CHAPTER III

THE BOTTOM OF THE BOWL

[Sidenote: Early geological days.]

[Sidenote: The former Gulf.]

In the ancient days when the shore of the Pacific was young, when the

white sierras had only recently been heaved upward and the desert

itself was in a formative stage, the ocean reached much farther inland

than at the present time. It pushed through many a pass and flooded

many a depression in the sands, as its wave-marks upon granite bases

and its numerous beaches still bear witness. In those days that portion

of the Colorado Desert known as the Salton Basin did not exist. The

Gulf of California extended as far north as the San Bernardino Range

and as far west as the Pass of San Gorgonio. Its waters stood deep

where now lies the road-bed of the Southern Pacific railway, and all

the country from Indio almost to the Colorado River was a blue sea. The

Bowl was full. No one knew if it had a bottom or imagined that it would

ever be emptied of water and given over to the drifting sands.

[Sidenote: Sea-beaches on desert.]

[Sidenote: Harbors and reefs.]

No doubt the tenure of the sea in this Salton Basin was of long

duration. The sand-dunes still standing along the northern shore--fifty

feet high and shining like hills of chalk--were not made in a month;

nor was the long shelving beach beneath them--still covered with

sea-shells and pebbles and looking as though washed by the waves only

yesterday--formed in a day. Both dunes and beach are plainly visible

winding across the desert for many miles. The southwestern shore,

stretching under a spur of the Coast Range, shows the same formation in

its beach-line. The old bays and lagoons that led inland from the sea,

the river-beds that brought down the surface waters from the mountains,

the inlets and natural harbors are all in place. Some of them are

drifted half full of sand, but they have not lost their identity. And

out in the sea-bed still stand masses of cellular rock, honeycombed and

water-worn (and now for many years wind-worn), showing the places where

once rose the reefs of the ancient sea.

[Sidenote: Indian remains.]

[Sidenote: The Cocopas.]

These are the only records that tell of the sea’s occupation. The

Indians have no tradition about it. Yet when the sea was there the

Indian tribes were there also. Along the bases of the San Bernardino

and San Jacinto Ranges there are indications of cave-dwelling,

rock-built squares that doubtless were fortified camps, heaps of stone

that might have been burial-mounds. Everywhere along the ancient shores

and beaches you pick up pieces of pottery, broken ollas, stone pestels

and mortars, axe-heads, obsidian arrow-heads, flint spear-points, agate

beads. There is not the slightest doubt that the shores were inhabited.

It was a warm nook, accessible to the mountains and the Pacific; in

fact, just the place where tribes would naturally gather. Branches of

the Yuma Indians, like the Cocopas, overran all this country when the

Padres first crossed the desert; and it was probably their forefathers

who lived by the shores of this Upper Gulf. No doubt they were

fishermen, traders and fighters, like their modern representatives on

Tiburon Island; and no doubt they fished and fought and were happy by

the shores of the mountain-locked sea.

[Sidenote: The Colorado River.]

[Sidenote: The delta dam.]

But there came a time when there was a disturbance of the existing

conditions in the Upper Gulf. Century after century the Colorado River

had been carrying down to the sea its burden of sedimental sand and

silt. It had been entering the Gulf far down on the eastern side at

an acute angle. Gradually its deposits had been building up, banking

up; and gradually the river had been pushing them out and across the

Gulf in a southwesterly direction. Finally there was formed a delta

dam stretching from shore to shore. The tides no longer brought water

up and around the bases of the big mountains. Communication with the

sea was cut off and what was once the top of the Gulf changed into an

inland lake. It now had no water supply from below, it lay under a

burning sun, and day by day evaporation carried it away.

[Sidenote: The inland lake.]

No one knows how many days, how many years, elapsed before the

decrease of the water became noticeable. Doubtless the lake shrunk

away slowly from the white face of the sand-dunes and the red walls

of the mountains. The river-mouths that opened into the lake narrowed

themselves to small stream-beds. The shelving beaches where the waves

had fallen lazily year after year, pushing themselves over the sand in

beautiful water-mirrors, shone bare and dry in the sunlight. The ragged

reefs, over which the chop sea had tumbled and tossed so long, lifted

their black hulks out of the water and with their hosts of barnacles

and sea-life became a part of the land.

