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Part Two: Principle

Preface - Way - Principle - Idea - Method - Synthesis - References
 

I N D E X
Principle

Language
Vocabulary
Grammar


Land
Flat Formations
Convex Formations
Concave Formations
Combinations and Adornments
Overlaps and Connections
Modifications
Textures and Shadings

Water
Sheet Formations
Band Formations
Step Formations
Shores, Banks, and Impediments
Surface Patterns and Reflections
Progression and Diversion

Atmosphere
Sky
Air
Light
Rain and Snow

Vegetation
Bare Trees
Foliage
Evergreens
Moss Dots
Grass


Principle
Chinese aesthetics has been guided by the concept of Tao, or the Way, which accounts for the predominance of landscape themes in Chinese painting. Following the Way, artists aspire to achieve oneness with nature--the ultimate goal in their visual expression. Their works, however, seldom represent what the artists momentarily observe from a stationary viewpoint. They are personal compositions with recognizable elements arranged in a kind of order to suggest evolution of space, maintaining some degree of realism. Such aims do pose specific pictorial problems. How does the Chinese artist tackle the problems?

To paint exactly what is seen within a restrictive framework of space and time contradicts somewhat the concept of Tao, as this practice excludes the artist from being part of the nature portrayed and stresses his separate and independent existence. Of course, at moments of wandering in nature, the Chinese artist becomes an outsider observer as he enjoys, sketches, or else memorizes specific sights of interest. In this way, he is no different from landscape artists of any other civilization. But as he paints, the Chinese artist prefers to rely on his own imagination, and arranges the elements as though he were building a model. From his mind-heart he selects mountains, which he can then rotate and reshape; directs water to wind as springs, jump as waterfalls, or flow as rivers along folds; plants trees and shrubs at choice locations; and combines these elements in a harmonious orchestration displaying vital breath. What results is the creative equivalent of nature.

Concerning this process, Sung Dynasty art essayist Huang Hsiui-fu made the following statement around 1006 A.D.:

Painting is to provide matter with form, but a specially endowed artist can merge his thoughts with the spirit, originate the idea, and establish the structure, all in a wondrous synthesis in accordance with nature's operations.

Remember that Li, the Principle, briefly discussed earlier, governs the operations of nature and defines the laws behind all physical phenomena. Nature, therefore, manifests itself in a variety of elements not haphazardly interrelated. An artist who is not painting exactly what he sees needs, first of all, an excellent acquaintance with the various elements and second, a clear understanding of the laws. Through acquaintance with the elements, the artist will be able to visualize at will in fabricating his scene. Through understanding of the laws, the artist will position the elements in appropriate positions, directions, and proportions, with transitions, extensions, and overlaps conforming to a definite order. The Principle assures that Chinese artists, now and through the ages, accomplish what needs to be accomplished. What they do not accomplish is unnecessary to them. [p. 29]


Language. The elements, how they take shape and how they work together in a painting, comprise the visual language of the artist. The way the artist chooses the elements corresponds to the way a writer chooses words with appropriate meanings, for expressing thoughts and feelings, for communication. As words make up the writerֽs verbal vocabulary, the elements comprise the artist's visual vocabulary. Like words arranged in sentences to make sense, in accordance with the grammar of the language, largely determined by common usage, the elements interrelate to reveal some underlying visual grammar, which is determined by the Principle.

In a general sense, the visual language consists of dots, lines, planes, volumes, tones, colors, and textures. These basic components constitute shapes, which a viewer perceives as forms, either abstract or representational. Representational forms make definite reference to objects and phenomena of the material world, and they must remain reasonably recognizable to any viewer. Tackling representational forms with a range of subject matter is, in fact, fundamental training for every artist, as this enables him to develop a visual vocabulary. [p. 29]

Vocabulary. Through direct observation a skilled artist can cope with any subject that remains unchanging and clearly in sight. Such familiarization with subject matter establishes a vocabulary. In this way the artist is able to capture likeness with less effort, and to deal with aspects of the subject where eyesight does not provide enough information. A Western artist doing figure painting should know every muscle and bone of the human body, and should be familiar with their shapes and structures. Similarly, a Chinese artist working with landscape themes has to be conversant with all the elements occupying his work.

Chinese landscape painting is called shan shui hua [Fig. 35], the three characters standing for respectively mountain, water, and painting. Shan and shui, together as a term, stand for landscape. The Chinese vision of landscape is not as something in an intimate scale, not a confined corner of nature. Mountain and water comprise the two main vocabulary categories of the Chinese artist, whose prime interest is in immense distances and majestic heights. Showing a mountain in its entirety, with springs, falls, and rivers as small details, the artist creates some sort of microcosm, including all the elements that can be found in nature, presenting a world manifesting the spirit of Tao.

