sustained, and where the land shifts toward semi-desert and desert. A surface that appears broad and stable may be highly sensitive to snowfall, drought, wind, and seasonal change.

These are not landscapes without people.

Life on the steppe has long depended upon pasture, water, and season. The movement of people and livestock means that place is not defined only by permanent buildings, but also by routes, camps, and land repeatedly returned to. In drier zones, the area required to support seasonal grazing becomes larger, and movement itself becomes a way of responding to environmental change.

Mongolia’s geological background is equally complex.

The country occupies an important part of the Central Asian Orogenic Belt, where different geological units have undergone accretion, collision, magmatism, metamorphism, and faulting over immense periods of time. These processes produced varied rock bodies, mineral belts, and ore-forming environments, as well as extensive resources of coal, copper, fluorite, gold, iron, tungsten, rare earth elements, and other minerals.

There is therefore no single appearance that can represent “minerals from Mongolia.”

A specimen may come from western mountains, northern rock bodies, mineral belts beneath the central or eastern steppe, or the basins and exposed formations of the southern Gobi. The same country name can contain entirely different host rocks, formation conditions, crystal structures, and collecting environments.

Mongolia first provides the range of an immense inland plateau.

Its mineral terroir only begins to emerge when the reading moves toward the Altai, the Khangai, the eastern steppe, the Gobi, and eventually to particular mountains, mines, and collecting sites.

蒙古大部分地區屬於古老的大陸地殼，由前寒武紀與古生代岩層構成。

長時間的地質穩定，使花崗岩侵入體、變質岩及火成岩廣泛分布，而乾燥寒冷的氣候則降低了植被覆蓋，使許多岩石與礦脈直接暴露於地表。

這些條件共同形成蒙古獨特的礦物產地，也保存了大量自然形成的岩石地貌。

Much of Mongolia is underlain by ancient continental crust dating back to the Precambrian and Paleozoic eras.

Long-term tectonic stability allowed granite intrusions, metamorphic rocks, and igneous formations to become widely exposed.

Combined with the country’s dry climate and sparse vegetation, many rock formations and mineral veins remain clearly visible at the surface.

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

蒙古的土地向遠方展開。

草原、山地與戈壁彼此相連，地表在漫長的距離中逐漸改變。植物變得稀疏，水源拉開距離，岩石與礫石裸露在天空之下。到了南方，視線經常越過大片沒有遮蔽的土地，直到地平線才停下來。

戈壁並不只是由沙構成的荒漠。

它也有礫石、裸岩、乾燥盆地、低矮山脈與被風長久經過的地表。色彩被陽光與塵土收斂，土地留下灰、黃、褐與暗紅。天空顯得更加寬廣，而人的身體則在這片廣大之中，變得很小。

