By Alan K. Lee
Introduction
Among the many national parks and monuments of southern Utah, Natural Bridges National Monument often gets overlooked. The Big Five national parks – Zion, Bryce Canyon, Capitol Reef, Canyonlands, and Arches (and Grand Staircase- Escalante National Monument) are all deserving of the accolades they receive. They all are full of spectacularly beautiful and awe inspiring places. But if a trip to southern Utah is on your bucket list, don’t leave out a visit to Natural Bridges.
First Impressions
My first visit to Natural Bridges made a lasting impression on me almost immediately. We were there on a very hot day, but once we descended into the canyon, we entered a cool, shaded riparian environment very different from the hot desert landscape above. Natural bridges, unlike arches, are formed by the erosive action of flowing water. And it is that water that makes this place such a welcoming oasis.
My wife and I have been back once since that first visit. The photos here were taken on that second trip in 2008. I think we’re long overdue for a third visit.
Geology
Some 260 million years ago eastern Utah was on the shores of an ancient sea. Over many millions of years the sand deposited on the sea floor was compressed into sandstone, then uplifted by tectonic forces that created the Colorado Plateau. Rivers and streams have since cut their way into the relatively soft sandstone, leaving arches where harder rock overlaid softer, more easily eroded rock.
The white Cedar Mesa Sandstone of the canyons in Natural Bridges was formed from white quartz sand with relatively little iron. The red and orange sandstone of the mesa tops gets its color from more iron rich rocks. Oxygen and hydrogen react with the iron, forming compounds that vary in color depending on the relative proportions of oxygen and hydrogen in the rock.
Human Presence
The Natural Bridges area has been inhabited periodically for about 9000 years. For most of that period, nomadic hunter-gatherers passed through the area. Many of the petroglyphs you’ll find on the canyon walls were done by these Archaic peoples.
The Ancestral Puebloan people began farming the mesa tops around 1500 years ago, but later abandoned the area, presumably because of a prolonged drought. After 300 years, the ancestors of modern day Hopi and Navajo returned to the Natural Bridges area, only to abandon the area again around the year 1280 CE. Modern Hopi, Navaho, and Paiute peoples reoccupied the area once again at later dates.
Europeans didn’t discover the area until 1883 when prospector Cass Hite ventured into the canyons looking for gold. He didn’t find any gold, but he did find the three magnificent natural bridges. Twenty years later, National Geographic Magazine published an article about the bridges, gaining the attention of President Theodore Roosevelt, who established Natural Bridges National Monument in 1908, Utah’s first national monument.
The bridges were named President, Senator and Congressman by Cass Hite. Later explorers gave them the names Augusta, Caroline and Edwin. But neither set of names stuck. In 1909 the bridges were given the Hopi names they carry today: Sipapu, Kachina, and Owachomo.
Getting There
Natural Bridges is located in southeastern Utah, south of Canyonlands National Park. From the town of Blanding drive south on US 191 then turn west on Utah Highway 95. In about 30 miles turn right on Utah 275. The Natural Bridges Visitor Center is 4.5 miles from the junction with Hwy 95.
Visitor Center
The Natural Bridges Visitor Center is a logical first stop when visiting the monument. Pick up a map of the park, fill your water bottles, and ask the staff for information on current conditions, hiking trails, park history, geology, plants and wildlife, etc. There is also a small store and public restrooms. The restrooms and water are available even when the visitor center is closed.
Bridge View Drive
Bridge View Drive is a nine mile one way loop road through the monument, with about a dozen viewpoints, all worth stopping at. There are maintained trails descending into the canyon to all three bridges from Bridge View Drive. All are short, easy hikes down into the canyons, without a huge amount of elevation gain on the return to the canyon rim. There is also an unmaintained trail in the canyon bottoms linking the three bridges, and there is a trail on top of the mesa between the Sipapu Bridge and Kachina Bridge viewpoints.
Night Skies
As beautiful and spectacular as Natural Bridges is during the day, it may be even more so at night. I say it may be only because I’ve not been there after dark. But by all accounts, star gazing is one of the park’s top attractions. Of the 104 International Dark Sky Parks in the world, Natural Bridges was the first so designated.
Where To Stay
There is a small first come first served campground adjacent to the visitor center in the monument, but there are no water, electric, or sewer hookups. The nearest town of any size is Blanding. There are several RV parks and a variety of motels and other accommodations in Blanding, as well as a number of cafes and restaurants.
Roadtripping
Natural Bridges can be included in a gigantic loop that includes Zion, Cedar Breaks, Bryce Canyon, Grand Staircase-Escalante, Capitol Reef, Arches, Canyonlands, Mesa Verde, Monument Valley, Lake Powell, and the North Rim of the Grand Canyon – a truly epic road trip that might take a month or longer to fully experience. And, of course, there are a variety of shorter loops that can be done if you can’t fit all of those destinations into your plans.
Conclusion
Any road trip to southeastern Utah should include a visit to Natural Bridges. It’s a beautiful, interesting, and unique place very worthy of its place among the other parks and monuments of the region. And the surrounding region, part of the 1.3 million acre Bears Ears National Monument, is also well worth exploring.
Originally posted July 10, 2021. Updated July 21, 2024.
