Black Canyon of the Gunnison National Park

Posted on October 2, 2025 by admin

A vast stretch of mountains majesty well over the tree line, a complex mass of sand piled at the edge of rugged mountains, and the well-hewn cliffside relics of a people remote in time but whose presence endures – the first three national parks we visited in Colorado in September all rated as exceptional destinations. But I’m glad, simply because it was last on the clockwise loop I’d planned through the state, that Black Canyon of the Gunnison National Park came last. It would have been a hard act to follow.

As a steep – and really deep – crack in the earth, the Black Canyon lives up its name, with most of the canyon cast in shadow most of the time, striking in its seeming darkness. But not pitch black all the way down its 2,000-foot cliffs. Far away, a whitish irregular ribbon runs through the gray bottom of the canyon, quickly recognizable as a river in quicksilver motion. The Gunnison, that is.

If there were no other people around, which happened sometimes at this park, you could hear the roar of the river. Faint, but distinct in its power. Mass snow melts and rushing tributary creeks enable the Gunnison to act (on a geological time scale) like a high-powered saw cutting through rocks that are unimaginably ancient. Before long, that is 2 million years, the river gouged the crack you see, exposing rocks 1,000 times older than the time it took to cut the canyon.

A single two-lane road snakes about seven miles along the south rim of the canyon (should I even have to say it? By the CCC), offering a string of overlooks. Not far from the park entrance, an overlook gives a taste of vistas to come. I might have named the place Gray Canyon, but that isn’t quite as poetic, is it?

Also, evidence of the fire that swept through the park in July, burning about a total of about 4,000 acres on both the south and north rims, along with some Park Service infrastructure. A number of trails leading away from the south rim overlooks were still closed when we visited the park on September 19, with signs disallowing access to charred grounds and slopes.

Fortunately for us, we were able to drive the South Rim Road and see what we could see at some of the overlooks. Unless you’re keen on some kind of lunatic climb into the canyon, that seems like a perfectly reasonable ambition. At the main visitor center on the road – which a ranger told us had barely escaped intact, through the efforts of hotshot crews – a path leads to scenic perch, built to accommodate casual visitors. It survived the fire as well.

Any photo’s going to be a pale image of this vista, but they will have to do. Believe me, it was a place to drop everything and gawk. And, even while safe behind rails, to experience a touch of vertigo. Nothing incapacitating, just an unsettling mental comparison between little you and the huge yawning drop.

A pointy ledge below. An opportunity for an Instagram death. It was hardly the only one.

Further down the road, a good view of the Gunnison. It’s hard to tell just by the images, but that’s around 2,000 feet down. Eventually, the water goes into the Colorado River.

Capt. John Gunnison is the U.S. Army officer and explorer who came to the canyon in 1853 as part of the effort to find a route for the transcontinental railroad. To sum up his conclusion, in terms he would have never used: Not through the Black Canyon, Secretary Davis. Are you kidding me? Later that year, Gunnison and most of his men got the worst of an encounter with some Ute warriors and, among other places, the river acquired his name as a posthumous honor.

I also have to say that Gunnison’s career also included surveying in the Upper Midwest, such as the Green Bay area, and that he surveyed the border between Wisconsin and Michigan. An underappreciated kind of achievement, I’d say.

None of the viewpoints were crowded. The Grand Canyon, this isn’t. The more accessible south rim of the Black Canyon isn’t crowded, even on a warm Friday afternoon, unlike the more accessible south rim of the Grand Canyon.

Near the end of the road is a view of the Painted Wall.

The stripes are not paint, of course, but pegmatite, an igneous rock that solidified after the surrounding rock did, for reasons that a geologist, which would not be me, might be able to explain. A sign at the viewpoint helpfully compares the height of the cliff (2,250 feet) to various manmade structures. The only one that would rise higher than the wall is Burj Khalifa, and that not by much. Note also that the top of the cliff, across on the remote north rim of the canyon, has absolutely nothing in the way of safety infrastructure. The cliff is a cliff, with gravity ready 24/7 to whisk the careless or suicidal to their doom.

I’d be remiss if I didn’t include a few more post-char landscapes: the sort that spread out from South Rim Road for long stretches. It would be a thrill of a road anyway — a little more thrill than I need, actually — with its sporadic few spots where the separation between the road’s edge and an enormous cliff was a single white line.

At the end of the road is the trailhead of Warner Point Trail. From the parking lot, according to a sign, the walk is 1,373 yards to the overlook at Warner Point. Near the sign, I heard a couple of young German men obviously working out the distance in meters (you don’t need much German to understand that). No matter how few people are at a U.S. national park, some are going to be Germans.