對底域而言，蒙古首先呈現的是「方向」。

在城市裡，方向經常由道路、牆面、路標與建築決定。

但在草原與戈壁之中，眼前未必有一條清楚的線。

方向可能來自山脊的延伸、風向的改變、雲層的聚集，也可能來自水源、牧草、動物移動的痕跡，以及季節在土地上留下的差異。

人不是沿著一條永遠不變的道路前進。

而是在不斷變化的環境中，反覆確認下一步應當朝向何處。

這種方向，也與追逐有關。

牲畜追隨可以飲水與生長的地方，人則跟隨牲畜、氣候與草場移動。當土地逐漸乾燥，便必須離開；當風雪逼近，也必須尋找可以停留與遮蔽的位置。

追逐在這裡不是毫無目的地奔跑。

它是追隨生命仍能延續的條件。

因此，移動並不代表沒有中心。

一個人的位置可以改變，生活的空間也可以被拆下、搬運，再重新建立。真正維持方向的，不是固定的地址，而是對氣候、地形、動物與土地狀態的持續辨認。

蒙古的遊牧文化，使這種觀看方式長久存在於日常之中。

居所可以移動，季節可以改變，路徑也不一定被永久留在地面。然而，生活並沒有因此失去秩序。人知道何時出發、何時停留，也知道一片土地不能被無止境地使用。

在道路、山口與高地上，人們也會以石塊堆成敖包。

它沒有形成牆，也沒有阻止人繼續前進。

它只是讓廣大的土地之中，出現一個可以辨認的位置。

人從遠方靠近，在此停下、繞行或留下石頭，然後再度出發。風景仍然向四周展開，但道路已經有了一個短暫的中心。

石頭因此不只是被留在原地的物質。

它也可以是一個方向。

蒙古戈壁中的瑪瑙、玉髓與其他石英類礦物，讓這種方向進入更微小的尺度。

它們不一定具有清楚向上的晶尖。

有些只是安靜的塊體，外部帶著粗糙、磨蝕與長久暴露留下的痕跡。色彩並不總是在表面顯現，而可能藏在石頭內部，以層帶、空腔與深淺不同的線條緩慢展開。

方向在這裡，不再只是一個尖端所指向的位置。

它也可能是一條由外向內延伸的紋理，是不同色層彼此包覆的次序，或是視線沿著裂隙與起伏，逐漸進入石頭深處的路徑。

一件戈壁石頭，也許沒有完整而明確的形狀。

它的表面可能不平整，邊緣也可能已經被磨去。它曾經長久留在乾燥的土地上，經過溫差、塵土、碰撞與風化，才以現在的狀態出現在人的面前。

這些痕跡不一定是需要被消除的缺陷。

它們使物質保留了與外部世界接觸過的證據。

風無法被收藏。

遼闊也無法被放進房間。

但當一件來自戈壁的石頭被托在掌心，原本向地平線展開的距離，便暫時收束成可以觸摸的重量。

這不表示石頭代表整片戈壁。

一件礦物無法替蒙古的土地、文化與生活發言。它所保留的，只是一處具體環境曾經留在物質上的表面、結構與色彩。

然而，人仍可能對它產生感情。

不是因為它把荒漠縮小，也不是因為它擁有某種由產地自動賦予的力量。

而是因為一件曾經位於廣大土地中的物質，跨越距離，來到人的生活裡。它使視線在有限的空間中，仍能想起遠方、風與沒有邊界的天空。

收藏在此，不是占有荒漠。

更像是在日常之中，為遠方保留一個可以停下的位置。

石頭被放在桌面上，移動暫時停止。

但它所帶來的方向並沒有消失。

當光線改變，原本不明顯的紋理逐漸浮現；當石頭被轉動，另一側的表面、裂隙與色層重新進入觀看。它留在原地，視線卻仍能沿著它向外行走。

從蒙古進入戈壁，廣大的國家逐漸收束成荒漠的風、地形與地平線；從戈壁進入一件石頭，遙遠的土地又收束成表面、紋理、色彩與重量。

每收束一次，想像便退後一步，物質則向前一步。

而從這件石頭出發，觀看仍然可以再次向外展開。

回到氣候如何改變道路，回到人與動物如何追隨水源與牧草，也回到一片沒有固定邊界的土地，如何使方向不再只是地圖上的線，而成為生命面對變化時，不斷作出的選擇。

蒙古在底域之中，因此呈現為一種關於方向的閱讀。

方向來自風，也來自地形。

來自生命追逐水源與草場，也來自人在遼闊之中，仍然知道何時前進、何時轉向、何時停下。

荒漠將視線帶向遠方。

石頭則讓遠方獲得重量。

在兩者之間，方向不是一條已經畫好的道路，而是一種即使環境不斷改變，仍願意繼續辨認下一步的能力。

願你在閱讀中，找到一個不被邊界限制，也不會在遼闊之中失去自己的方向。

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

The land of Mongolia opens toward the distance.

Grasslands, mountains, and the Gobi are connected across a vast terrain whose surface gradually changes. Vegetation becomes sparse, water sources grow farther apart, and rock and gravel lie exposed beneath the sky. Toward the south, the gaze often passes across immense stretches of unobstructed land before coming to rest upon the horizon.

The Gobi is not simply a desert made of sand.

It also contains gravel plains, exposed rock, dry basins, low mountain ranges, and surfaces crossed by wind over long periods of time. Sunlight and dust quieten its colours into shades of grey, yellow, brown, and dark red. The sky appears wider, while the human body becomes small within the scale of the land.

For DIYU, Mongolia first presents itself through the idea of direction.

Within a city, direction is often established by roads, walls, signs, and buildings.

Across the grassland and Gobi, however, there may be no clearly marked line ahead.