[Sidenote: The first fall.]

[Sidenote: Springs and wells in the sea-bed.]

[Sidenote: The New River.]

The waters of the great inland lake fell perhaps a hundred feet and

then they made a pause. The exposed shores dried out. They baked hard

in the sun, and were slowly ground down to sand and powdered silt

by the action of the winds. The waters made a long pause. They were

receiving reinforcements from some source. Possibly there was more

rainfall in those days than now, and the streams entering the lake from

the mountains were much larger. Again there may have been underground

springs. There are flowing wells to-day in this old sea-bed--wells

that cast up water salter than the sea itself. No one knows their

fountain-head. Perhaps by underground channels the water creeps through

from the Gulf, or comes from mountain reservoirs and turns saline by

passing through beds of salt. These are the might-bes; but it is far

more probable that the Colorado River at high water had made a breach

of some kind in the dam of its own construction and had poured overflow

water into the lake by way of a dry channel called the New River. The

bed of this river runs northward from below the boundary-line of Lower

California; and in 1893, during a rise in the Colorado, the waters

rushed in and flooded the whole of what is called the Salton Basin.

When the Colorado receded, the basin soon dried out again.

[Sidenote: New beaches.]

It was undoubtedly some accident of this kind that called the halt in

the original recession. During the interim the lake had time to form

new shores where the waves pounded and washed on the gravel as before

until miles upon miles of new beach--pebbled, shelled, and sloping

downward with great uniformity--came into existence. This secondary

beach is intact to-day and looks precisely like the primary except

that it is not quite so large. Across the basin, along the southern

mountains, the second water-tracery is almost as apparent as the first.

The rocks are eaten in long lines by wave-action, and are honeycombed

by the ceaseless energies of the zoöphite.

[Sidenote: The second fall.]

Nor was the change in beach and rock alone. New bays and harbors were

cut out from where the sea had been, new river-channels were opened

down to the shrunken lake, new lagoons were spread over the flat

places. Nature evidently made a great effort to repair the damage

and adapt the lake to its new conditions. And the Indians, too,

accepted the change. There are many indications in broken pottery,

arrow-heads, and mortars that the aboriginal tribes moved down to the

new beach and built wickiups by the diminished waters. And the old

fishing-foraging-fighting life was probably resumed.

[Sidenote: The third beach.]

[Sidenote: The failing water.]

Then once more the waters went down, down, down. Step by step they

receded until the secondary beach was left a hundred feet above the

water level. Again there was a pause. Again new beaches were beaten

into shape by the waves, new bays were opened, new arroyos cut through

from above. The whole process of shore-making--the fitting of the land

to the shrunken proportions of the lake--was gone through with for

the third time; while the water supply from the river or elsewhere

was maintained in decreased volume but with some steadiness of flow.

Possibly the third halt of the receding water was not for a great

length of time. The tertiary beach is not so large as its predecessors.

There never was any strong wave-action upon it, its pebbles are few,

its faults and breaks are many. The water supply was failing, and

finally it ceased altogether.

[Sidenote: Evaporation.]

What fate for a lake in the desert receiving no supplies from river

or sea--what fate save annihilation? The hot breath of the wind blew

across the cramped water and whipped its surface into little waves;

and as each tiny point of spray rose on the crest and was lifted into

the air the fiery sunbeam caught it, and in a twinkling had evaporated

and carried it upward. Day by day this process went on over the whole

surface until there was no more sea. The hollow reefs rose high and

dark above the bed, the flat shoals of silt lifted out of the ooze,

and down in the lowest pools there was the rush and plunge of monster

tortuabas, sharks and porpoises, caught as it were in a net and vainly

struggling to get out. How strange must have seemed that landscape

when the low ridges were shining with the slime of the sea, when the

beds were strewn with _algæ_, sponges, and coral, and the shores were

whitening with salt! How strange, indeed, must have been the first

sight of the Bottom of the Bowl!

[Sidenote: Bottom of the Bowl.]

