CHAPTER XIV. The Canyon--Above And Below

The Canyon Rim. There are several rather remarkable and surprising points

of difference between the Canyon on the rim, and the Canyon in its depths.

Above, the whole Canyon region, save during the rainy season, is waterless,

and while not barren, owing to the growths made possible by winters' snows

and summers' rains, it is a veritable desert as far as water, whether in

streams, creeks, rivulets or springs, is concerned.

Drainage of the Canyon. On both sides of the Canyon, all the surface water

of the rains drains away from the Canyon for miles, and not until it has

flowed, perhaps from within a few feet of the edge of the abyss itself,

from twenty to a hundred miles, does it empty into the drainage channels

which, burrowing down into the earth, reconvey the water back, by

circuitous routes, into the depths of the Canyon, there to add to the flow

of the Colorado.

Rain at El Tovar. Take rain that falls, for instance, at El Tovar itself,

within sight of the Canyon. After a heavy storm, the visitor may see it

dashing down the Bright Angel Wash (up which the railway runs) to Bass

Station, where it turns and enters the narrower section of the Wash. It

flows in a general southwesterly direction, and enters the Coconino Wash,

which discharges into the open plain, once the bed of the great inland

Eocene Sea. Here it disappears.

An Underground Stream. In this plain are some breaks in the rocky bed,

which allow the water to flow down to join the underground current of the

Havasu (or Cataract) Creek, which runs on the northern slope of Bill

Williams Mountain. This underground stream (as explained in the chapter on

Havasu Canyon) emerges at the head of the village of the Havasupai Indians,

in a thousand springs, and then flows on, over several precipices, to the

lower levels, thus making the exquisite waterfalls that have rendered this

Canyon world-famous. It finally reaches the Colorado some fifteen miles

away, where its clear blue waters are soon lost in the muddy flood of the

"Red."

Water in the Canyon. After one has ridden in the hot summer sun over this

waterless region, and seen the waterwagons of the miners and sheep men, and

the great train of water-tanks being hauled for the guests at El Tovar, it

is a surprise and a wonder to find below, in the heart of this rocky-walled

Canyon, a mighty river dashing its headlong way to the west. Many a time,

after a week of riding horseback on the plateau above, until every particle

of moisture seemed to have evaporated from my body, have I gone down the

trail to the river and camped there, enjoying a swim several times a day,

and rowing up and down one of the quiet stretches, between the rapids,

where boating is not only possible but reasonably safe. In the Bright Angel

and the Shinumo on the north side, and the Havasu on the south side, one

may swim, or at least soak and paddle, in cooling waters, where waving

willows, giant sycamores, and green cottonwoods sway above the streams, and

rich verdure of great variety lines their banks. What a wonderful

contrast,--above and below!

Difference between the Rim and the River. Another remarkable difference, or

surprise, is found when one leaves the rim above, where the weather is

lovely and there is not a sign of rain, and go below to the river, which

gives evidence of a great rise. How can the river rise without rain? Yet it

seems to, and one almost doubts the evidence of his own senses.

Experience on the River. Engineer Stanton tells of an experience as his

party went through the river: "About 2:30 P. M. we heard a deep, loud

roar, and saw the breakers ahead in white foam. With a great effort we

stopped upon a pile of broken rock that had rolled into the river. When we

went ahead to look, much to our surprise, the whole terrible rapid that we

had expected to see had disappeared, and there was only a rushing current

in its stead. While we stood wondering, there rose right at our feet those

same great waves, twelve to fifteen feet in height and from one hundred to

one hundred and fifty feet long across the river, rolling down stream like

great sea waves, and breaking in white foam with terrible noise. We watched

and wondered and at last concluded that this was the forefront of a vast

body of water rolling down this narrow trough from some great cloud-burst

above. (We learned afterwards that there had been such a cloud-burst on the

head-waters of the Little Colorado.) Believing that discretion was the

better part of valor, we camped right there on that pile of rocks, fearing

that, although our boats would ride the waves in safety, we might be caught

in one of these rolls just at the head of a rapid, and, unable to stop, be

carried over the rapid with the additional force of the rushing breakers."

High and Low Water. The piles of driftwood found on the rocks in the Canyon

reveal a difference of upwards of two hundred feet between high and low

water. This, however, does not refer to the general condition of high

water, but to exceptional cases. As, for instance, I myself once saw a mass

of rock, the whole face of the cliff, containing doubtless millions of

tons, fall into the trough of the stream. The whole course was at once

dammed up, and the river rose sixty feet in one hour before the principal

mass of rock was made topheavy by the power of the flood. Then it rolled

over with the force of the millions of tons of water behind it, and

crumbled as it rolled. The mighty wave dashed on, carrying everything

before it. In less than another hour the rock mass had disappeared, and the

water had resumed its normal level. A rise of fifty to seventy feet is not

so very unusual in the heart of the gorge, where it is narrow and the

waters would necessarily pile up. To see such a rise, without any evidence

of a rain above, is a wonderful experience that one occasionally enjoys.

Snow on the Rim. Another remarkable contrast is observed by winter

tourists. On the rim at El Tovar, Grand View, or Bass Camp snow may fall

during December, January and February, and sometimes in March, though it

quickly disappears. This is not surprising when one considers the high

altitudes. The weather is then sometimes quite frigid, but it is a dry cold

which rapidly yields to the warm midday sun. Do not imagine from this

general statement that winter, as we know it in the East, is the usual

thing at the Canyon. Quite the reverse. There are more sunshiny, warm,

windless, stormless and no-snow days than otherwise, taking one year with

another. Real winter weather often stays away until well into January. Some

years it is a negligible quantity. At no time need it be feared by the

traveller.