Direction may arise from the extension of a ridge, a change in the wind, or clouds gathering in the distance. It may also be found in water, pasture, the movement of animals, and the differences that each season leaves upon the land.

A person does not follow one unchanging road.

Direction must be recognised again and again within an environment that continues to change.

This form of direction is also connected with pursuit.

Animals move toward places where water and growth remain possible. People move with livestock, climate, and pasture. When the ground becomes too dry, departure becomes necessary. When snow or wind approaches, a more sheltered place must be found.

Pursuit here is not movement without purpose.

It is the pursuit of conditions through which life may continue.

Movement therefore does not mean the absence of a centre.

A person’s location may change, and a living space may be dismantled, carried, and established again. What preserves direction is not a permanent address, but an ongoing awareness of climate, terrain, animals, and the condition of the land.

Mongolia’s nomadic cultures have long carried this way of seeing within daily life.

Homes can move, seasons change, and paths are not always permanently inscribed upon the ground. Yet life does not lose its order. People recognise when to depart, when to remain, and when a place must no longer be asked to carry more.

Along roads, mountain passes, and high ground, stones may also be gathered into an ovoo.

It forms no wall and prevents no one from continuing onward.

It simply makes one location visible within a vast landscape.

A traveller approaches from afar, pauses, circles the stones or adds another, and then departs again. The land remains open in every direction, yet the route has acquired a temporary centre.

Stone is therefore not only matter left behind.

It can also become a direction.

Agate, chalcedony, and other quartz materials from the Mongolian Gobi allow this idea of direction to enter a smaller scale.

They do not always possess a clear termination pointing upward.

Some appear as quiet masses, their outer surfaces carrying roughness, abrasion, and traces of long exposure. Colour may not reveal itself immediately, but remain within the stone, gradually unfolding as bands, cavities, and lines of varying depth.

Direction here is no longer only the place toward which a crystal point is aimed.

It may be a pattern moving from exterior to interior, the sequence through which coloured layers surround one another, or the path by which the gaze follows fractures and contours into the depth of the stone.

A Gobi stone may not possess a complete or clearly defined form.

Its surface may be uneven, and some edges may already have been worn away. It remained upon dry ground through changes in temperature, dust, impact, and weathering before arriving in its present condition.

These traces need not be treated simply as defects to be removed.

They allow matter to retain evidence of its contact with the world beyond itself.

Wind cannot be collected.

Vastness cannot be placed inside a room.

Yet when a stone from the Gobi is held in the palm, distance once extending toward the horizon briefly narrows into a weight that can be touched.

This does not mean that the stone represents the entire Gobi.

A mineral cannot speak for the land, cultures, or lives of Mongolia. It preserves only the surfaces, structures, and colours left by one particular material environment.

A person may nevertheless develop an emotional connection with it.

Not because the stone reduces the desert to a smaller form, nor because origin automatically grants it a special power.

The connection may arise because matter once situated within an immense landscape has crossed a distance and entered human life. Within a limited space, it allows the gaze to remember the distant, the wind, and a sky without visible boundaries.

Collecting, in this sense, is not the possession of a desert.

It is closer to preserving a place where the distant may briefly come to rest within daily life.

The stone is placed upon a table, and its movement temporarily stops.

Yet the direction it carries does not disappear.

As the light changes, patterns previously hidden begin to emerge. When the stone is turned, another surface, fracture, or band of colour enters the act of seeing. The object remains in place, while the gaze continues to travel through it.

As we move from Mongolia into the Gobi, the breadth of the country narrows into desert wind, terrain, and horizon. As we move from the Gobi into a single stone, distant land narrows again into surface, pattern, colour, and weight.

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

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

It may return to the ways climate changes a route, to the ways humans and animals pursue water and pasture, and to the way a land without fixed boundaries transforms direction from a line upon a map into a continuing choice made by life in response to change.

Within DIYU, Mongolia therefore becomes a reading of direction.

Direction comes from wind and from terrain.

It comes from life pursuing water and grass, and from the ability to recognise when to move forward, when to turn, and when to stop within an immense landscape.

The desert carries the gaze toward the distant.

Stone gives the distant weight.

Between them, direction is not a road already drawn. It is the ability to continue recognising the next step even while the environment changes.

May you find, through this reading, a direction that is not confined by boundaries—and does not lose itself within the vastness.