I preferred to work out the distances in miles. That would be nearly eight-tenths of a mile, so roughly a 1.6 miles there and back. Or 2.5 km for Euro-types. Better shoes on, poles in hands, hats on heads and water in a small backpacks, we set off on the trail. Yuriko and a few other people (including the Germans) got to Warner Point before I did , but get there I did.

The walk was partly on this kind of trail.

With a fair amount of this kind of thing.

Along the way, an impressive collection of deadwood that the recent fires missed.

With views of the agricultural valley outside the park..

Finally, the end of the trail at Warner Point.

When I got there, Yuriko was waiting. Two other people were there (not the Germans; as athletic sorts, they’d come and gone). Soon they left. So we had the vista to ourselves for about 10 minutes, until another couple came along and we left. When we were quiet, the only sound was the Gunnison far below.

Mesa Verde National Park

Posted on October 1, 2025 by admin

In 800 years or so, will people come from significant distances to look at the ruins of my mid-century neighborhood? That doesn’t seem likely for any number of reasons. I’d be surprised if my own house survives until the next century, considering how good people are now at razing and rebuilding. But considering such a long span of time, there’s no way to know.

That’s the kind of thing I wonder about when facing structures of that age, especially those whose inhabitants are known mainly by the structures and other items they long ago cast off.

On September 17, we’d come to the Cliff Palace at Mesa Verde National Park. To get close, you sign up and pay for a ranger-guided tour, which goes down stone stairs, along the edge of the cliff near the dwellings, and then back up some stone stairs (built by the CCC; does that even need to be said?). The elevation is 7,500 feet or so, but that didn’t cool things down that day. It was hot and sweaty.

A shot like that took some effort. We were hardly alone at Cliff Palace.

The ruins, which are most certainly near a cliff, are probably not a palace in the grand sense of a royal residence. More of a neighborhood, one of many in the vicinity, though the largest. Also, not quite as much of a ruin as it used to be. This is an image of the Cliff Palace from 1891, taken by Gustaf Nordenskiöld.

Not as long ago as all that, considering the age of the structures, but before TR inked the bill creating the national park, and back when you could help yourself to whatever was lying around, as the explorer (and photographer) Nordenskiöld apparently did, taking many items back home to Sweden. Eventually, the items made their way to Finland. A few were returned recently.

The ruins aren’t quite as ruined these days. The 20th century was a period of stabilization. Not as many artifacts got nicked either.

A kiva. The largest one at the Cliff Palace, I think. A religious site similar to others in the Southwest, such as at Bandelier National Monument (and now I know that was a kiva).

The canyon below the Cliff Palace. Imagine having to scramble up and down the walls regularly, to tend to fields or fetch water or escape from marauders.

Mesa Verde is of course much more than the Cliff Palace, since the park protects an estimated 5,000 archaeological sites, including 600 cliff dwellings. The main road through the park (built by the CCC, naturally) takes visitors to other overlooks. The dwellings of Spruce Tree House are sizable and also off limits these days, until the overhead rocks are stabilized.

More cliff dwellings. They are a little hard to see, but they are there.

On top of the main mesa, the road also goes through areas burned by wildfire at one time or another.

Flora always bounces back.

I had the vague idea that the inhabitants of the cliff dwellings disappeared mysteriously after about 1300, but visiting the park schooled me on more current thinking. They left, but there was nothing mysterious about it. Drought hit them, and hit them hard, so they migrated to find water and other sustenance. Persistent violence was probably a factor, too, as tends to happen in periods of strained resources. So it’s pretty clear that Ancestral Puebloans’ descendants even now live among the tribes along the Rio Grande, not too far away.

I also didn’t realize that the well-known cliff dwellings were only occupied for a relatively short time, in the grand scheme of native inhabitation: only about a century. Before that, most of the inhabitants lived atop the mesas. One such ruin is called Far View, which isn’t far from the road.

I heeded this signs and didn’t enter. But you can walk around the perimeter and imagine the passing centuries.

Great Sand Dunes National Park and Preserve

Posted on September 30, 2025 by admin

It’s a safe bet that when most Americans think of scenic Colorado, they think of the sort of mountains you see at Rocky Mountain National Park, or many of the other ranges in the state. Less likely to come to mind is 1.5 cubic miles of sand. That much sand is hard to imagine at all.