Trails in Winter. The trails for half a mile, or even a mile, down into the

Canyon, during a part of the winter, are sometimes covered with light snow.

As soon as the snow line is passed, the climate begins to change. The cold

is less penetrating, and by and by one enters what might be called a

temperate zone. Warmer and more comfortable it becomes, until, on reaching

the river, the word "delicious" alone conveys the rich sense of

satisfaction that one feels all over the body in the delightful sensation

experienced. No time is so agreeable for a long stay in the depths of the

Canyon as in the heart of winter. A semi-tropical climate below, while

above, within three hours easy ride, a snowy winter may be reigning

supreme!

Winter in the Canyon. Robert Brewster Stanton, who made his successful trip

through the Canyon in wintertime, comments on this as follows: "It has been

the fortune of but few to travel along the bottom of the great chasm for a

whole winter, while around you bloom the sweet flowers, and southern birds

sing on almost every bush, and at the same time far above, among the upper

cliffs, rage and roar, like demons in the air, the grandest and most

terrific storms of wind and snow and sleet that I have ever witnessed, even

above the clouds among the summit peaks of the Rocky Mountains."

Change in the Flora. This climatic diversity above and below is noticeable

all through the year to the man or woman of sharp eyes, in the difference

of the flowers, the shrubs, and the trees. Above are the pines, the cedars,

and junipers of the cooler climes. The further down one goes, the greater

the change becomes. The pines drop out, then the cedars and junipers, and

when one reaches the patches of growth in the lowest depths, the agave, and

other plants and flowers that we find only in semi-tropical climates here

grow profusely.

Indian Garden. Another difference between the "above" and the "below" is

found in the fact that a garden is almost unknown on the rim, and that

there are many down below. On the Bright Angel Trail is the Indian Garden,

where, for many years, the Havasupais used to cultivate their corn, beans,

onions and melons. Along the Shinumo, on the north side, Mr. Bass has a

garden where all these things grow; where peaches, plums, grapes, and

apricots have thriven abundantly, and where now he is planting figs,

lemons, oranges and grape-fruit. The Havasupais, in the depths of their

Canyon, grow the finest, largest and most tender corn in the world,

peaches and figs galore, and all the ordinary vegetables. Boucher also has

fruit and vegetables on the level near the river, on his trail. At Lee's

Ferry also, Elder Emet has his gardens and orchards, as well as fine

alfalfa fields. Nothing is more delightful than to come, after a hot

journey down the trail, to these unexpected oases in the heart of the

canyons.

Soil on the River and in the Canyon. The soil of the "above," too,

largely differs from the soil of the "below." On the plateaus above, there

are millions of acres, most of which careful examination shows to be

covered with disintegrated rock and comparatively little vegetable soil,

except below the surface. The winds and rains have carried away the softer

and lighter soil, and allowed the heavier and harder rocks to remain. This

process goes on all the time. In the depths of the Canyon, however, except

on the steeper slopes, the soil remains.

The Silence on the Rim. A remarkable contrast between the rim and the

Canyon is sometimes found in the absolute silence above, and the roar of

the river below. It often occurs that not a sound of any kind can be heard

on the rim but one's breathing and the beating of his own heart. One

morning I lay for an hour before I arose, and during the whole of that

time, though I listened again and again, not the slightest sound reached my

ears save the two named.

Song of the River. Now descend to the river and, day or night, early or

late, June or December, hot or cold, wet or dry, fair or stormy, the roar

and rush, fret and fume of the water is never out of one's ears. Even when

asleep it seems to "seep" in through the benumbed senses, and tell of its

never-ending flow. After a few weeks of it, one comes away and finds he

cannot sleep. He misses it and finds himself unable to sleep away from the

accustomed noise.

The Wind. In nothing is the difference of "above" and "below" more

marked than in the wind. Last night on the rim the wind blew almost a gale.

The pines sang loudly, and one could hear their roar for miles. A dozen

times I awoke and listened to their weird music. If you go outdoors, the

wind plays with your hair, and tosses garments to and fro with frolicsome

glee, or even, at times, with apparent angry fury. There are times when the

wind comes toward you, on the rim, with a rapidity and force that are

startling. Every one has had the experience of hearing a military band

approaching from a distance.

As it comes nearer, the sound grows louder and louder, and if it approaches

with great rapidity, as for instance, in an automobile or a speeding

electric car, the music assails the ear with an increasing force that is a

surprise. It is just so with the noises of the wind at the rim of the

Canyon.

Now leave the rim and walk down the trail a couple of rods. All is quiet

and still. The change is startling m its suddenness. The wind may be

blowing far above you, and if you listen, you will hear its effect in the

trees, but here, where you stand, you are protected and sheltered.

Diversity of Color. Perhaps the greatest difference between the rim and the

interior of the Canyon is found in the diversity in color and feature

between them. While there is a fascination to the long, wide stretches of

plateau on the rim, and the forest has its attractive points, there are not

many prominent features (looking away from the Canyon) that would occupy

the attention of travellers. There is little striking in color, in scenery,

in rocky contour. Plains, trees, sky, clouds, sunset,--and nearly all is

said. But immediately one stands on the rim and looks below, all is

changed. Here is feature after feature that compels not only attention but

reverent homage. Color such as is seen nowhere else in the world on such a

grand scale; massive walls that have no counterpart; rock forms that dazzle

and bewilder; and an unfoldment of the stone book of creation that is alike

a joy and a pain, a delight and a sorrow, a something seen at a glance, and

that requires a lifetime to comprehend.

The Grand Canyon of Arizona: How to See It · 第 14 / 32 章