This kind of vision cannot be realized without a considerable range of vocabulary. A mountain in a Chinese landscape painting is not the mountain to be observed out in nature. It is probably an ideal mountain, and frequently also represents the artists. A good vocabulary enables the artist to establish his scene at will, without making direct reference to actual locations. If the artist wants to have a towering mountain with a steep front of solid granite, he proceeds to paint it without feeling restricted by any inadequacies of source material. If he wants to have a waterfall, he does not hesitate to put one with the right shape and length at the right place, and to relate it to adjacent elements.

By tradition, a Chinese artist learns to paint by studying with a mentor, copying the mentor's work and those of earlier masters. The artist's acquisition of vocabulary inevitably includes acquaintance with numerous conventions, codified ways to paint particular types of rocks, mountains, trees, or other elements in the manner of this or that great master. Such conventions, which appear in the various painting manuals, represent the essence of the tradition. They present a danger, however, in that an artist may adopt them as formulas, making no attempt to seek real understanding of nature, and just painting in the styles of his predecessors. [p. 30]

Grammar. Visual grammar guides various elements from the artistֽs vocabulary toward the establishment of organic wholeness. Generally speaking for example, a mountain cannot be bent or tilted arbitrarily without jarring the vision, and a tree cannot be planted just anywhere in the pictorial space. Nature, as seen by us in its present manifestations, is the result of millions of years of the earthֽs evolution, itself determined by the laws of physics. Explanations exist for the presence of all objects and substances, as well as for their changes.

To understand the working of the Principle is not exactly the same as making a scientific inquiry, although modern science does provide a wide spectrum of information relevant to any artist with high intellectual curiosity. An artist normally observes nature and discovers the Principle through intuition. He does not have to be a geologist to look into land formations. He need not be able to distinguish types of rocks, nor to identify every tree portrayed in his work. He should be sensitive, however, to the characteristics of shapes and textures, aware of structural significance behind the forms, able to organize pictorial space and effect rhythms. He should be easily moved by beauty, and ready to imbue the subject matter chosen for his work with his personal feelings and thoughts.

Understanding nature is made much easier today by advanced technology. Artists can visit previously unapproachable places with little difficulty, cover long distances in a relatively short time, ascend great heights with ease, view the earth's surface directly from above, use the camera to record sights instantaneously, and glimpse places not yet experienced first hand from photographic, cinematic, video, computer, and print sources. [p. 30]

Land. As land dwellers, we see a landscape dominated by land, the part of the earth above sea level and the part of the environment with the widest variety of elements. From the point of view of a geologist, land consists of different soil and rock formations, the results of weathering, erosion, denudation, sedimentation, earth movements, and metamorphosis over time. From the point of view of the artist, however, land consists of shapes, which can be categorized simply as flat formations, convex formations, and concave formations. [p. 31]


Flat Formations. The term flat formation refers to the type of land normally regarded as a plain, which stretches across and beyond the horizon with only very slight, if any, change in elevation. To illustrate the concept of ideal flatness diagramatically, an artist might draw a series of evenly spaced, horizontally placed parallel lines [Fig 36]. The angle in this case--observed perpendicularly from above--would be quite unnatural, however. In general, the artist relates himself to the subject matter from a slanting view, presenting what is nearer to him in a larger scale than what appears in the distance. Thus, the space between the parallel lines will increase gradually from top to bottom of the pictorial area [Fig. 37]. This technique introduces a sense of perspective, but not to the extent of having the sort of dramatic diminishing effects and vanishing points commonly found in Western art.

The artist may arrange the parallel lines in intermittent narrowing and widening distances to introduce slight rises and falls [Fig. 38], or disarrange them slightly to suggest the irregularity of a wrinkled surface [Fig. 39]. He might bend [Fig. 40] or curl [Fig. 41] the lines to stress surface changes, or even replace horizontal lines with diagonal ones [Fig. 42]. Adding naturalistic touches to the harsh geometry, the artist may transform any of these diagrams into more sensuous pictorial expression [Figs. 43, 44]. Adding descriptive textures with light-dark modulations further enhances the naturalistic effects [Fig 45].

As subject matter for a painting, however, flat formations are probably not interesting enough without the inclusion of other types of formations and additional elements. For example: the artist can exaggerate wrinkles, displaying prominent folds and crevices [Fig. 46], depict a formation with a shoreline [Fig. 47], add creeks and streams to break up the continuity [Fig. 48], or foil the plain with distant hills [ Fig. 49]. [p. 31]


Convex Formations. Land rises and falls, shaped by the earth's internal movements and external forces, leading to convex formations of different sizes and shapes. Such formations, which we might simply call mountains, constitute the most important category of forms and represent the wide range of vocabulary with the most varied manifestations in Chinese landscape painting. To represent a convex formation, the artist should, first of all, grasp its basic form and look into the extent of variations. Then he should examine its different parts to determine which might require special emphasis through modifications, combinations, and applications of texture.