That’s the amount of sand thought to be piled at Great Sand Dunes National Park in southern Colorado. Naturally, it isn’t a 1.5-mile cube, though the idea is amusing. The NPS notes that the sand is more spread out: “The 30 square mile (78 sq. km) active dunefield is where the tallest dunes reside. It is stabilized by opposing wind directions (southwestly [sic] and northeasterly), creeks that recycle sand back into it, and a 7% moisture content below the dry surface.”

We approached the park on September 14, heading eastward on Lane 6 North, an Alamosa County road through the flatlands of San Luis Valley, an enormous stretch of land between the San Juan Mountains and the Sangre de Cristo Mountains. At 8,000 square miles, San Luis is the world’s largest alpine valley, the Denver Gazette asserts, with an average elevation at more than 7,600 feet.

Great Sand Dunes was a national monument for longer than it has been a park, though park status represents an enlargement of the monument that President Hoover created. It is Colorado’s newest national park, raised to that status only a little more than 20 years ago.

At a distance of some miles from the park, you notice a pale rim at the foot of the Sangre de Cristo range. As the mountains come better into view, so does the rim, soon looking like a vast pile of sand – which it is – pushed up against the mountains by some enormous broom – which it was not (see above).

Also on offer: a nice view of the Sangre de Cristo, including flora that thrives in the sandy soil of its foothills.

The tourist side of GSDNP features a visitor center and a parking lot and, a short ways away, camp sites. Vegetation girds the parking lot. From there – dunes at the other end of a long sand flat.

No further signs, no trails. Visitors head toward the dunes and wander around wherever they want.

A major activity is sandboarding. Like snowboarding, I suppose, only without the freezing white stuff. Atop this dune, sandboarders are ready to slide.

It’s a young person’s and young families’ game. We happened to meet a pair of young men on one of the dune crests, boards in hand. One of them was wearing a Texas A&M cap, and I asked if he’d gone to school there. He had, finishing a few years ago. I wasn’t entirely certain that he believed me when I told him my grandfather was Class of ’16. That is, 1916.

Horseback riding is also allowed on the dunes, under certain conditions.

We merely took a walk, climbing a few of the smaller dunes. I’d learned my lesson back in 2007, when we clawed our way up a large sand dune in Michigan, at Sleeping Bear Dunes National Lakeshore: “It was a slog. One foot up, then it slides down a bit. After all, it’s warm sand. Make that pretty hot sand. Step, slide back, step, slide back, step, slide back. Rest. Heat. Sweat. Sand in shoes. Remove sand pointlessly, because it comes back. Step, slide back, step, slide back…”

The day at GSDNP wasn’t quite as hot as in Michigan, but the sand was just as sandy. So we admired North America’s largest pile of sand, but not from the top of any particularly large pile.

Rocky Mountain National Park

Posted on September 29, 2025 by admin

On September 15, KKTV in Colorado reported that Trail Ridge Road through Rocky Mountain National Park was “briefly closed Sunday [the 14th] due to the wintry weather. This was first time snow and ice shut down the road since it reopened in May.”

We drove that road two days before, on the 12th. As the article notes, the “48-mile highway through the park is North America’s highest continuous paved road and connects the east and west sides of the park… [it] reaches 12,180 feet at its highest point. Alpine Visitor Center, where snowfall was caught on webcam, is located at about 11,796 feet.”

We’d spent the night before in Granby, Colorado, from the looks of it a growing town – complete with large rows of spanking-new townhouses – and from there entered the park from the western, or less crowded side. The eastern entrance near Estes Park, Colorado, has a more direct connection to the mobs coming from greater Denver.

RMNP is a place of majestic vistas. We came for that, and were not disappointed. But I was just as impressed by something we saw near the western entrance at a place called Holzwarth Historic Site, in the Kawuneeche Valley. A picturesque place.

It was the first place we stopped in the park, walking on a path through part of the valley. A small bridge crossed what looked like a creek.

A sign on the bridge informed us, however, that this was the Colorado River. A flabbergasting moment. I’d known that the Colorado rises in one of the remote parts of the park, but I didn’t know we were going to encounter the river – whose downstream will carve epic canyons and be dammed to the hilt for the water and power needs of millions of people – by crossing it on foot in a few seconds.

The Holzwarths ran a dude ranch on the site for much of the 20th century, before selling it to the Nature Conservancy, which eventually resulted in the area being added to the national park. A number of the dude ranch buildings still exist not far from the baby Colorado River.

From the valley Trail Ridge Road, which is also US 34, heads upward. A look back at the valley.

Soon you reach Milner Pass on the Continental Divide, crossing back to the Atlantic side; we’d crossed to the Pacific side at Berthoud Pass the day before outside the park, on the way to Granby.

