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  At first glance, speeding by car through this valley that is not a valley, one might think there was scarcely any plant life at all. Between oases you will be impressed chiefly by the vast salt beds and the immense alluvial fans of gravel that look as hostile to life as the fabled seas of the moon.

  And yet there is life out there, life of a sparse but varied sort—salt grass and pickleweed on the flats, far-spaced clumps of creosote, saltbush, desert holly, brittlebush, and prickly poppy on the fans. Not much of anything, but a little of each. And in the area as a whole, including the surrounding mountains up to the 11,000-foot summit of Telescope Peak, the botanists count a total of 900 to 1,000 different species, ranging from microscopic forms of algae in the salt pools to limber pine and the ancient bristlecone pine on the peaks.

  But the first impression remains a just one. Despite variety, most of the surface of Death Valley is dead. Dead, dead, deathly—a land of jagged salt pillars, crackling and tortured crusts of mud, sunburnt gravel bars the color of rust, rocks and boulders of metallic blue naked even of lichen. Death Valley is Gravel Gulch.

  TELESCOPE PEAK, OCTOBER 22. To escape the heat for a while, we spend the weekend up in the Panamints. (Summer still baking the world down below, far below, where swirls of mud, salt, and salt-laden streams lie motionless under a lake of heat, glowing in lovely and poisonous shades of auburn, saffron, crimson, sulfurous yellow, dust-tinged tones of white on white.)

  Surely this is the most sterile of North American deserts. No matter how high we climb it seems impossible to leave behind the influence of aridity and anti-life. At 7,000 feet in this latitude we should be entering a forest of yellow pine, with grassy meadows and freshwater brooks. We are farther north than Santa Fe or Flagstaff. Instead there are only the endless barren hills, conventional in form, covered in little but shattered stone. A dull monotonous terrain, duncolored, supporting a few types of shrubs and small, scattered junipers.

  From 7,000 to 9,000 feet we pass through a belt of more junipers and a fair growth of pinyon pines. Along the trail to Telescope Peak—at 10,000 feet—appear thin stands of limber pine and the short, massive, all-enduring bristlecone pine, more ancient than the Book of Genesis. Timberline.

  There is no forest here. And fifty or sixty airline miles to the west stands the reason why—the Sierra Nevada Range blocking off the sea winds and almost all the moisture. We stand in the rain shadow of that still higher wall.

  I walk past three wild burros. Descendants of lost and abandoned prospectors’ stock, they range everywhere in the Panamints, multiplying freely, endangering the survival of the native bighorn sheep by trespassing on the latter’s forage, befouling their springs. But the feral burros have their charm too. They stand about 100 feet from the trail watching me go by. They are quite unafraid, and merely blink their heavy eyelashes like movie starlets when I halt to stare at them. However they are certainly not tame. Advance toward them and they trot off briskly.

  The bray of the donkey is well known. But these little beasts can make another sound even more startling because so unexpected. Hiking up some arid canyon in the Panamints, through what appears to be totally lifeless terrain, you suddenly hear a noise like a huge dry cough behind your shoulder. You spring ten feet forward before daring to look around. And see nothing, nothing at all, until you hear a second cough and scan the hillsides and discover far above a little gray or black burro looking down at you, waiting for you to get the hell out of its territory.

  I stand by the cairn on the summit of Telescope Peak, looking out on a cold, windy, and barren world. Rugged peaks fall off southward into the haze of the Mojave Desert; on the west is Panamint Valley, the Argus Range, more mountains, more valleys, and finally the Sierras, crowned with snow; to the north and northwest the Inyo and White mountains; below lies Death Valley—the chemical desert—and east of it the Black Mountains, the Funeral Mountains, the Amargosa Valley and farther mountains, wave after wave of wrinkled ridges standing up from the oceanic desert sea until vision gives out somewhere beyond the curving rim of the world’s edge. A smudge hangs on the eastern horizon, suggesting the presence of Death Valley’s counterpart and complement, the only city within 100 miles: Las Vegas: Glitter Gulch West.

