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Canyons of the Colorado

by John Wesley Powell

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Canyons of the Colorado

southern margins constitute the highest steps of the great system of terraces of erosion. This escarpment is known as the Pink Cliffs. Above, pine forests are found; below the cliffs are hills and sand-dunes. The cliffs themselves are bold and often vertical walls of a delicate pink color.

In one of the earlier years of exploration I stood on the summit of the Pink Cliffs of the Paunsagunt Plateau, 9,000 feet above the level of the sea. Below me, to the southwest, I could look off into the canyons of the Virgen River, down into the canyon of the Kanab, and far away into the Grand Canyon of the Colorado. From the lowlands of the Great Basin and from the depths of the Grand Canyon clouds crept up over the cliffs and floated over the landscape below me, concealing the canyons and mantling the mountains and mesas and buttes; still on toward me the clouds rolled, burying the landscape in their progress, until at last the region below was covered by a mantle of storm—a tumultuous sea of rolling clouds, black and angry in parts, white as the foam of cataracts here and there, and everywhere flecked with resplendent sheen. Below me spread a vast ocean of vapor, for I was above the clouds. On descending to the plateau, I found that a great storm had swept the land, and the dry arroyos of the day before were the channels of a thousand streams of tawny water, born of the ocean of vapor which had invaded the land before my vision.

Below the Pink Cliffs another irregular zone of plateaus is found, stretching out to the margin of the Gray Cliffs. The Gray Cliffs are composed of a homogeneous sandstone which in some places weathers gray, but in others is as white as virgin snow. On the top of these cliffs hills and sand-dunes are found, but everywhere on the Gray Cliff margin the rocks are carved in fantastic forms; not in buttes and towers and pinnacles, but in great rounded bosses of rock.

The Virgen River heads back in the Pink Cliffs of the Markagunt Plateau and with its tributaries crosses one of these plateaus above the Gray Cliffs, carving a labyrinth of deep gorges. This is known as the Colob Plateau. Above, there is a vast landscape of naked, white and gray sandstone, billowing in fantastic bosses. On the margins of the canyons these are rounded off into great vertical walls, and at the bottom of every winding canyon a beautiful stream of water is found


A PERMIAN BUTTE.


VERMILION CLIFFS AT KANAB.


CLIFFS AND TERRACES.

running over quicksands. Sometimes the streams in their curving have cut under the rocks, and overhanging cliffs of towering altitudes are seen; and somber chambers are found between buttresses that uphold the walls. Among the Indians this is known as the “Rock Rovers’ Land,” and is peopled by mythic beings of uncanny traits.

Below the Gray Cliffs another zone of plateaus is found, separated by the north-and-south faults and divided from the Colob series by the Gray Cliffs and demarcated from the plateaus to the south by the Vermilion Cliffs. The Vermilion Cliffs that face the south are of surpassing beauty. The rocks are of orange and red above and of chocolate, lavender, gray, and brown tints below. The canyons that cut through the cliffs from north to south are of great diversity and all are of profound interest. In these canyon walls many caves are found, and often the caves contain lakelets and pools of clear water. Canyons and re-entrant angles abound. The faces of the cliffs are terraced and salients project onto the floors below. The outlying buttes are many. Standing away to the south and facing these cliffs when the sun is going down beyond the desert of the Great Basin, shadows are seen to creep into the deep recesses, while the projecting forms are illumined, so that the lights and shadows are in great and sharp contrast; then a million lights seem to glow from a background of black gloom, and a great bank of Tartarean fire stretches across the landscape.

At the foot of the Vermilion Cliffs there is everywhere a zone of vigorous junipers and piñons, for the belt of country is favored with comparatively abundant rain. When the clouds drift over the plateaus below from the south and west and strike the Vermilion Cliffs, they are abruptly lifted 2,000 feet, and to make the climb they must unload their burdens; so that here copious rains are discharged, and by such storms the cliffs are carved and ever from age to age carried back farther to the north. In the Pink Cliffs above and the Gray Cliffs and the Vermilion Cliffs, there are many notches that mark channels running northward which had their sources on these plateaus when they extended farther to the south. The Rio Virgen is the only stream heading in the Pink Cliffs and running into the Colorado which is perennial. The other rivers and creeks carry streams of water in rainy seasons only. When a succession of dry years occurs the canyons coming through the


CANYONS OF THE COLORADO.

cliffs are choked below, as vast bodies of sand are deposited. But now and then, ten or twenty years apart, great storms or successions of storms come, and the channels are flooded and cut their way again through the drifting sands to solid rock below. Thus the streams below are alternately choked and cleared from period to period.