From there, the road takes you above the tree line. By that elevation, the warmth down in the valley is just a memory, as brisk chilly winds blow. The air was still above freezing that day, but not by much.

From one of the several pullouts on the road, a path through fields of alpine tundra.

Been a long time since I’d seen any. Back in the Canadian Rockies? No, Alaska. Still, a while ago. We’d reached autumn above the tree line, with the tundra turning.

The road goes on.

Who first built the road? There was none when Rocky Mountain NP became a national park, with President Wilson’s signature on the bill. Improvements came later, and of course they were by the CCC.

At the Alpine Visitor Center, parking was hard but not impossible to find. The views are good from there, but if you want the better vistas, you climb some outdoor stairs. Roughly 200 feet of them.

The air was cold and there wasn’t enough of it. Or so it seemed. I took my hiking pole, put on a sweater and cap and started up. I could have bought a small can of oxygen at the gift shop, had I known about it. I saw a woman, clearly older than me, coming up the stairs as I was headed down, pausing to inhale vigorously from such a can.

Yuriko and Emi made it to the top before I did, but by taking a number of breaks, I managed to get to there myself. Just another thing I should have done 30 (40) years ago. But even then, I’d have been tired at the top.

It’s that extra five feet that leaves you gasping, I think. No matter, the view was worth the gasps. Entirely. The images, as usual for this kind of vista, barely convey the scene in its glory. This is going to be a persistent reality over the next few days’ posts.

Enough to make you burst out with a rendition of “Rocky Mountain High.” If you had the oxygen. I have to say I was glad to repair soon to a lower altitude, one below the tree line. From the Alpine Visitor Center, the road heads toward the eastern entrance to the park, a good many miles away and several thousand feet closer to sea level.

Before we left the parking lot, we saw a fox — guess that would be an alpine fox, pointy snout, pointy ears, billowing with orange and white fur — trot onto the parking lot, as if it had a car parked there. A young ranger, presumably used to the elevation, took chase. Not to catch the fox, which would have been impossible, but probably to prevent the animal from getting run over. Roadkill is one thing, but parking lot kill would have put a small dint in the scenic wonder all around. Anyway, the fox headed for the slopes.

Not only was the air better below tree line, fall foliage was well under way, something we haven’t gotten much of even now here in northern Illinois, though it won’t be long.

One down, three to go. One of the marvels of Colorado’s four national parks is how different each of them are from the others, as we would soon see for ourselves.

Colorado Lasso ’25

Posted on September 28, 2025 by admin

Driving down from the alpine wonders of Rocky Mountain National Park a couple of weeks ago on highway US 36, I realized we’d be passing through Boulder, Colorado. So during one of the moments of standstill traffic on that highway as it winds into Boulder — it’s a crowded road, especially on a weekend during warm weather — a thought occurred to me. More of a memory-thought, since it harkened back almost 50 years.

At zero mph, I had time to consult Google for more information. (Remarkably, the signal was strong.) Google Maps pinpointed the location I’d thought of, on a leafy street in Boulder. That day I expended some tourist energy, of which I don’t have quite as much as I used to, to find Mork’s house.

That is, the house used in establishing shots in Mork & Mindy to show their home, since the show was set in Boulder. I know I’d seen Boulder on maps. Funny name, I thought as a kid. Really Big Rock City. It’s still a little funny. But other than as a spot on the map, the show was probably the first time I’d heard anything else about the place.

The passengers in my car, Yuriko and Emi, having grown up outside of the orbit of ’70s American sitcoms, didn’t particularly appreciate the place. At least not until I conveyed the information that the show made Robin Williams famous. He’s a known quantity. I read a bit about the house later, and there seems to be no consensus about whether the owner cares whether anyone stops by the take a picture. My guess would involving factoring in a dwindling number of people coming by. You know, because the show went off the air over 40 years ago.

Then again, if my U.S. travels have taught me nothing else, it’s that retirees are out being tourists. They have the time they didn’t used to, and currently are just the right age to take a peek at Mork’s house at 1619 Pine Street, which is easy enough to find. Even if, like me, their fondness for that show was lukewarm at best.

Boulder and Mork came early in the second leg of my three-legged, 4,498-mile drive, which seemed to kill that many bugs on the windshield and front hood and bumper. The house counted as merely one spot in a trip that took me through hundreds of places. I spend most of September on the road, heading west from Illinois early in the month along I-80 and smaller roads, especially Nebraska 2 through the Sandhills, and spending time in western Nebraska and its rocky outcroppings and in southeast Wyoming, before going to Denver. That would be the first leg. Which, I’m very happy to say, included a good look at Carhenge.