He can distinguish three basic convex formations: pyramidal, semispherical, and prismatic. A pyramidal formation features sharp outlines with a pointed top and a centrally raised edge, characterized by hard, solid rockiness. A semispherical formation has a roundish body and a more earthy surface, suitable for exuberant vegetation. A prismatic formation has a terraced top and steep cliffs.

The simplest way to represent a pyramidal formation is to draw parallel lines [as in Fig. 37] bent in the middle, sloping forty-five degrees down the left and forty-five degrees down the right [Fig. 50]. The parallel lines become serial lines, seen as edges of triangular planes arranged from front to back. Along the tips of the planes, an invisible line divides the solid form into left and right sloping surfaces. To introduce variations, this invisible line can be slanted [Fig. 51], bent [Figs. 52, 53], or curled [Figs 54, 55], just as the parallel arrangement of the planes can change [Figs 56, 57].

Again, an artist can easily transform these geometrical diagrams into naturalistic scenes, with mountains displaying a kind of angular stoniness of almost crystalline quality [Figs 58, 59]. The centrally projecting invisible line represents a dominant ridge, distinguishing the yin and the yang, or the shady and the sunny components. The ridge marks the spine of the mountain, which is the main vein or artery, where minor veins originate. The Chinese call this main vein the dragon's vein, or lung-mo [Fig. 60], and name the vein system mo-lo [Fig. 61]

Substituting the triangular serial planes with semicircular planes [Fig. 62], the artist can construct a semispherical formation. Shifting the semicircular planes, he can depict any specific semispherical mountain [Fig. 63]. This type of mountain displays more flesh than bone, with a much less noticeable ridge, but the presence of a ridge remains essential [Fig. 64]. The frontality of the mountain conveys prominence, and the projection can be located centrally or slightly off-center.

Using rectangular serial planes, meanwhile, the artist can construct a prismatic formation [Figs 65, 66]. This form suggests a steeply rising mountain, of majestic height, in solid granite. The narrow frontality tends to dominate, and there may not be a noticeable ridge [Fig 67]. Shifting the rectangular serial planes results in formations with precarious projections [Figs 68, 69].

Horizontally stacking serial planes is another way to construct any of the mountain forms just discussed [Figs 70-72]. With such planes underlying its structure, the mountain thus visualized displays the layered characteristics of sedimentary rocks [Figs 73, 74]. The serial planes can vary in shape, with more angular edges [Figs. 75, 76] or wavy edges [Fig. 77].

Yet another way of constructing a convex formation is to use a number of vertical and slanting lines, starting from the top and joined to the base, a horizontally positioned plane [Figs. 78-80]. This method is particularly effective for the visualization of prismatic formations, since any horizontally positioned planar shape can represent the terraced top, with the addition of a few vertical lines to represent the cliffs [Figs. 81-83]. Additional horizontally positioned planes, inserted between the top and the base, create specific shape articulations [Figs 84-86].

Generally, convex formations of considerable size are seen as mountains [Fig. 87], but small ones with gradual slopes may appear as hills [Fig. 88]. Mountains consist of distinct parts, with the uppermost part identified as the peak [Fig. 89]. An exaggerated peak tends to soar high in a narrowly pointed shape, becoming a pinnacle [Fig. 90]. Next to the peak might be another high area, a bit flattened, called a shoulder [Fig. 91]. Protruding flat areas along the slopes are known as terraces [Fig. 92], usually surrounded on one or more sides by cliffs, which are nearly vertical rocky walls [Fig. 93]. A ridge starts from the base and leads to the top, marking a continuous, raised portion of a mountain slope [Fig. 94]. One mountain may have several peaks, or may be linked to another or several other mountains, forming a range [Fig. 95]. Familiarity with these commonplace terms helps the artist to understand, and thence to develop, individual shapes and forms, and this vocabulary can be expanded to include more sophisticated geological knowledge. [p. 33]


Concave Formations. If convex formations represent the positive elements of the land, the negative elements exist in spaces between convex formations, in depressions, cracks, sunken folds, hollowed-out areas, and sudden openings on a surface. These concave formations are also essential components of an artist's landscape vision.

Concave formations can be classified as V-shape, U-shape, and O-shape. A V-shape formation is a narrow strip of space between sections of land, such as a narrow passage between the steep slopes of two adjacent mountains. A U-shape formation has a wider bottom and more space than the V-shape formation, defined with steep or gently slanting slopes on two or three sides. An O-shape formation is a circular opening or depression in a vertical or horizontal surface.

To depict a V-shape formation, an artist might bend the parallel horizontal lines in Fig. 37, with lines tilting upwards on both sides, forming a sharp depression at the center [ Fig. 96]. Extending the tilted lines will suggest either flat formations or convex formations to the sides of the concave formation [Figs. 97, 98]. Varying the serial planes in the diagrams [Figs. 99-101] will create ravines, gorges, or canyons, which can be partially concealed [Figs 102, 103].