[Sidenote: Drying out of the sea-bed.]

[Sidenote: Advance of desert.]

But the sun never relaxed its fierce heat nor the wind its hot breath.

They scorched and burned the silt of the sea-bed until it baked and

cracked into blocks. Then began the wear of the winds upon the broken

edges until the blocks were reduced to dry fine powder. Finally the

desert came in. Drifts upon drifts of sand blown through the valleys

settled in the empty basin; gravel and bowlder-wash came down from

the mountains; the grease wood, the salt-bush, and the so-called

pepper-grass sprang up in isolated spots. Slowly the desert fastened

itself upon the basin. Its heat became too intense to allow the falling

rain to reach the earth, its surface was too salt and alkaline to allow

of much vegetation, it could support neither animal nor bird life; it

became more deserted than the desert itself.

[Sidenote: Below sea-level.]

[Sidenote: Desolation of the basin.]

And thus it remains to this day. When you are in the bottom of it you

are nearly three hundred feet below the level of the sea. Circling

about you to the north, south, and west are sierras, some of them

over ten thousand feet in height. These form the Rim of the Bowl. And

off to the southwest there is a side broken out of the Bowl through

which you can pass to the river and the Gulf. The basin is perhaps the

hottest place to be found anywhere on the American deserts. And it is

also the most forsaken. The bottom itself is, for the great part of

it, as flat as a table. It looks like a great plain leading up and

out to the horizon--a plain that has been ploughed and rolled smooth.

The soil is drifted silt--the deposits made by the washings from the

mountains--and is almost as fine as flour.

[Sidenote: Beauty of the sand-dunes.]

The long line of dunes at the north are just as desolate, yet they are

wonderfully beautiful. The desert sand is finer than snow, and its

curves and arches, as it builds its succession of drifts out and over

an arroyo, are as graceful as the lines of running water. The dunes are

always rhythmical and flowing in their forms; and for color the desert

has nothing that surpasses them. In the early morning, before the sun

is up, they are air-blue, reflecting the sky overhead; at noon they

are pale lines of dazzling orange-colored light, waving and undulating

in the heated air; at sunset they are often flooded with a rose or

mauve color; under a blue moonlight they shine white as icebergs in the

northern seas.

[Sidenote: Cactus and salt-bush.]

But neither the dunes nor the flats grow vegetation of consequence.

About the high edges, up near the mountain slopes, you find growths

of mesquite, palo verde, and cactus; but down in the basin there are

many miles where no weed or grass breaks the level uniformity. Not

even the salt-bush will grow in some of the areas. And this is not due

to poverty of soil but to absence of water and intense heat. Plants

cannot live by sunlight alone.

[Sidenote: Desert animals in the basin.]

[Sidenote: Birds.]

[Sidenote: Lizards and snakes.]

Nor will the desert animals inhabit an absolute waste. The coyote and

the wild-cat do not relish life in this dip in the earth. They care

little for heat and drouth, but the question of food appeals to them.

There is nothing to eat. Even the abstemious jack-rabbit finds living

here something of a difficulty. Many kinds of tracks are found in the

uncrusted silt--tracks of coyotes, gray wolves, sometimes mountain

lions--but they all run in straight trails, showing the animals to be

crossing the basin to the mountains, not prowling or hunting. So, too,

you will occasionally find birds--linnets, bobolinks, mocking-birds,

larks--but they are seen one at a time, and they look weary--like land

birds far out at sea that seek a resting-place on passing vessels. They

do not belong to the desert and are only stopping there temporarily on

some long flight. Snakes and lizards are not particular about their

abiding-place, and yet they do not care to live in a land where there

is no bush or stone to creep under. You meet with them very seldom.

Practically there is no life of any kind that is native to the place.

[Sidenote: Mirage.]

[Sidenote: The water illusion.]