Yuriko flew to Denver on the last of the points I got from SWA for the Christmastime FUBAR a few years ago and we met there. (New motto for the airline: Now We’re Just Another Airline!) After an overnight jaunt to Rocky Mountain NP in the company of our friend Emi, the two of us then spent more than a week taking a clockwise circle-(like) course — a lasso, you might call it, a straight line connected to a loop — from Denver to Colorado Springs to Pueblo to Walsenburg to Alamosa to (coming down from Wolf Creek Pass) Pagosa Springs to Durango to Silverton to Ouray to Montrose to Salida and back to Denver, where Yuriko flew home. That was the second leg. The drives were varied and gorgeous.

You’d think that would be enough, but I had to drive home, loosely following I-70 this time, making my way from Colorado through Kansas, Missouri and Illinois, and making a number of stops, big and small, such as Kit Carson, Colorado; Abilene, Kansas; and Kansas City, Missouri, for a third and final leg. No single small road took me through Kansas, but a series of them did, some as empty as, well, eastern Colorado and western Kansas. That’s some fine driving. Mountains are great, but after a week or so of their twisty ups and downs on two lanes, flat is all right. More relaxing, even.

For reasons that will soon be obvious, not long ago I looked up 2024 visitation statistics for the four national parks in Colorado: Rocky Mountain, Mesa Verde, Great Sand Dunes, and Black Canyon of the Gunnison.

Far and away the top national park draw in Colorado is Rocky Mountain NP, which received 4.2 million people last year, according to the NPS. In fact, it’s a top ten among most-visited U.S. parks. That isn’t so much of a surprise, considering the monster population that lives nearby in greater Denver and other parts of the Front Range. Indeed, for a lot of people, RMNP is easily a day trip.

That isn’t true for the other three national parks, but even so I was surprised to learn how few people actually visit any of them. They aren’t that remote. We aren’t talking Gates of the Arctic NP or American Samoa NP remote. Still, out of the 63 current U.S. national parks, last year Mesa Verde ranked 41st, Great Sand Dunes 44th, and Black Canyon 49th. The three of them combined saw only about 30 percent as many visitors as Rocky Mountain in 2024.

We set out to see all four of the national parks in Colorado. And we did. You could call it a national park trip, along the lines of the one a few years ago mostly on the Colorado Plateau. But the parks were only a framework, never the total picture, over mountains and across plains. We saw a lot else besides, such a male bear outside our window about 10 miles north of Durango, a female in a tall nearby pine snarling at him, and cubs higher up in the tree. More detail to come on that, in the fullness of time.

Rocky Mountain NP is an exercise in rising above the tree line, by vehicle but also on foot, up a path, into to a satisfying exhaustion before majestic mountains. The pale sand dunes of the Great Sand Dunes NP rise from a valley and back up against a mountain range, as if a giant broom swept it off to corner, and for visitors amounts to a giant sand box. Mesa Verde NP, where the stone dwellings of the Ancient Ones are tucked away in steep stone canyons, shows how much effort people will put into making a home for themselves. Black Canyon of the Gunnison NP is a scenic great unknown, a great dark crack in the earth that reminds you that gravity is in charge, its ragged cliff edges rife with opportunities to die for an Instagram image.

Old Faithful

Posted on August 3, 2025 by admin

Ten years ago, I wrote: Has it been ten years since we visited Yellowstone NP? So it has. Tempus fugit, dude.

I see that decade and raise it by another decade. The children who went with us are now grown. The green Sienna we drove across North America that year and the next, to the Canadian Rockies, is long gone, to a junkyard or just maybe still held together with wire and gum and puttering around some distant road in Mexico.

Less than a week after our visit, I wrote: Naturally we visited Old Faithful. Gotta go see Old Faithful, and wait for it to fulfill its impressive duty, which it did for us at about 6:45 pm on August 5, 2005, pretty much as the rangers predicted — at the information booth, they wrote an estimated time of eruption on a little whiteboard.

That exact eruption 20 years ago.

The geyser is still blowing regularly, according to the NPS, though a little more slowly:

“Old Faithful is one of nearly 500 geysers in Yellowstone and one of six that park rangers currently predict. It is uncommon to be able to predict geyser eruptions with regularity and Old Faithful has lived up to its name, only lengthening the time between eruptions by about 30 minutes in the last 30 years. Thermal features change constantly and it is possible Old Faithful may stop erupting someday.”

