Temple of Giants

IMG_4651.JPGYosemite Valley is full of superlatives – the world’s largest exposed granite monolith, some of its highest cliffs, the continent’s tallest series of waterfalls – but these remarkable things are only there because of what isn’t. Billions (if not trillions) of tons of the valley’s granite were ground away more than 1 million years ago. A river started the job before glaciers took over, scouring off Half Dome’s other half, carving El Capitan’s 3,000-foot heights and leaving cliffs tall enough to scrape the clouds. Granite’s a tough rock, and this specific granite is as ancient as the dinosaurs. But sculpting it into some of the biggest and most recognizable formations on the planet took the strength of water.

Yosemite National Park now is defined more by rivers of liquid water rather than frozen, with spring snowmelt tumbling down falls that fill every valley with mist and sound. Some are huge and iconic – Bridalveil Fall accents the image of Yosemite Valley every visitor sees, and Yosemite Falls drops almost half a mile altogether. Countless smaller falls are tucked away in hidden corners of the valley, glistening threads running down distant ravines or vanishing into vapor high above the valley floor.

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IMG_4593.JPGOur first taste of Yosemite Valley’s scale was the football-field-size cliff that breaks through the forest across the valley near its entrance, streaked black from lichen and water. Tiny cars drove along the road at its base. On our side of the valley, another smooth granite outcropping sloped toward the floor at a gentle angle. Still, standing on it, seeing the earth drop away and looking out over a valley thousands of feet across was enough to get my heart pumping. The feeling didn’t go away during my four-day stay in one of our first national parks.  “No temple made with hands can compare with Yosemite,” famed naturalist John Muir wrote a century ago. “Every rock in its wall seems to glow with life.”

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IMG_4638.JPGBefore seeing what Muir meant, we had to actually get there, with a stop in Arizona to pick up my mom. That meant a whole lot of driving, passing through Roswell (and stopping at the International UFO Museum, obviously), across the Rockies and a dust-blown desert in bloom, and between stands of wind turbines that often stretched to the horizon. In California’s Central Valley the turbine groves were replaced with miles upon miles of tree orchards and vineyards. Occasionally a semi drove past hauling trailers filled to the brim with garlic or oranges.

Then it was back up the mountains to Yosemite’s Wawona Campground.

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IMG_4929.JPGMore than 4 million people pile into Yosemite every year, and nearly all of them head to Yosemite Valley, which stretches across a paltry 1 percent of the park’s 1,200 square miles. I couldn’t blame them. I also couldn’t wait to see parts of the park many of them don’t visit. Wawona, which sits 30 winding miles south of the valley and was home base for four days, was the first of three non-valley stops.

We were mostly alone when we hiked partway up the nearby Chilnualna Falls trail one morning. The steep and rugged path wove between house-sized boulders and precarious trees up into some of the park’s official wilderness. The air was sweet from ponderosa pines and cinnamon-colored incense cedars that towered more than 100 feet overhead – even the trees are oversized in Yosemite. Chilnualna Creek’s rapids were never out of earshot. On the way back down, a group of a couple dozen seniors passed us looking as if they did this every day.

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IMG_4736.JPGNext we swung back around to Yosemite Valley; though the valley visitor area is packed with thousands of people during the warmer months, a nearby, little-used trail runs 5 or 6 miles past Mirror Lake into the valley’s quieter upper end. Almost no hikers went further than the crowded lake shore. Half Dome soared almost a mile overhead, the occasional cloud hiding its peak. The sun was bright and the breeze was soft. An hour or so passed, the stream flowing quietly nearby. The path seemed to keep turning away from the rest of the valley as it passed stands of aspen and pine. We started to wonder if the trail was still actually going anywhere. Eventually we joined a family of four wondering the same thing. We kept going.

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IMG_4778.JPGNear where the valley transitions into the smaller and steeper Tenaya Canyon, a sturdy bridge over gushing rapids came into view. Egg-sized granite stones formed little islands in the stream where more pines and cedars grew. Mosquitoes wouldn’t let us enjoy the scene for long. As we finally turned back toward the rest of the valley, we came across a few more hikers. Each asked us if the trail was actually going anywhere.