To the south of the Vermilion Cliffs the last series or zone of plateaus north of the Grand Canyon is found. The summits of these plateaus are of cherty limestone. In the far west we have the Shiwits Plateau covered with sheets of lava and volcanic cones; then climbing the Hurricane Ledge we have the Kanab Plateau, on the southwest portion of which the Uinkaret Mountains stand—a group of dead volcanoes with many black cinder cones scattered about. It is interesting to know how these mountains are formed. The first eruptions of lava were long ago, and they were poured out upon a surface 2,000 feet or more higher than the general surface now found. After the first eruptions of coulees the lands round about were degraded by rains and rivers. Then new eruptions occurred and additional sheets of lava were poured out; but these came not through the first channels, but through later ones formed about the flanks of the elder beds of lava, so that the new sheets are imbricated or shingled over the old sheets. But the overlap is from below upward. Then the land was further degraded, and a third set of coulees was spread still lower down on the flanks, and on these last coulees the black cinder cones stand. So the foundations of the Uinkaret Mountains are of limestones, and these foundations are covered with sheets of lava overlapping from below upward, and the last coulees are decked with cones.

Still farther east is the Kaibab Plateau, the culminating table-land of the region. It is covered with a beautiful forest, and in the forest charming parks are found. Its southern extremity is a portion of the wall of the Grand Canyon; its western margin is the wall of the West Kaibab Fault; its eastern edge is the wall of the East Kaibab Fault; and its northern point is found where the two faults join. Here antelope feed and many a deer goes bounding over the fallen timber. In winter deep snows lie here, but the plateau has four months of the sweetest summer man has ever known.

On the terraced plateaus three tribes of Indians are found: the Shiwits (“people of the springs”), the Uinkarets (“people of the pine

A MIDSUMMERDAY’S DREAM ON THE COLOB.


CANYONS OF THE COLORADO.

mountains”), and the Unkakaniguts (“people of the red lands,” who dwell along the Vermilion Cliffs). They are all Utes and belong to a confederacy with other tribes living farther to the north, in Utah. These people live in shelters made of boughs piled up in circles and covered with juniper bark supported by poles. These little houses are only large enough for half a dozen persons huddling together in sleep. Their aboriginal clothing was very scant, the most important being

AN INDIAN VILLAGE.

wildcatskin and wolfskin robes for the men, and rabbitskin robes for the women, though for occasions of festival they had clothing of tanned deer and antelope skins, often decorated with fantastic ornaments of snake skins, feathers, and the tails of squirrels and chipmunks. A great variety of seeds and roots furnish their food, and on the higher plateaus there is much game, especially deer and antelope. But the whole country abounds with rabbits, which are often killed with arrows and


CLIFFS AND TERRACES.

caught in snares. Every year they have great hunts, when scores of rabbits are killed in a single day. It is managed in this way: They make nets of the fiber of the wild flax and of some other plant, the meshes of which are about an inch across. These nets are about three and a half feet in width and hundreds of yards in length. They arrange

ANTINAINTS, PUTUSIV, AND WICHUTS, IN FESTAL DRESS.

such a net in a circle, not quite closed, supporting it by stakes and pinning the bottom firmly to the ground. From the opening of the circle they extend net wings, expanding in a broad angle several hundred yards from either side. Then the entire tribe will beat up a great district of country and drive the rabbits toward the nets, and finally into


CANYONS OF THE COLORADO.

the circular snare, which is quickly closed, when the rabbits are killed with arrows.

A great variety of desert plants furnish them food, as seeds, roots, and

PERSPECTIVE VIEW OF TYPICAL SOLITARY HOUSE.

stalks. More than fifty varieties of such seed-bearing plants have been collected. The seeds themselves are roasted, ground, and preserved in cakes. The most abundant food of this nature is derived from the sunflower and the nuts of the piñón. They still make stone arrowheads, stone knives, and stone hammers, and kindle fire with the drill. Their medicine men are famous sorcerers. Coughs are caused by invisible winged insects, rheumatism by flesh-eating bugs too small to be seen, and the toothache by invisible worms. Their healing art consists in searing and scarifying. Their medicine men take the medicine themselves to produce a state of ecstasy, in which the disease pests are discovered. They also practice dancing about their patients to drive away the evil beings or to avert the effects of sorcery. When a child is bitten by a rattlesnake the snake is caught and brought near to the suffering urchin, and ceremonies are performed, all for the purpose of prevailing upon the snake to take back the evil spirit. They have quite a variety of mythic personages. The chief of these are the


CLIFFS AND TEBEACES.

Enupits, who are pigmies dwelling about the springs, and the Rock Rovers, who live in the cliffs. Their gods are zoic, and the chief among them are the wolf, the rabbit, the eagle, the jay, the rattlesnake, and the spider. They have no knowledge of the ambient air, but the winds are the breath of beasts living in the four quarters of the earth. Whirlwinds that often blow among the sand-dunes are caused by the dancing of Enupits. The sky is ice, and the rain is caused by the Rainbow God; he abraids the ice of the sky with his scales and the snow falls, and if the weather be warm the ice melts and it is rain. The sun is a poor slave compelled to make the same journey every day since he was conquered by the rabbit. These tribes have a great body of romance, in which the actors are animals, and the knowledge of these stories is the lore of their sages.

Scattered over the plateaus are the ruins of many ancient stone pueblos, not unlike those previously described.