Bending both ends of the horizontal lines upward in a vertical or slanting direction, meanwhile, produces a U-shape formation [Figs. 104, 105]. Naturalistic scenes based on the diagrams reveal a flat-bottom valley or some kind of basin [Figs 106, 107]. Varying the shapes of the steep cliff walls, and the widths between them, results in different negative shapes [Figs 108, 109]. It is also possible to have enclosure from three sides [Figs 110].

Stacking increasingly large rectangular or circular serial planes front to back produces an O-shape formation [Figs 111, 112]. Found less frequently in nature than either V-shape or U-shape formations, O-shape formations appear as caves, caverns, arches, and windows [Figs. 113-116]. [p. 39]


Combinations and Adornments. Combining the different formations, an artist can achieve a wide variety of interesting shapes. For instance, one or more prismatic formations added to a pyramidal formation appear as terraced areas in a mountain [Figs. 117, 118]. A semispherical formation can incorporate a pyramidal peak, increasing its grandeur [Fig. 119]. All concave formations require the presence of convex or flat formations to give them shape [Figs. 120-122]. O-shape formations create special focal points in any type of land formations [Fig 123].

Introducing adornments such as rocks, boulders, or small stones to surfaces of land formations adds visual interest. Frequently globular or cubical in shape, rocks sometimes look like miniaturized mountains [Figs 124-126]. They may be positioned along the ridge of a convex formation to stress its rising presence [Figs 127, 128], or be nested in concave areas, near the foot of a mountain, and on flat surfaces requiring accentuation [Figs. 129-132]. Other adornments include buildings, bridges, boats, manufactured artifacts, and people, with definite cultural, historical, and geographical references, but these are not the natural components of Chinese landscape painting. [p. 41]


Overlaps and Connections. When two land formations are brought together without being combined into one mass, one formation may overlap the other. They may be entirely separate [Fig. 133] or partially connected [Fig 134].

To establish connection between two rising mountain slopes is to have the ridge of one joining the ridge of the other, showing a feeling of continuity. The ridge, or dragon's vein, can move uphill and down hill. In moving downhill, it might extend out of sight at the back of the mountain and must be implied [Fig. 135]. Using the dragon's vein concept, an artist can connect a series of mountains in obvious and less obvious manners [Figs. 136, 137]. [p. 44]


Modifications. An artist begins to visualize a land formation with external contours, which define the overall shape [Fig. 138]. Internal contours, added to suggest folds on the slopes, reveal the position and direction of the ridge and determine its volume [Fig. 139]. Modification of both the external and the internal contours, or simply the internal contours, resulting in alteration of their shape, length, quantity, spacing, and direction, remodels the entire mass [Figs. 140-142]. It is possible, however, to modify the internal contours considerably while generally maintaining the basic shape of the external contours [Fig. 143].

Modification means giving individuality to the form created, introducing refinements, establishing a center of interest, and stressing rhythmical movements. Like a sculptor chiseling marble, kneading clay, or molding with plaster, the painter delineating contours creates, at will, protrusions and depressions, smoothness and cragginess, to achieve the appropriate simplicity or complexity. [p. 45]


Textures and Shadings. After the internal contours are defined, the next step is to apply textures and shadings. Textures provide a descriptive quality to the surfaces. Shadings show the modeling of light and enhance solidity of the form. The application of textures, an important part of the Chinese painting process, incorporates the use of specific brushstrokes. Shadings are done with a tonal wash that helps to pull the textures together, strengthening light-dark effects not related to any single light source.

The Chinese use the character ts'un [Fig. 144], also meaning wrinkles, to stand for textural brushstrokes applied to land formations. Over the centuries, the masters developed various types of ts'un techniques, which form the essential foundation of any artist's training. Names for the brushstrokes were for the most part given by followers of the pioneering master. In relation to the classification of pyramidal, semispherical, and prismatic formations discussed earlier, three basic types of ts'un techniques exist: ax-cut strokes, hemp-fiber strokes, and bent-ribbon strokes. [A f ull discussion of brush techniques appears in Part Four, under the heading Brush].

To make an ax-cut stroke, the artist holds the brush in a slanting position so that the brush tip is bent slightly to one side [Fig. 145]. The stroke has a triangular shape: Its application resembles chiseling with an ax. Using a pen or pencil, the artist can approach the same effect by first exerting pressure, then letting the line taper off [Fig. 146].

The ax-cut stroke is most useful for depicting hard, rocky surfaces, as in pyramidal formations [Fig. 147]. Contours for such a formation can be in sharply bending lines [Fig. 148], with the strokes applied at right angles to the contours to stress sharpness and cragginess [Fig. 149]. The stroke is also effective for the description of angularly shaped rocks of crystalline quality and sedimentary rocks displaying layered structures [Figs. 150, 151]. The best-known exponents of the ax-cut stroke are Li T'ang, Ma Yüan, and Hsia Kwei, associated with the Northern School of landscape painting, which thrived particularly in the Southern Sung Dynasty [1127-1280 A.D.].