All photos © Alan K. Lee
Bayocean Peninsula, on the northern Oregon coast, is a sandspit that separates Tillamook Bay and the Pacific Ocean. It is, by any measure, a nature lover’s paradise, whether you’re a beachcomber, hiker, mountain biker, boater, birder, wildlife lover, or photographer.
To make crossing the Tillamook bar safer, the Army Corps of Engineers recommended jetties be built on both the north and south sides of the bay’s mouth. But half of the cost (a then considerable $2.2 million) would have to be paid by local residents. To cut the cost to a more affordable amount, the local port district proposed building only one jetty. The resulting north jetty, completed in 1917, did make crossing the bar much smoother and safer, but it also contributed to the town’s demise by changing the near shore currents, which began eroding away the beach in the 1920s.
In 1932 the north jetty was extended, further accelerating the erosion. The natatorium was destroyed by waves during a massive storm that winter. By 1938 almost 60 homes had fallen into the sea. Other storms over the years took many of the remaining buildings, and in 1952 another major storm breached the southern end of the peninsula, turning Bayocean Peninsula into an island. The Bay Ocean Park post office closed in 1953 and most of what was left of the town was bulldozed by the Corps of Engineers in 1956 during a project to build a dike across the breach created in 1952. The last house on the peninsula washed away in 1960, and the last structure, a long abandoned garage, fell into the sea in 1971.
The south jetty was eventually built in the 1970s and that stopped the erosion of the peninsula, but by then the town of Bay Ocean Park was long gone. Today, nothing remains of the town. What’s left, though, is a treasure trove of delights for the outdoor enthusiast: miles of untrammeled beach, unspoiled dunes, a bay shore sheltered from the prevailing winds, an upland spruce and pine forest, and an abundance of waterfowl and other wildlife. The haul road used in building the south jetty is now an ideal mountain bike and hiking trail on the bay side of the peninsula.
To reach Bayocean from the town of Tillamook, follow the signs for the Three Capes Scenic Route (Oregon Highway 131). After crossing the Tillamook River bridge, turn right onto Bayocean Road toward Cape Meares. At milepost five, turn right onto the old south jetty haul road (aka the dike road) and proceed to the trailhead parking area. There are pit toilets at the trailhead, but no water.
From the trailhead, the road continues north beyond a locked gate. You can also hike through the dunes to the beach from the trailhead parking area. The road along the bay shore is mostly gravel, with a few sandy stretches, and mostly flat. It’s an easy four mile bike ride to the south jetty.
Hikers can do a 7½ mile loop by hiking through the dunes to the beach, walking the beach to the south jetty, and returning along the bay side on the gravel road. There are several trails connecting the dike road to the beach, making shorter loops possible. And a longer hike or bike ride (10 mile loop or 9 mile out and back along the beach) can be done by starting at the beach access in the town of Cape Meares, instead of the Bayocean trailhead. See my 
The north Oregon coast has much to offer beyond Bayocean Peninsula, of course. 
Originally posted April 23, 2019 by Alan K. Lee, updated July 8, 2021 and March 4, 2024
If you’re ever in the Tucson area, consider making the drive to the top of Mount Lemmon. A paved road takes you to the summit, more than 6500 feet above the valley floor. Numerous viewpoints along the way provide spectacular vistas of the mountain, the surrounding desert below, and the mountains beyond. And numerous trailheads provide access to the ridges and canyons beyond the road for those who want to lace up their hiking boots and immerse themselves in the desert or mountain environment.
The drive takes you through numerous climatic and ecological zones, from the iconic saguaro cactus of the Sonoran Desert at the base of the mountain to an aspen and ponderosa pine forest at the summit.
My wife and I made the drive to the summit in October 2019 while in Arizona to visit my brother and attend a wedding. I had never heard of Mount Lemmon and I wasn’t keen on making that long of a side trip, but my wife convinced me that it would be worthwhile, and she nailed this one. Mount Lemmon is more than just worthwhile, and worth more than just a side trip. It’s a worthy destination in its own right.
Windy Point, about seventeen miles from the beginning of the highway in Tanque Verde, has got to be one of the most spectacular viewpoints in southern Arizona. You’ll want to stop here and just wander around for a while. Take in the views of Tucson and the desert far below, the mountains beyond, and the rock formations around you. About four miles farther up the highway you’ll come to the San Pedro Vista, which gives you a panoramic view east across the San Pedro Valley to the Galiuro Mountains.
Another couple miles brings you to the 
If you go, note that the summit of Mount Lemmon can be thirty degrees cooler than Tucson, so dress accordingly. And if you plan to do any hiking, avoid mid-summer if possible and always bring plenty of water. There are no sources of safe drinking water on any of the hiking trails in the area, to my knowledge.
Not only am I glad we took the drive, I wish we could have spent more time exploring the mountain. For those that do have the time, there are several picnic areas along the highway and a few places to eat in Summerhaven, and there are several campgrounds a short ways off of the highway if you want to spend more than a day on the mountain. If you don’t want to camp, Summerhaven also has a few rental cabins, and a newly built small hotel. Check the 
Note: In the summer of 2020 the entire area was closed to the public because of the Bighorn Fire that burned 120,000 acres in the Santa Catalina Mountains. Photos taken after the fire showed some badly burned areas, but others that were largely untouched. All of the area is open again, including the Palisades Visitor Center.