Congaree National Park

Posted on July 31, 2025 by admin

Yesterday rain came again to this rainy summer, and had the happy effect of turning the temps down outside today to wrap up July – pleasant 70s F. even at the noonday peak. Northern summers have much to recommend them.

At a hotter time and place, I walked along a boardwalk through a patch of old-growth floodplain forest in the middle of South Carolina. Turns out, that’s a rare kind of landscape, but I didn’t know that at the time.

Somewhere on the way, I renamed Congaree National Park, my location at that moment, in my head. I imagined an act of Congress special to do so. The new name: Congaree National Park and Mosquito Preserve.

I can’t say I wasn’t warned. This information was on display at the park visitors center.

I wouldn’t call Congaree a great unknown, but it is true that among the 63 U.S. national parks, it stood as the 51st-most visited in 2024, attracting 242,049 visitors. Considering that no admission is charged, I wonder how the NPS came up with such an exact number. In any case, that’s a remarkably skinny total compared with the millions who go annually to better-known parks, especially considering that the main park entrance is roughly 30 miles from a sizable city, namely Columbia, SC.

Anecdotal evidence points to the same conclusion: no one I’ve told about the park seems to have heard of it. Then again, I don’t know that I ever gave it much thought myself, except to note it a few times over the years on maps of South Carolina, a state I’d scarcely seen before June – among the Lower 48, the last one I visited.

Other national parks have majestic mountains or picturesque glaciers or striking deserts or epic coastlines or an important history of human activity. They have high-profile wildlife and ecosystems unique in the world. Congaree does count as a special place, preserving a tiny fraction of the floodplain forests that used to cover much of the Southeast, but that’s a little hard to appreciate on the ground, especially as the target of its high-profile wildlife, mosquitoes.

Of the former vast stands of Southeastern floodplain forests, the park, at 11,000 acres, represents much of the roughly 0.5 percent that survives, according to the NPS. Most such land lost its trees to build buildings, plank ships and create railroad ties. The land itself was drained for pastures, farms and settlements.

So Congaree NP is essentially a high-quality museum piece of a landscape, surviving the 19th and early 20th centuries due to inaccessibility. After much agitation on the part preservationists, the area became a national monument by act of Congress in 1976, with President Ford’s signature on the bill (and became a national park in 2003). Apparently that kind of story doesn’t fire the tourist imagination.

Also, while the boardwalk was an easy walk, most of the rest of the park sounds logistically hard on foot. “The Congaree is a wetland forest, and indeed it seems like water is everywhere,” notes American Forests. “There are very few places in the park where you can travel more than a half-mile in one direction without having to cross a pond, lake, creek, seasonal channel (locally called a gut), slough, wet flat, or muck swamp. It is an aquatic and terrestrial maze that constantly changes. About 10 times a year there really is water everywhere as the Congaree River rises to flood the entire area.”

Still, the article lists a large number of tree species that call the park home, including some very tall examples – taller than anywhere else, in some cases.

I’m no expert on trees, but I do know cypress when I see them, with their exaltation of “knees,” those knob-like growths.

***

Not long ago, I found out that Dr. Jamison died late last year. That would be Theodore Roosevelt (Ted) Jamison Jr., born 1933, so he made it past 90. I added this message on an obituary site:

I’m sorry to learn about the passing of Dr. Jamison, but glad that he clearly lived a long, interesting life, loved by family and friends. In 1978, he taught a summer school class for a few weeks at Alamo Heights High School in San Antonio. I was 17 that summer and in that class. It might have been a history or political science class – I don’t remember – but in fact, the class was the Wisdom of Ted Jamison. That wisdom was considerable, as he offered his thoughts and observations about the nation and the world, including prescient warnings about attacks on our freedoms. He also shared snippets about his life up to that point. I didn’t know the half of it, but even then I realized he was a remarkable teacher, an assessment I haven’t revised in the near half-century since then. Reading his obituary, I also see what a remarkable human being he was. RIP, Dr. Jamison.

Bruce Peninsula National Park: The Sand

Posted on October 17, 2024 by admin

Clambering around on rocks, even the kind that don’t require any technical skills, takes energy, so lunch was the next order of business after our hike along the shore of Georgian Bay last Wednesday. We spotted a food truck outside the park, on Ontario 6, called the Hungry Hiker. That seemed fitting.

It had a Bigfoot theme. That seemed odd.

During our travels in the U.S. West, especially Montana-Idaho-Washington state, we noticed many roadside Bigfoot depictions, including this one in metro Seattle, in front of a place in Edmonds where we had lunch one day.