A slightly sinuous and perhaps broken line, the hemp-fiber stroke is used for describing the gentle slopes of earthy semispherical formations [Fig. 152]. For this the artist applies layers of the strokes, usually with a vertically held brush, with more density next to the outer sides of curved, internal contours to give them a clear definition [Fig. 153].

Long hemp-fiber strokes express relatively smooth surfaces [Fig. 154]. Short hemp-fiber strokes provide more wrinkles [Fig. 155]. Entangled hemp-fiber strokes tend to intercept one another from different directions, expressing roughness of the surface and a feeling of casualness in the brush application [Fig. 156]. The great Southern School master Tung Yüan [907-960 A.D.] first developed the short hemp-fiber strokes. These were given variations and generally favored by the literati painters, who dominated mainstream Chinese landscape painting beginning with the emergence of the Four Masters of the Yüan Dynasty. The most important of the Four Masters is Huang Kung-wang [1269-1354 A.D.], who practiced the strokes in a loose, calligraphic manner.

An artist obtains a bent-ribbon stroke with a brush held slantingly, making a horizontal line, then bending it downward sharply into a slightly thicker vertical line [Fig. 157]. This stroke is appropriate for representing prismatic formations, sedimentary rocks, slab-shape rocks, and terraces [Figs. 158-160]. This stroke, however, is of limited application, but the artist can overcome the restrictions by combining it with other brush expressions, particularly ax-cut strokes in depicting cubical rocky structures [Figs. 161, 162]. Bent-ribbon strokes were created by Ni Tsan [1301-1374 A.D.], another of the Four Masters, and later practiced by Hung-jen [circa 1603-1663 A.D.].

Among the many less popular types of strokes are the lotus-leaf strokes, which have lines branching and proliferating downward as veins and wrinkles [Fig. 163]; the raveled-rope strokes, with long and dry brush marks resembling disarranged rope fibers [Fig. 164]; the entangled-firewood strokes, with sharp lines from conflicting directions [Fig. 165]; the ox-hair strokes, featuring fine curly lines densely applied [Figs. 166, 167]; and the cloud-head strokes which suggest globular rock forms [Fig. 168]. Of course, as the artist acquires all of the different techniques, he may apply any of them as appropriate to the form. He may intermix various types in one painting, or develop his own special types of strokes.


Water Whereas land provides solid elements with definite forms, water, as a liquid element, helps to enhance the sense of movement in a painting. Water tends to seek a level surface if it is contained. It fills cavities and, easily affected by gravity, will rush down slanting channel beds and passages. Water has no form of its own, except for its surface patterns, which may display some specific shapes. The general shape of a body of water is defined by the land that marks its edge, on one, two, or more sides. So, with reference to its relationship with land, water breaks down into three basic types: sheet formations, band formations, and step formations. [p. 50]

Water
Whereas land provides solid elements with definite forms, water, as a liquid element, helps to enhance the sense of movement in a painting. Water tends to seek a level surface if it is contained. It fills cavities and, easily affected by gravity, will rush down slanting channel beds and passages. Water has no form of its own, except for its surface patterns, which may display some specific shapes. The general shape of a body of water is defined by the land that marks its edge, on one, two, or more sides. So, with reference to its relationship with land, water breaks down into three basic types: sheet formations, band formations, and step formations. [p. 50]


Sheet Formations. The term sheet formations refers to large, level bodies of water. These are found on oceans and seas, which may or may not be next to any coastal land and which may contain islands [Figs. 169-171]. Bays, with surrounding land on one or more sides [Fig. 172], and lakes, completely or almost completely surrounded by land [Fig. 173], also represent sheet formations.

An artist might depict a sheet formation graphically either as a horizontally placed rectangle, a circle, or a less readily identifiable shape [Figs. 174-176]. Varying The edges in a curvilinear manner and converting the figure into a stack of serial planes, the artist could obtain broad patterns made by the flow of currents [Figs. 177, 178]. With added land formations, some edges become more clearly defined [Fig. 179]. [p. 51]


Band Formations. As water flows along a valley or through a gorge, it runs and winds as a band. Band formations denote creeks, streams, and rivers, which move forward with directional significance. These can be illustrated diagramtically as a horizontally placed S-shape with a bit of perspective [Fig 180]. Notice that the band widens as the curves turn downward and narrows as they turn sideways, and that the lower end, which is closer, is wider than the upper end, in the distance.