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IMG_4867.JPGLast came the giant sequoias, relatives of the coastal redwoods. Of the two, redwoods are the giants in terms of height, soaring to almost 380 stunning feet in some cases and holding the record as the tallest trees in the world. Giant sequoias are their heftier cousins, slightly shorter than coastal redwoods but making up for it with their colossal trunks. They’re one of the largest known single organisms and can weigh in at more than 1,000 tons – that’s 10 blue whales to you. They can also be prodigiously old, living up to around 3,000 years. They’re so well adapted to forest fires that they actually need them to reproduce. In the meantime, they can get so big that their own tremendous girth is often what brings them down.

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IMG_4877.JPGIt’s difficult to describe the feeling of being among a group of sequoias, even one as relatively small as Yosemite’s Tuolumne Grove. I could only crane my neck all the way back and try to take in how immense these living towers are. Even the young, “small” ones stand out from the surrounding full-grown pines, imposing and powerful. Yet their bark is spongy and soft, well suited to keeping out flames and the bugs that have decimated conifers throughout the Rockies (thanks partly to climate change, some researchers have found). Strength through softness, my mom said. Like the water that shapes the valley.

We took one last drive through Yosemite Valley before leaving. Long before Muir and others like me walked here, indigenous Miwok people and other tribes lived within the valley’s walls for some eight millennia. Settlers violently took it from them, with the last village removed around when my parents were born. Those people’s descendants are still around. I hope I at least honor their home well.

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IMG_4806.JPGOn the way home from this crazy road trip, New Mexico’s White Sands National Monument was the final major stop. Dust rose from the dune field like steam in the wind on the way to Yosemite. It seemed fitting, in a way, to venture into the field on the way home, almost a sequel to last year’s trek to the Great Sand Dunes. The two places shared the same odd, muffled quietness, though White Sands’ dunes are much smaller. The missile range where the first nuclear weapon was detonated is next door, and an occasional jet broke the silence. The wind-sculpted gypsum sand, pure white and soft as sugar, radiated heat in the sun but stayed cool to the touch. Shadows of puffy clouds sailed across sand waves.

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IMG_4998.JPGA brief stop there, then it was back in the car. All in all, it was a trip full of beauty and bigness and way too much driving.

Thanks for looking.

Dan

Fairs and Elephants

Nothing can deliver nostalgia quite like a county fair — other than the clothes and the cars, they probably look just the same today as they did decades ago in the days of The Sandlot and A Long Way from Chicago. It’s good, pricey, old-fashioned fun, with the added benefit of being a reliable photo-taking ground.

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_C1_0304It was an old-fashioned holiday weekend for me, starting with the Washington County Fair, then continuing up in Missouri with some of the most old-fashioned fun there is: exploring a pair of state parks with the family.

First was Elephant Rocks State Park, sitting about 80 miles south of St. Louis and named for its very own herd of massive, rounded granite boulders and hills nestled within the Missouri forest.

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IMG_9731These behemoths look like they could have tumbled in from elsewhere, but it turns out rain and wind carved them in place over millennia. The boulders are very big – one of the biggest weighs in near 700 tons, or about the same as a hundred actual elephants – and very old. Granite forms when magma cools underground, and this magma did its cooling about 1.5 billion years ago, perhaps before life had even ventured outside of the Earth’s oceans.

The rocks are also fun to climb.

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Nearby sits Johnson’s Shut-Ins State Park, a stretch of the Black River that winds through outcroppings of tough rhyolite rock that’s around the same age as the elephant granite, worn smooth as carved marble to form a really beautiful maze of little water slides and wading pools.

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IMG_9820Rhyolite forms from molten rock, too – it’s the same stuff as granite, but it cooled above ground and quickly instead of below and slowly, giving it that smooth texture. Missouri was active and full of lava back in the day, apparently.

An upstream reservoir ruptured in 2005, flooding the park, but its shut-ins seem unharmed, and the human-made buildings have been rebuilt better than ever. (No one was killed.) I love this place. I could wander between its rocks for hours. Watch your step, though, if you ever go; getting around the smooth rock takes a fair share of scooting and pulling.

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IMG_9859Thanks for looking!

Dan