The Hungry Hiker Bigfoot was the only one we saw in Canada. Whimsy on the part of the owner, maybe, which also included some of the menu items, such as the Sweaty Yeti, a chicken sandwich with a sweet glaze. We ordered one, but not The Big Foot, which was a foot-long hot dog. Sasquatch theme or not, the Hungry Hiker’s food was satisfying.

Next stop: Singing Sands Beach at Bruce Peninsula NP. The park includes more than one section, with the beach on the other side of the peninsula, facing Lake Huron proper.

Nice. A big, almost empty beach. In mid-summer, it’s probably overrun. In October, there were only a few people and a frolicking dog.

Behind the beach, a fen.

I don’t know a fen from a bog or a marsh, even though I’ve seen a fen, but that’s what the sign said. It also informed us that resident in the area is the Massasauga rattlesnake (Sistrurus catenatus), “Ontario’s only venomous snake.”

I didn’t know Ontario had any venomous snakes either, much less a rattler. We were further assured that they are small (not a good thing) and shy (better), so they are likely to avoid you. Also, they are endangered, so gardeners in, say, suburban Toronto aren’t at much risk. Canada ≠ Australia, despite some historic similarities. As we tromped along, none were to be heard.

A short trail wandered into the trees near the beach, past a couple of creeks meeting Lake Huron.

The trail was a loop, returning by way of grasslands and more beach, which was a little rocky at that point.

We still had some afternoon left – a warmish day in October isn’t to be wasted – so we went to the BPNP visitor center, back on the Georgian Bay side, to climb the observation tower.

Nice views, though not as much fall color as we’d expected. I could feel the tower shake just a little in the wind, which wasn’t a pleasant sensation. I’m still up for climbing towers for the vistas, but find myself a bit more unnerved by the experience than I used to be.

We still weren’t quite done. We drove the short way to Big Tub Harbour, which isn’t part of the national park, but rather part of the town of Tobermory.

The thing to see there is the lighthouse.

Still a working light, so no climbing, unlike others. Not as storied as the Lighthouse of Alexandria or even the Eddystone Light, but good enough on a windy afternoon in Ontario.

Bruce Peninsula National Park: The Rocks

Posted on October 16, 2024 by admin

A few years ago, Parks Canada, which oversees Bruce Peninsula National Park in Ontario, made noises about changing the name of the park to Saugeen Peninsula NP, after the place name used by the Saugeen Ojibway Nation for the peninsula. The agency started calling the peninsula that, at least internally, and promised a review about the park name. I’d think an actual change would require an act of parliament, but the ways of Canada are mysterious, so I can’t say for sure.

We were merely passing through, but I have a hunch that residents might be attached to “Bruce,” at least for the peninsula itself, so the idea of a name change hasn’t moved forward. Or maybe the process is slow by design. But anyway this was a common sign on the Bruce.

Also, one of the few radio stations receivable on the peninsula is 97.9 FM, The Bruce. If you drive through Port Elgin, as we did twice, you’ll pass the station’s well-marked HQ. If your listen enough, you’ll hear the slogan: Respect the Rock.

In any case, the name remains for now.

In his time – the 19th century – James Bruce, Eighth Earl of Elgin (d. 1863), was a governor of Jamaica, governor general of the province of Canada, and viceroy of India, among other things. Safe to say, then, that he was an imperialist. Pretty much a textbook example. Also, at another point in his career, he ordered the destruction of the Old Summer Palace in Beijing. Oops.

On the other hand, Bruce is a pretty solid name. Maybe the relevant board or committee can declare the peninsula to be named in honor of the entire Clan Bruce, who were so important in the history of Scotland, and whose doughty descendants can be found throughout Canada. That’s a pretty good example of lateral thinking, if I say so myself.

We came to BPNP last week on Wednesday morning (October 9), because this ship wasn’t sailing.

We’d booked round-trip passage to a place called Flowerpot Island, one of the peninsula’s picturesque offshore islands and part of Fathom Five National Marine Park, intending to stay much of the day. But the wind was up, and early that morning, the tour company sent a cancellation notice via email (and we got a refund).

Then we went through a minor amount of rigmarole to change our parking permit at BPNP, because while admission to the park isn’t timed, parking at the park is. We’d planned on visiting the next morning (October 10), before leaving for London. As it turned out, hiking around the Bruce took a fair amount of energy, so best to do it the day before a longish drive, not the same day as a longish drive. Sometimes adjustments on the road work out better.

Our first hike in the national park was simple enough, in theory – out to Georgian Bay, along the edge of Georgian Bay, back from Georgian Bay to the parking lot we’d finagled an early spot in.

The path to Georgian Bay, most of the way along a shallow lake.

