Circumnavigating the White Rim
It's also long, slow, bumpy and monotonous driving, when you're not looking at that scenery, but more on that later.
It's also long, slow, bumpy and monotonous driving, when you're not looking at that scenery, but more on that later.
As I took my morning walk today and watched the canyons fill with sunlight and shadow, it occurred to me: If I ever become deaf, I would move to the desert.
Nor is the desert really silent, actually, though it certainly is in contrast to the rest of the world. So it must especially seem to those that visit the desert briefly in air-conditioned cars to snap a few pictures and then move on. Which is to say almost everyone, including most that move to the rapidly growing cities of the southwest, looking for inexpensive real estate and winter sun, and not for the desert itself.
Summer is the time of storms in the deserts of much of the Southwest, just as it is the time of intense heat. Except for its mountainous areas, the Southwest receives most of its meager precipitation in this way. The weather systems that form the thunderstorms of summer are thus vital to the cycle of desert life, and were they ever to fail, so, too, would most of what lives in these dry regions.
When desert updrafts meet this moist Gulf air, they carry it skyward into cooler altitudes, where the moisture condenses into white, decorative cumulus clouds reminiscent of cauliflowers. If the air is sufficiently moist, the clouds can grow in height, becoming "towering cumulus" clouds. And if the updraft is strong, the air more saturated with moisture, and the differential in temperature between warm updraft and cool upper air sufficiently great, then you have all of the necessary elements to create a cumulonimbus cloud - also known as a potential thunderstorm.
So there was naught to do but rig my ground sheet up as a rough lean-to against a barbed wire fence, and listen to the pit-pit-patter-pit of rain from dusk to midnight as the occasional thunderstorm struck a glancing blow, scattering droplets via gusty winds as it passed in the night, and illuminating the valley floor in sudden bursts of light as it rumbled by.
I'm currently hiking and camping in Nevada and Utah, which explains this off-topic post. I'll continue to cover big news when I'm able to access email, and will also upload and time-phase these entries for posting when I come into town for gas and supplies. To find more of this type of writing based on past trips, look to the folder link at left titled Not Here but There: A Wilderness Journal.
When you think of spectacular Native American ruins, you're likely to first envision the magnificent cliff houses of Mesa Verde, and their cousins in the Four Corners region of the Southwest. But there are less-well known and equally dramatic sites that can be found near the intersection of Utah, Colorado, Arizona and New Mexico, with the grandest to be found in and near Chaco Canyon.
These buildings were constructed at the same time as the cliff houses, but they are more mysterious. While Mesa Verde and the other cliff ruins in canyons throughout the region were clearly once habitations, the purpose(s) of the "Great Houses" of Chaco Canyon is ambiguous. For example, they contain many rooms, like the cliff houses, and the circular kiva chambers as well. But unlike the cliff dwellings, fireplaces and granaries are very few. If they were dwellings, then, where did they cook? And where did they store their food?
Many archaeologists today therefore believe that the Great Houses of Chaco were not full-time dwellings, but rather some sort of cultural centers, acting as gathering places for a more distributed population. This, despite the great size of the buildings, with hundreds of rooms, and their impressive height - some are as tall as five stories. Indeed, the buildings raised by the Chaco culture were among the largest buildings in the world at their time. And like the cliff dwellings, they were all built – and then abandoned - at roughly the same time.
The single dirt track that branches off the road in from the north leads to the Lava Falls trailhead, which zigzags drops precipitously from the edge of the canyon, and drops rapidly down to the river, a half a mile below. The name of the trail derives from what must have been a spectacular event of only a few thousand years ago, when a lava flow cascaded in a flood of fire over the brink, presumably damning the Colorado far below in a cloud of steam. Over time, the force of the backed up river would have worn the dam away, or perhaps more cataclysmically torn it apart.
When I had stowed my gear, I drove north to St. George, the first town lying across the Utah border, to gas up before heading south again. St. George is exploding with growth, and seems like nothing so much as a piece of southwestern Florida somehow transported by night into the middle of the desert, there to open its eyes with surprise, blinking, in the bright sun of the new day. The town is sourrounded by new construction, and each upscale, impeccably landscaped development is graced by its own substantial brick Church of Latter Day Saints house of worship, complete with tall white steeple.
Across the valley in the older part of town you can't help noticing a much grander temple, the oldest LDS church in Utah. Brigham Young broke ground for it himself in 1871, and even today it rises high above everything that surrounds it, commanding the valley. The swampy ground upon which it was built was supposedly "packed with volcanic rock using a cannon — first employed by Napoleon during the French Revolution — as a pile driver. The temple itself was constructed using timbers hauled by oxcart from the ramparts of Mount Trumbull, 80 long miles to the southwest, along a dirt track I drove a few hours later.
The emptiness of the Arizona Strip is also due to the fact that it is almost exclusively public land in all of the popular western flavors (National Park, National Monument, State Park, and the balance under the supervision of the Bureau of Land Management). At its greatest extent, the Strip is 150 miles wide, and almost as many again from north to south, and nowhere in that vast expanse can you find a single paved road. No paved roads, and no towns, gas stations or even running water, either – but a great deal of quietly (and often spectacularly) beautiful country can be enjoyed wherever you go.
It had been six long weeks since I returned from a backcountry trip to Utah, and six exhausting weeks at that. Thoroughly drained, it was high time to leave my demons behind (or try to), and seek comfort in the clean fall air of the White Mountains of New Hampshire.
Saturday morning found me not on a trail that would lead to the dramatic viewpoints popular at peak-foliage time, but instead on one that would thread the valleys between the peaks, meander past beaver ponds, and eventually bring me back to my point of departure, suitably (I hoped) refreshed.
The landscape I explored all that day proved to be unexpectedly spectral, haunted by the shadows of countless thousands of dead birches that loomed above a maturing understory of hemlock, spruce and maple. The explanation for their presence was not hard to guess: birch is a "pioneer" species with small, easily wind-borne seeds that sprout into seedlings that not only tolerate, but demand bright sunlight to survive. Throughout the west, aspens are the opportunists that retake the clearings. But in these northeastern woods, it is birch that is most likely to colonize areas burned by fire, or (like this) clearcut by man.
But birch is not a long-lived tree. The thousands of pioneers that together sprouted on these mountainsides a century ago had now together died, their reforesting mission accomplished. In the years that followed, their twigs rotted and dropped, and then their larger branches. Now, like hapless lepers, they raised only blunted limbs to the sky.