If it represents a big river, a band formation can appear as a broad passage [Fig. 181]. In most cases, it is a narrow path, sometimes completely exposed [Fig. 182], sometimes partially concealed [Fig. 183], leading to a sheet formation [Fig. 184]. The land formation it passes through can appear as vertical cliffs [Fig. 185], or as a series of gradually sloping projections, or sand banks [Fig. 186]. [p. 52]


Step Formations. In a band formation, water might move from a higher level to a lower level, but the change is always gradual. A sudden change of level causes the water to jump, resulting in a step formation. This could be in one or two simple steps, or multiple steps [Figs. 187, 188]. The steps need not be parallel, and could split into rows [Figs. 189, 190]. Step formations include springs and waterfalls [Figs. 191, 192]. Rapids are half-way between band and step formations [Fig. 193].

Due to the change of altitude, as the water moves it washes off soft soil, carves hard rocks, carries sediments, and moves rocks in its course. The rocks, frequently scattered in the rapids, lodged at the more level places in springs, and deposited at the lower end of waterfalls, split up the water flow into ribbons [Figs. 194, 195]. Exposed rocks along the course, especially at the starting point of the fall, also cause splitting effects [Fig. 196].

Step formations tend to stress verticality, their water surfaces resembling curtains draped in soft folds [Fig. 197]. A large waterfall might have a curvilinear upper edge, anchoring several step formations grouped in close proximity [Fig. 198]. [p. 53]


Shores, Banks, and Impediments. Except in the case of an ocean or sea not edged by land at all, water is accommodated or wrapped by land, which provides the elements that shape the body of water. Generally, it is concavity on flat or convex land formations that holds the water, or directs its course.

A bay or lake is fringed with a shore, which may be composed of steep cliffs or gentle slopes. Along the shore may be a sandy beach, with pebbles and rocks, useful adornments providing desirable detail in a painting [Figs. 199, 200].

A stream or river has a bank on each side. These curve in and out, but not always in the same manner. The two banks at different intervals could be near or far from each other, with different kinds of land formations [Figs. 201, 202]. As a river makes a turn, the outer curve of the turn usually displays steeper walls, caused by the significant effects of erosion, than the inner curve, which has a flatter land formation [Fig. 203]. This effect does not appear at every turn or in every painting, however, since certain kinds of land structure might resist erosion.

Loose rocks and hard rocky formations projecting above the water surface act as impediments to the water flow. They are essential details for a waterfall, dividing the water surface [Fig. 204] and helping to articulate the step formation [Fig. 205]. [p. 55]


Surface Patterns and Reflections. Visually intrinsic to water is its surface pattern, which reveals calmness or movement and is affected by wind, adjacent land formations and impediments, light, and reflections. Moving water generally displays more articulated lace-lilke patterns than still water. Water moves in currents, with the direction and velocity of the currents sometimes quite visible [Fig. 206].

To depict currents an artist adds texture in the form of short, horizontal, diagonal, straight, or sinuous lines [Fig. 207]. The texture for ripples, effected by wind or breeze in still water, is less agitated and most noticeable near the shore or bank [ Fig. 208]. Water speeding down a narrow passage could have a lace-like pattern in a forward-pointing direction [Fig. 209].

Water as sheet formation might display waves, suggesting a rough sea caused by strong wind, in a pattern reminiscent of fish scales [Fig. 210]. Crests and foam, or whitecaps, further emphasize the turbulence [Fig. 211].

We see reflections in water as the mirroring of trees and land formations along the shore of a lake or the bank of a river, or else as the mirroring of light from the sky. Reflecting the sky, the water surface displays a sweeping area of brightness, with or without clear definition [Fig. 212]. Reflecting solid objects, the surface mirrors corresponding shapes when the water is quite calm, but produces blurred images in most cases [Fig. 213]. Depending more on a fixed viewpoint, however, reflection is rarely expressed in traditional Chinese landscape painting. [p. 56]


Progression and Diversion. Water moving as a stream or a river carves through the land surface and continues its progress. Sometimes it is fully visible and sometimes partially hidden behind trees and foliage, protrusions of rock, and land masses [Fig. 214].

The path of moving water can diverge at any point, splitting into two or more streams [Fig. 215], just as two or more separate streams can join as one [Fig. 216]. In fact, various types of water formations spreading over a large land area can join and split in an intricate manner [ Fig. 217]. When depicting the complicated progression of water, the artist must be sure to maintain its flow, so that a viewer may trace the entire course with its apparently disconnected parts. [p. 57]


Atmosphere
Beyond land and water is the earth's atmosphere, including a number of phenomena, such as the sky, air, light, rain, and snow, that are not earthbound and lack definable shapes. Such elements enable the artist to introduce voidness, fading effects, and tonal changes in a painting, and facilitate the creation of moods related to time, season, climate, and weather. [p. 58]

Sky. Artists generally leave the sky blank in Chinese landscape painting. Sometimes they apply a simple ink tone, most often in depicting wintry scenes. The presence of sky is implied behind mountain peaks, but the exact area of sky remains vague, since the paintings rarely display a marked horizon dividing the land or water from the sky. And since the sun, the moon, the stars, or other heavenly bodies seldom appear in Chinese landscapes, the sky frequently resembles that of an overcast day, with no distinct clouds. The blank sky traditionally serves the purpose of carrying the artists' inscriptions. [p. 58]


Air. Air is invisible, but it carries moisture that may appear as haze and mist. Artists can represent haze by depicting distant hills, mountains, or other background elements in lighter and lighter tones, with faint ink and with less and less detail. Likewise, giving the lower part of a mountain scarce texture and faint ink treatment suggests the presence of mist.