The Kanab River heading in the Pink Cliffs runs directly southward

PERSPECTIVE VIEW OP ROUND-HOUSE STRUCTURE OF LAVA.

and joins the Colorado in the heart of the Grand Canyon. Its way is through a series of canyons. From one of these it emerges at the foot of the Vermilion Cliffs, and here stood an extensive ruin not many years ago. Some portions of the pueblo were three stories


CANYONS OF THE COLORADO.

high. The structure was one of the best found in this land of ruins. The Mormon people settling here have used the stones of the old pueblo in building their homes, and now no vestiges of the ancient structure remain. A few miles below the town other ruins were found. They were scattered to Pipe’s Springs, a point twenty miles to the westward. Ruins were also discovered up the stream as far as the Pink Cliffs, and eastward along the Vermilion Cliffs nearly to the Colorado River, and out on the margin of the Kanab Plateau. These were all ruins of outlying habitations be-longing to the Kanab pueblo. From the study of the existing pueblos found elsewhere and from extensive study of the ruins, it seems that everywhere tribal pueblos were built of considerable dimensions, usually to give shelter to several hundred people. Then the people cultivated the soil by irrigation, and had

AN ANCIENT CLIFF HOUSE.


A ZUÑI EAGLE CAGE.


A VIEW OF ZUÑI.


CLIFFS AND TERRACES.

their gardens and little fields scattered at wide distances about the central pueblo, by little springs and streams and wherever they could control the water with little labor to bring it on the land. At such points stone houses were erected sufficient to accommodate from one to two thousand people, and these were occupied during the season of cultivation and are known as rancherías. So one great tribe had its central pueblo and its outlying rancherías. Sometimes the rancherías were occupied from year to year, especially in time of peace, but usually they were occupied only during seasons of cultivation. Such groups of ruins and pueblos with accessory rancherías are still inhabited, and have been described as found throughout the Plateau Province except far to the north beyond the Uinta Mountains. A great pueblo once existed in the Uinta Valley on the south side of the mountains. This is the most northern pueblo which has yet been discovered. But the pueblo-building tribes extended beyond the area drained by the Colorado. On the west there was a pueblo in the Great Basin at the site now occupied by Salt Lake City, and several more to the southward, all on waters flowing into the desert. On the east such pueblos were found among mountains at the headwaters of the Arkansas, Platte, and Canadian rivers. The entire area drained by the Rio Grande del Norte was occupied by pueblo tribes, and a number are still inhabited. To the south they extended far beyond the territory of the United States, and the so-called Aztec cities were rather superior pueblos of this character. The known pueblo tribes of the United States belong to several different linguistic stocks. They are far from being one homogeneous people, for they have not only different languages but different religions and worship different gods. These pueblo peoples are in a higher grade of culture than most Indian tribes of the United States. This is exhibited in the slight superiority of their arts, especially in their architecture. It is also noticeable in their mythology and religion. Their gods, the heroes of their myths, are more often personifications of the powers and phenomena of nature, and their religious ceremonies are more elaborate, and their cult societies are highly organized. As they had begun to domesticate animals and to cultivate the soil, so as to obtain a part of their subsistence by agriculture, they had almost accomplished the ascent from savagery


WALPI DANCE ROCK.


CLIFFS AND TERRACES.

to barbarism when first discovered by the invading European. All the Indians of North America were in this state of transition, but the pueblo tribes had more nearly reached the higher goal.

The great number of ruins found throughout the land has often been interpreted as evidence of a much larger pueblo population than has been found in post-Columbian time. But a careful study of the facts does not warrant this conclusion. It would seem that for various reasons tribes abandoned old pueblos and built new, thus changing their permanent residence from time to time; but more frequent changes were made in their rancherias. These were but ephemeral, being moved from place to place by the varying conditions of water supply. Most of the streams of the arid land are not perennial, but very many of the smaller streams of the pueblo region discharge their waters into the larger streams in times of great flood. Such floods occur now here, now there, and at varying periods, sometimes fifty years apart. When dry years follow one another for a long series, the channels of these intermittent streams are choked with sand until the streams are buried and lost. Under such circumstances the rancherias were moved from dead stream to living stream. In rare instances pueblos themselves were removed for this cause. Other pueblos, and the rancherias generally, were abandoned in time of war; this seems to have been a potent cause for moving. When pestilence attacked a pueblo the people would sometimes leave in a body and never return. The cliff pueblos and dwellings, the cavate dwellings, and the cinder-cone towns were all built and occupied for defensive purposes when powerful enemies threatened. The history of some of the old ruins has been obtained and we know the existing tribes who once occupied them; others still remain enshrouded in obscurity.


A PASSAGEWAY IN WALPI.


THE HURRICANE FAULT.


TOWERS OF THE VERMILION CLIFFS.


TEMPLES AND TOWERS OF THE RIO VIRGEN.


PANORAMA. UPPER VIEW LOOKING EAST, WITH THE GRAND CANYON IN THE DISTANCE. LOWER VIEW LOOKING DOWN THE TOROWEAP.


A PASSAGEWAY IN MASHONGNAVI


TERRACED HOUSES IN ZUÑI.

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