Is there any beauty, other than the dunes, down in this hollow of the

desert? Yes. From a picturesque point of view it has the most wonderful

light, air, and color imaginable. You will not think so until you

see them blended in that strange illusion known as mirage. And here

is the one place in all the world where the water-mirage appears to

perfection. It does not show well over grassy or bushy ground, but over

the flat lake-beds of the desert its appearance is astonishing. Down in

the basin it is accompanied by a second illusion that makes the first

more convincing. You are below sea-level, but instead of the ground

about you sloping up and out, it apparently slopes down and away on

every side. You are in the centre of a disk or high point of ground,

and around the circumference of the disk is water--palpable, almost

tangible, water. It cannot be seen well from your horse, and fifty feet

up on a mountain side it would not be visible at all. But dismount and

you see it better; kneel down and place your cheek to the ground and

now the water seems to creep up to you. You could throw a stone into

it. The shore where the waves lap is just before you. But where is the

horizon-line? Odd enough, this vast circling sea does not always know

a horizon; it sometimes reaches up and blends into the sky without any

point of demarcation. Through the heated air you see faint outlines of

mountains, dim glimpses of foot-hills, suggestions of distance; but no

more. Across them is drawn the wavering veil of air, and the red earth

at your feet, the blue sky overhead, are but bordering bands of flat

color.

[Sidenote: Decorative landscapes.]

[Sidenote: Sensuous qualities in nature.]

And there you have the most decorative landscape in the world, a

landscape all color, a dream landscape. Painters for years have been

trying to put it upon canvas--this landscape of color, light, and air,

with form almost obliterated, merely suggested, given only as a hint of

the mysterious. Men like Corot and Monet have told us, again and again,

that in painting, clearly delineated forms of mountains, valleys,

trees, and rivers, kill the fine color-sentiment of the picture. The

great struggle of the modern landscapist is to get on with the least

possible form and to suggest everything by tones of color, shades

of light, drifts of air. Why? Because these are the most sensuous

qualities in nature and in art. The landscape that is the simplest in

form and the finest in color is by all odds the most beautiful. It is

owing to just these features that this Bowl of the desert is a thing

of beauty instead of a dreary hollow in the hills. Only one other

scene is comparable to it, and that the southern seas at sunset when

the calm ocean reflects and melts into the color-glory of the sky. It

is the same kind of beauty. Form is almost blurred out in favor of

color and air.

[Sidenote: Changing the desert.]

[Sidenote: Irrigation in the basin.]

Yet here is more beauty destined to destruction. It might be thought

that this forsaken pot-hole in the ground would never come under the

dominion of man, that its very worthlessness would be its safeguard

against civilization, that none would want it, and everyone from

necessity would let it alone. But not even the spot deserted by

reptiles shall escape the industry or the avarice (as you please) of

man. A great company has been formed to turn the Colorado River into

the sands, to reclaim this desert basin, and make it blossom as the

rose. The water is to be brought down to the basin by the old channel

of the New River. Once in reservoirs it is to be distributed over the

tract by irrigating ditches, and it is said a million acres of desert

will thus be made arable, fitted for homesteads, ready for the settler

who never remains settled.

[Sidenote: Changing the climate.]

[Sidenote: Dry air.]

A most laudable enterprise, people will say. Yes; commercially no one

can find fault with it. Money made from sand is likely to be clean

money, at any rate. And economically these acres will produce large

supplies of food. That is commendable, too, even if those for whom it

is produced waste a good half of what they already possess. And yet the

food that is produced there may prove expensive to people other than

the producers. This old sea-bed is, for its area, probably the greatest

dry-heat generator in the world because of its depression and its

barren, sandy surface. It is a furnace that whirls heat up and out of

the Bowl, over the peaks of the Coast Range into Southern California,

and eastward across the plains to Arizona and Sonora. In what measure

it is responsible for the general climate of those States cannot

be accurately summarized; but it certainly has a great influence,

especially in the matter of producing dry air. To turn this desert into

an agricultural tract would be to increase humidity, and that would be

practically to nullify the finest air on the continent.

[Sidenote: Value of the air supply.]

And why are not good air and climate as essential to human well-being

as good beef and good bread? Just now, when it is a world too late,

our Government and the forestry societies of the country are awakening

to the necessity of preserving the forests. National parks are being

created wherever possible and the cutting of timber within them is

prohibited. Why is this being done? Ostensibly to preserve the trees,

but in reality to preserve the water supply, to keep the fountain-heads

pure, to maintain a uniform stage of water in the rivers. Very proper

and right. The only pity is that it was not undertaken forty years ago.