  ECHO CANYON, NOVEMBER 30. A hard place to love. Impossible? No, there were a few—the prospectors, the single-blanket, jackass prospectors who wandered these funeral wastes for a century dreaming of what? Sudden wealth? Not likely. Not Shorty Borden, for example, who invested eight months of his life in building by hand a nine-mile road to his lead and silver diggings in Hanaupah Canyon. Then discovered that even with a road it would still cost him more to transport his ore to the nearest smelter than the ore itself was worth.

  Echo Canyon. We are deep into the intricacies of the Funeral Mountains. Named not simply for their proximity to Death Valley, but also for shape and coloration: lifeless escarpments of smoldering red bordered in charcoal, the crags and ridges and defiles edged in black and purple. A primeval chaos of faulted, uplifted, warped, and folded dolomites, limestones, fanglomerates of mud, sand, and gravel. Vulcanism as well: vesiculated andesite, walls embellished with elegant mosaics of rose and yellow quartz. Fool’s gold—pyrite—glittering in the black sand, micaceous shales glinting under back light, veins of pegmatite zigzagging and intersecting like an undeciphered script across the face of a cliff: the writing on the wall: “God Was Here.” Shallow caves, holes in the rock, a natural arch, and the canyon floor littered with boulders, deep in coarse gravel.

  Nowhere in Echo Canyon can I find the slightest visible trace of water. Nevertheless it must be present under the surface, at least in intermittent or minute amounts, for here and there stand living things. They look dead but are actually dormant, waiting for the resurrection of the rain. I mean the saltbush, the desert fir, the bladderweed, a sprinkling of cottontop cactus, the isolated creosote bush. Waiting.

  You may see a few lizards. In sandy places are the hoofprints of bighorn sheep, where they’ve passed through on their way from the high parts of the range to the springs near Furnace Creek. Sit quite still in one spot for an hour and you might see a small gray bird fly close to look you over. This is the bird that lives in Echo Canyon.

  The echoes are good. At certain locations, on a still day, one clear shout will create a series of overlapping echoes that goes on and on toward so fine a diminuendo that the human ear cannot perceive the final vibrations.

  Tramp far enough up Echo Canyon and you come to a ghost town, the ruins of a mining camp—one of many in Death Valley. Deep shafts, a tipple, a rolling mill largely intact, several cabins—one with its inside walls papered with pages from the Literary Digest. Half buried in drifted sand is a rusted model-T Ford without roof or motor, a child’s tricycle, a broken shovel.

  Returning through twilight, I descend the narrow gorge between flood-polished walls of bluish andesite—the stem of the wineglass. I walk down the center of an amphitheater of somber cliffs riddled with grottoes, huge eyesockets in a stony skull, where bats hang upside down in the shadows waiting for night.

  Through the opening of the canyon I can see the icy heights of Telescope Peak shining under the cloud-reflected light of one more sunset. Scarlet clouds in a green sky. A weird glow pervades the air through which I walk; it vibrates on the canyon walls, revealing to me all at once a vision of the earth’s slow agony, the convulsive grinding violence of a hundred million years. Of a billion years. I write metaphorically, out of necessity. And yet it seems impossible to believe that these mountains, old as anything on the surface of the planet, do not partake in some dim way of the sentience of living tissue. Genealogies: From these rocks struck once by lightning gushed springs that turned to blood, flesh, life. Impossible miracle. And I am struck once again by the unutterable beauty, terror, and strangeness of everything we think we know.

  FURNACE CREEK, DECEMBER 10. The oasis. We stand near the edge of a grove of date palms looking eastward at the soft melting mud hills above Texa
s Spring. The hills are lemon yellow with dark brown crusts on top, like the frosting on a cake. Beyond the hills rise the elaborate, dark, wine-red mountains. In the foreground, close by, irrigation water plunges into a pool, from which it is diverted into ditches that run between the rows of palms.

  The springs of Furnace Creek supply not only the palms but also the water needs of the hotel, the motel (both with swimming pools), Park Service headquarters and visitor center, an Indian village, and two large campgrounds. I do not know the output of these springs as measured in gallons per minute. But I do know that during the Christmas and Easter holidays there is enough water available to serve the needs of 10,000 people. Where does it come from? From a natural reservoir in the base of the bleak, fatally arid Funeral Mountains. A reservoir that may be joined to the larger underground acquifers beneath the Amargosa and Pahrump valleys to the east.