Soon you come to the rocky shores of the bay. This place has some centuries (millennia?) to go before it’s a sandy beach. For our part, we’d never seen Georgian Bay before. But for a low place in the Niagara Escarpment, it could have been an entire other great lake, so large is it — 5,800 square miles, or only somewhat smaller than Lake Ontario.

More rocks than you can shake a stick at. And we had our sticks – poles, anyway – and good thing, because the trail crossed the lakeside rock field. It took a little while to eye the course of the trail across the rocks.

I’m not suggesting it was a technically difficult hike. Tricky is more like it, and at my partly advanced age, slow going. But after a few minutes you get the knack for it, or at least enough to position your steps to avoid a tumble.

The trail eventually led back into the woods, which was just as slow.

But worth it, as the trail soon to us back to the wind-swept coast.

With its cliffs.

Winds would have made a bad day on a boat. On the shore, it was a fortuitous ingredient of a good day.

Grand Teton National Park

Posted on October 6, 2024 by admin

Time for a fall break, though it hasn’t been much like fall lately. Cool nights, but warm and almost hot days. This weekend, the nights weren’t even that cool. On Saturday evening we sat on the deck and ate our pizza dinner. The wind was a bit brisk, and willing to carry away unanchored napkins, but other than that it was a wonderful time for dining al fresco. Here in October.

Back to posting on October 13 or so. Or maybe October 15, to honor Italian Food Day, as Ann calls it. Still technically a holiday in most states.

For a North American mountain range, the Tetons are pups, with current scientific assessment putting their age at 6 million to 9 million years. The likes of the Sierra Nevada and the Cascades come in between 40 million and 45 million years old; the Sierra Madre at 60 million years; the Great Smoky Mountains from 200 million to 300 million, just to cite North American examples.

The Tetons’ ongoing formation has something to do with one plate subducting under another and a vast crack in the Earth. I don’t have a deep understanding of geology, but I can get a sense of a slow motion crash – really slow motion, from a human perspective – and enormous volumes of rock being pushed upward.

The wider geology of this part of the West is just as strange and interesting. Deep down under the crust is a hot spot, an imponderable heat bulge that brought volcanism to the surface in Idaho and later Wyoming, as the big North American plate passed over the spot over the last few million years. An eruption of the Yellowstone Caldera is due. Could be tomorrow, could be 1,000 or 10,000 years from now, I understand.

Then there’s the matter, very recent on a geological scale, of the freezing and thawing of ice ages, creator and destroyer of ancient lakes in the area, as illustrated by the unstable ice dams on the Columbia and the cubic miles of water unleased on the gorge not only once, but many times.

Geologically speaking, this part of North America’s having a rumble. What’s really remarkable is that we humans, with our firefly lifespans, have figured all that out. Mostly in my lifetime. You can’t tell that just looking at the grandeur. But knowing all that adds to the view.

Day one. Our first day at the park was driving and some hiking.

Jenny Lake. A scenic drive skirts its shore.

A roadside view of the mountains, but also a river.

The trees line the Snake River. I had little appreciation for the Snake before taking this trip and looking at fine maps like this, which not only details the mighty Columbia but the serpentine Snake, though both of them wind around. We saw the Snake at Grand Teton NP near its origin, but also crossed it where it forms the Oregon-Idaho border, and at Idaho Falls.

Our second day was hiking and some driving.

The trail to Taggert Lake.

When we passed these boulders, the thought popped into my head: What’s the difference, really, between these chunks of rock in the foreground and the peaks in the background? Just mass.

The lake. Wow.

Not a solitary experience.

Father and daughter, I assume. They spent quite a while looking at the many tadpole-like fish in the shallows.

More solitary away from the lake, on the long looping trail back to the parking lot.

We did make the nodding acquaintance of a family. Probably grandparents and their two university-aged grandsons (or maybe one with a friend), probably from a metro in the Northeast. The grandmother, maybe 10 years my senior, looked particularly exhausted by the trail, grayish hair frazzled, face a little pink.

We passed them, though they passed us later as we relaxed in a shady spot. Later, we passed them again as they rested, the grandsons clearly worried about grandma, though I don’t think she was in any real danger, unless she had a health problem I didn’t know about. Still, she was making the effort at however many thousands of feet we were in elevation, with its thinner air.

Again I ask – and always wonder – what is it about mountains? I don’t have the urge to climb, but I do want to get close enough to see their majesty.

Once the hiking is over —

Waiting are the comforts of a rented room. Ahh.

Been There, Seen That

By Dees Stribling

Category Archives: National Parks