But how is the water supply, from an economic and hygienic stand-point,

any more important than the air supply?

[Sidenote: Value of the deserts.]

Grasses, trees, shrubs, growing grain, they, too, may need good air as

well as human lungs. The deserts are not worthless wastes. You cannot

crop all creation with wheat and alfalfa. Some sections must lie fallow

that other sections may produce. Who shall say that the preternatural

productiveness of California is not due to the warm air of its

surrounding deserts? Does anyone doubt that the healthfulness of the

countries lying west of the Mississippi may be traced directly to the

dry air and heat of the deserts. They furnish health to the human; why

not strength to the plant? The deserts should never be reclaimed. They

are the breathing-spaces of the west and should be preserved forever.

[Sidenote: Destruction of natural beauty.]

[Sidenote: Effects of mining, lumbering, agriculture.]

[Sidenote: Ploughing the prairies.]

[Sidenote: “Practical men”]

To speak about sparing anything because it is beautiful is to waste

one’s breath and incur ridicule in the bargain. The æsthetic sense--the

power to enjoy through the eye, the ear, and the imagination--is just

as important a factor in the scheme of human happiness as the corporeal

sense of eating and drinking; but there has never been a time when the

world would admit it. The “practical men,” who seem forever on the

throne, know very well that beauty is only meant for lovers and young

persons--stuff to suckle fools withal. The main affair of life is to

get the dollar, and if there is any money in cutting the throat of

Beauty, why, by all means, cut her throat. That is what the “practical

men” have been doing ever since the world began. It is not necessary

to dig up ancient history; for have we not seen, here in California

and Oregon, in our own time, the destruction of the fairest valleys

the sun ever shone upon by placer and hydraulic mining? Have we not

seen in Minnesota and Wisconsin the mightiest forests that ever raised

head to the sky slashed to pieces by the axe and turned into a waste of

tree-stumps and fallen timber? Have we not seen the Upper Mississippi,

by the destruction of the forests, changed from a broad, majestic

river into a shallow, muddy stream; and the beautiful prairies of

Dakota turned under by the plough and then allowed to run to weeds? Men

must have coal though they ruin the valleys and blacken the streams of

Pennsylvania, they must have oil though they disfigure half of Ohio

and Indiana, they must have copper if they wreck all the mountains of

Montana and Arizona, and they must have gold though they blow Alaska

into the Behring Sea. It is more than possible that the “practical

men” have gained much practice and many dollars by flaying the fair

face of these United States. They have stripped the land of its robes

of beauty, and what have they given in its place? Weeds, wire fences,

oil-derricks, board shanties and board towns--things that not even a

“practical man” can do less than curse at.

[Sidenote: Fighting wind, sand, and heat.]

[Sidenote: Nature eternal.]

[Sidenote: Return of desolation.]

And at last they have turned to the desert! It remains to be seen what

they will do with it. Reclaiming a waste may not be so easy as breaking

a prairie or cutting down a forest. And Nature will not always be

driven from her purpose. Wind, sand, and heat on Sahara have proven

hard forces to fight against; they may prove no less potent on the

Colorado. And sooner or later Nature will surely come to her own again.

Nothing human is of long duration. Men and their deeds are obliterated,

the race itself fades; but Nature goes calmly on with her projects. She

works not for man’s enjoyment, but for her own satisfaction and her own

glory. She made the fat lands of the earth with all their fruits and

flowers and foliage; and with no less care she made the desert with its

sands and cacti. She intended that each should remain as she made it.

When the locust swarm has passed, the flowers and grasses will return

to the valley; when man is gone, the sand and the heat will come back

to the desert. The desolation of the kingdom will live again, and down

in the Bottom of the Bowl the opalescent mirage will waver skyward on

wings of light, serene in its solitude, though no human eye sees nor

human tongue speaks its loveliness.

The desert · 第 3 / 12 章