  This does not mean that the Furnace Creek portion of Death Valley could support a permanent population of 10,000 drinking, back-scrubbing, hard-flushing suburbanites. For the water used here comes from a supply that may have required 20,000 years to charge; it is not sustained by rainfall—not in a country where precipitation averages two inches per year.

  That’s the mistake they made in central Arizona—Tucson and Phoenix—and are now making in Las Vegas and Albuquerque. Out of greed and stupidity, but mostly greed, the gentry of those cities overexpanded their investment in development and kept going by mining the underground water supply. Now that the supply is dwindling, they set up an unholy clamor in Congress to have the rest of the nation save them from the consequences of their own folly. Phoenix might rise again from ashes—but not, I think, from the sea of sand that is its likely destiny.

  There are about 200 springs, all told, within the boundaries of Death Valley National Monument, counting each and every tiny seep that produces any flow at all. None except those in the northeast corner of the park are comparable to the springs at Furnace Creek. In addition to the springs there are the heavily saline, undrinkable waters of Salt Creek, Badwater, and the valley floor itself.

  All this water is found in what meteorologists believe to be the hottest place on earth, year in and year out hotter than the Sahara, the Great Karroo, the Negev, the Atacama, the Rub’-al-Khali (“Empty Quarter”) of Arabia, or the far-out-back-of-beyond in central Australia. The world’s record is held by Libya, where a temperature of 136 degrees Fahrenheit was once recorded at a weather station called Azizia. Death Valley’s high so far is a reading of 134 degrees at Furnace Creek. But Azizia has been unable to come near repeating its record, while temperatures at Furnace Creek consistently exceed the mean maximums for Azizia by ten percent. And Badwater, only twenty miles south of Furnace Creek, is on the average always four degrees hotter. It follows that on the historic day when the thermometer reached 134 at Furnace Creek, it was probably 138 at Badwater. But there was nobody around at Badwater that day (July 10, 1913).

  Official weather readings are made from instruments housed in a louvered wooden box set five feet above the ground. In Death Valley the temperature on the surface of the ground is ordinarily fifty percent higher than in the box five feet above. On a normal summer’s day in Death Valley, with the thermometer reading 120 degrees Fahrenheit, the temperature at ground surface is 180.

  Curiosities: There are fish in the briny pools of Salt Creek, far out on the hottest, bleakest, saltiest part of the valley floor—the inch-long cyprinodon or pupfish. There is a species of soft-bodied snail living in the Epsom salts, Glauber’s salt, and rock salts of Badwater. There are fairy shrimp in the tinajas or natural cisterns of Butte Valley in the southwest corner of the park; estivating beneath the clay most of the year, they wriggle forth to swim, rejoice, and reproduce after that rarest and most wonderful of Death Valley events, a fall of rain.

  More curiosities: Blue herons enter the valley in winter; also trumpeter swans; grebes, coots, and mallards can be seen in the blue ponds of Saratoga Springs; and for a few weeks in the fall of one year (1966) a real flamingo made its home among the reeds that line the shore of the sewage lagoon below Park Village. Where this flamingo came from no one could say; where it went the coyotes most likely could testify. Or perhaps the lion.

  A lean and hungry mountain lion was observed several times that year during the Christmas season investigating the garbage cans in the campgrounds. An old lion, no doubt—aging, possibly ill, probably retired. In short, a tourist. But a lion even so.

  But these are mere oddities. All the instruments agree that Death Valley remains the hottest place on earth, the driest in North America, the lowest in the Western Hemisphere. Of all deathly places the most deadly—and the most beautiful.

  BADWATER, JANUARY 19. Standing among the salt pinnacles of what is called the Devil’s Golf Course, I heard a constant tinkling and crackling noise—the salt crust expanding in the morning sun. No sign of life out there. Experimentally I ventured to walk upon, over, among the pinnacles. Difficult, but not impossible. The formations are knee-high, white within but stained yellow by the dusty winds, studded on top with sharp teeth. Like walking on a jumble of broken and refrozen slabs of ice: At every other step part of the salt collapses under foot and you drop into a hole. The jagged edges cut like knives into the leather of my boots. After a few minutes of this I was glad to return to the security of the road. Even in January the sun felt uncomfortably hot, and I was sweating a little.