Introducing mist helps to stress distantness and separateness of the elements [Fig. 218]. A mountain with mist at its foot tends to appear very high: as it is not resting on any definite ground, its receding distance opens to free interpretation [Fig. 219]. Indeed, in troducing mist to a landscape is like adding to it a veil of mystery that enhances its spirituality.

Clouds, again made of the moisture in the air, help to break up the solidity of land formations and create a sense of movement in a composition. Clouds appear in clusters, rows, strips, and layers, composed of large and small spherical and rippling forms with feathery edges [Figs. 220-223]. They rise from valleys and other concavities, stretch across the fronts of mountains, lace distant peaks, spread in the sky, and serve to shield off any part of a scene [Figs. 224-227]

Air movements have no shapes. As wind blows, it bends branches, weeds, and grass in one direction. Artists cannot depict wind directly, but can show the presence of wind by stressing its effects on the softer elements of the landscape. [p. 58]


Light. Chinese landscape painters use lightness and darkness as rhythmic modulations of ink tones and textural applications. They are not interested in a fixed light source, which imposes a sense of transience. Backlit scenes, bursts of light from above, long shadows cast across surfaces of land and water, and other dramatic light situations are only found in some contemporary Chinese painting showing Western influence.

In traditional works, elements are modeled with soft light from above, with sunken and wrinkled areas given darker tones or denser textures. The two sloping sides of a mountain may be treated differently to enhance solidity [Fig. 228]. The front of a mountain may be light, allowing trees and shrubs to be visible [Fig. 229], or it may be dark, with fringed mist [Fig. 230]. [p. 60]


Rain and Snow. A series of vertical but slightly slanting parallel streaks left as gaps in a densely textured area expresses the presence of heavy rain, the effects of which can be strengthened with subsequent ink washes. Usually heavy rain is accompanied by wind, and the streaks appear in a diagonal direction. Layers of horizontal dots in rather undefined shapes suggest light rain veiling the landscape with general haziness [Fig. 231].

Opaque white pigment soaking the hair of a brush, which is then lightly tapped to sprinkle tiny dots of white on the surface of the painted area, creates the illusion of falling snow. A snow-covered landscape is not done with white pigment, however. Here, darkened sky and water surfaces provide a tonal contrast to light and scantily painted areas, which become positive forms with white surfaces. [p. 60]


Vegetation
Vegetation provides more than mere adornment in a landscape, for plants and trees, as organic matter, contribute a sense of life and movement to the general scene. Furthermore, vegetation suggests conditions of a particular season, strengthening communication of feelings. Vegetation encompasses a wide range of subjects including grass, shrubs, trees, forests, and numerous kinds of ground-covering growth, from clearly definable shapes to vaguely discernible presences to textural manifestations. In special cases, vegetation serves as the dominant feature in a painting, with mountains as background elements. [p. 61]

Bare Trees. A tree consists of a trunk, with roots extending from its base, branches extending from its sides and top, and foliage encrusting the branches. An artist normally draws the trunk of a tree first, indicating its position, height, and thickness. The trunk may be twisted or slanted, and its surface may carry wrinkled lines and knots. Knots represent scars from broken branches, and their occurrence affects the shape of the trunk.

Next come the major branches. Branching out normally reduces the trunk's thickness. With further branching from the major branches, and the display of some root formation similar to the branching pattern, a bare tree is visualized [Fig. 232].

Trees should convey some feeling of rhythmic movement, free from stiffness. A single bare tree should bend gracefully, balanced with the branches [Fig. 233]. Groupings of two or more bare trees should show the trunks and branches overlapping and intersecting in different directions [Figs. 234-236]. Different tree trunks should appear behind, above, and in front of specific contour lines, to express their spatial relationships [Fig. 237].

The branching pattern, further articulated with shapes and lengths of the branches, gives each bare tree its identity. There are three basic branching patterns. The ascending pattern is constructed with most of the branches pointing in an upward direction, which is called the deer-horn method [Fig. 238]. The descending pattern shows drooping branches. If the branches are short and curly, it is referred to as the crab-claw method [Fig. 239]. When the branches are long, the tree takes the shape of a willow [Fig. 240]. The side-stretching pattern is attained with branches delineated horizontally [Fig. 241].