  Where the salt flats come closest to the base of the eastern mountains, at 278 feet below sea level, lies the clear and sparkling pool known as Badwater. A shallow body of water, surrounded by beds of snow-white alkali. According to Death Valley legend the water is poisonous, containing traces of arsenic. I scooped up a handful and sampled it in my mouth, since the testing of desert waterholes has always been one of my chores. I found Badwater lukewarm, salty on the tongue, sickening. I spat it out and rinsed my mouth with fresh water from my canteen.

  From here, the lowest point in all the Americas, I gazed across the pale lenses of the valley floor to the brown outwash fan of Hanaupah Canyon opposite, ten miles away, and from the canyon’s mouth up and up and up to the crest of Telescope Peak with its cornices of frozen snow 11,049 feet above sea level. One would like to climb or descend that interval someday, the better to comprehend what it means. Whatever it means.

  I have been part of the way already, hiking far into Hanaupah Canyon to Shorty Borden’s abandoned camp, up to that loveliest of desert graces, a spring-fed stream. Lively, bubbling, with pools big enough and cold enough, it seemed then, for trout. But there are none. Along the stream grow tangles of wild grapevine and willow; the spring is choked with watercress. The stream runs for less than a mile before disappearing into the sand and gravel of the wash. Beyond the spring, up-canyon, all is dry as death again until you reach the place where the canyon forks. Explore either fork and you find water once more—on the right a little waterfall, on the left in a grottolike glen cascades sliding down through chutes in the dark blue andesite. Moss, ferns, and flowers cling to the damp walls—the only life in this arid wilderness. Almost no one ever goes there. It is necessary to walk for many miles.

  DEVIL’S HOLE, FEBRUARY 10. A natural opening in the desert floor; a queer deep rocky sinkhole with a pond of dark green water at the bottom. That pond, however, is of the kind called bottomless; it leads down and down through greener darker depths into underwater caverns whose dimensions and limits are not known. It might be an entrance to the subterranean lakes that supposedly lie beneath the Funeral Mountains and the Amargosa Valley.

  The Park Service has erected a high steel fence with locked gate around the hole. Not to keep out tourists, who only want to look, but to keep out the aqualung adventurers who wish to dive in and go all the way down. Within the past year several parties of scuba divers have climbed over and under the fence anyway and gone exploring down in that sunless sea. One party returned to the surface one man short. His body has not been found yet, though many have
searched. If supposition is correct, the missing man may be found someday wedged in one of the outlets of Furnace Creek springs.

  Death Valley has taken five lives this year—one by water, two by ice, and two by fire. A hiker slipped on the glazed snow of the trail to Telescope Peak and tumbled 1,000 feet down a steep pitch of ice and rock. His companion went for help; a member of a professional mountaineering team, climbing down to recover the victim, also fell and was also killed.

  Last summer two young soldiers from the Army’s nearby Camp Irwin went exploring in the desert off the southwest corner of Death Valley. Their jeep ran out of gas, they tried to walk home to the base. One was found beside the seldom-traveled desert road, dead from exhaustion and dehydration. The body of the other could not be found, though 2,000 soldiers hunted him for a week. No doubt he wandered off the trail into the hills seeking water. Absent without leave. He could possibly be still alive. Maybe in a forgotten cabin up in the Panamints eating lizards, waiting for some war to end.

  Ah to be a buzzard now that spring is here.

  THE SAND DUNES, MARCH 15. At night I hear tree toads singing in the tamarisk along the water channels of Furnace Creek Ranch. The days are often windy now, much warmer, and rain squalls sail north through the valley, obscuring both sky and sun. The ground squirrels scamper from hole to hole in the mud hills, the Gambel’s quail swoop in flocks low over the ground, alight, and run in unison through the brush, calling to one another. Tawny coyotes stand bold as brass close to the road in broad daylight and watch the tourists drive by. And the mesquite thickets, black and lifeless-looking since last fall, have assumed a delicate tinge of spring green.

  Death Valley’s winter, much too lovely to last, is nearly over.

  Between winds and storms I walk far out on the dunes. How hot and implacably hostile this sea of sand appeared last June when we saw it for the first time. Then it seemed to be floating in heat waves, which gathered among the dunes and glistened like pools of water, reflecting the sky.