The three basic patterns provide guidance for the artist rather than dictating shapes. Some trees do not have branches of strong directional orientation, and all patterns can be given some diagonal bias to suggest effects of wind [Fig. 242]. Some branches wind and loop significantly, with many entanglements [Fig. 243]. Major branches grow at random [Fig. 244], or almost symmetrically [Fig. 245]. Artists can combine randomness and symmetry and juxtapose high and low trunks [Figs. 246, 247]. Branches can grow in smooth curves [Fig. 248], sharp bends [Fig. 249], or knotty twists [Fig. 250], and in short or long lengths [Figs. 251, 252].

In general, bare trees are deciduous, featured in autumn and winter scenes. Artists often draw trees with foliage as bare trees at the initial stage of the painting process, to provide the general structure and rhythm of their forms. [p. 61]


Foliage. Foliage refers to the leaves on the branches, depicted with a textural application that spreads into a vaguely distinguishable shape. Chinese artists tend to use characteristic leaf shapes as visual symbols, grouping the symbols on branches in accordance with natural growth processes. The textural application they employ falls into two broad categories: dotted formations and outlined formations. Numerous types of each exist for covering a wide variety of trees.

Dotted formations describe leaves of darker shades, which tend to be small. The simplest application involves round or oval dots [Fig. 254], or short strokes, with curved or wedged shapes, arranged vertically or horizontally [Figs. 255, 256]. The dots or short strokes may be grouped and shaped to reveal a radiating pattern, generally pointing upward [Fig. 257] or downward [Fig. 258], and repeated with slight variations.

Outlined formations describe leaves of lighter shades and of larger size. Foliage begins with a unit, created as a simple or special shape in outline, then repeated [ Fig. 259]. The unit can have a radiating pattern [Fig. 260], and the outlines facilitate the introduction of color.

Trees with an exuberant display of foliage give the feeling of warmer climates and fertile land formations [Fig. 261]. Trees with scanty foliage suggest the approach of a cold season [Fig. 262]. Of course, trees with different types of foliage can appear in the same landscape [Figs. 263-265]. Both dotted and outlined formations can be given expressionistic treatment [Figs. 266, 267], although outlined formations generally belong to paintings of a tighter style [Fig. 268].

Trees in the middle distance are smaller, but while they still maintain individually distinct shapes, their foliage is no different from that of nearby trees, except that it is less detailed [Figs. 269, 270]. Trees in the far distance lack clear identity, and their foliage can be considerably abbreviated [Fig. 271]. [p. 65]


Evergreens. Evergreens have needle-like leaves that remain on the branches all year long. Pines, spruces, and cypresses belong to this nondeciduous category. Among these, pines are of the utmost significance, symbolizing the unyielding tenacity of the virtuous. Chinese scholars. A Chinese pine of the temperate zone does not grow in a vertical cone shape, but has a long trunk with branches stretching horizontally near the upper end of the trunk [Figs. 272, 273]. The branches tend to gnarl and bend with angular gestures [Figs. 274, 275, and the trunk can writhe in an amazing shape on rocky surfaces and steep cliffs [Figs. 276, 277].

At close distance, an evergreen's needle-like leaves are expressed as units of fine strokes in a fan-shape or radiating pattern, positioned on the branches in layered clusters [Figs. 278-281]. Farther away, the fan-shape patterns of the leaves become rows of short vertical strokes [Fig. 282]. Distant wooded areas higher up in the mountains frequently feature evergreens in conical shapes, made with vertical strokes representing the trunks and layers of horizontal strokes representing the leaves [Figs. 283, 284]. [p. 67]


Moss Dots. A textural application unique to Chinese landscape painting, moss dots consist of round or irregularly shaped specks of ink [Figs. 285, 286], or of oval dots or short strokes laid horizontally, vertically, or diagonally [Figs. 287, 288]. Spreading rhythmically over land formations, edges of water, and even on tree trunks and roots, moss dots serve as accentuations, strengthen contours, enhance contrasts of tones and densities, provide a sense of general pictorial unification, and add a finishing touch. Moss dots do not represent moss formations but suggest vegetation that may be interpreted loosely. On land formations of closer distance, they might express minor plant growth. On more distant land formations, they represent trees, shrubs, or wooded areas. As distant trees are given more and more abbreviated brushwork treatment, they gradually intermix with or turn into moss dots [Fig. 289].

Blending moss dots with ts'un strokes as textural treatment for land formations provides extra richness and depth [Fig. 290]. Horizontal moss dots may be applied so abundantly that they cover and even replace the ts'un strokes and some of the contours [Fig. 291]. [p. 69]


Grass. This category of vegetation, visualized as fine and short vertical lines, perhaps slightly curled, applied along external and internal contours of land formations or on water surfaces, often in rows, includes all similar kinds of plant growth with sheath-like leaves, such as weeds, reeds, and rushes [Figs. 292, 293]. On land, grasses tend to appear on foreground terraced surfaces and along the feet of trees, sometimes hanging from protruding rocks and cliffs [Fig. 294]. On water, they fringe river banks and lake shores, suggesting the presence of marsh [Figs. 295, 296]. [p. 70]
 




 

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