by Alan K. Lee
In eastern Idaho, northwest of Idaho Falls, the Big Lost River, Little Lost River, and other smaller streams sink into the lava fields and disappear. That water re-emerges a hundred miles to the southwest, from springs on the north side of the Snake River west of Twin Falls – the Thousand Springs.

I can remember seeing part of the Thousand Springs somewhere along US Hwy 30 on a family vacation when I was a kid, back in the late 1950s or early 60s. We didn’t stop back then, but seeing all that water gushing out of the canyon wall obviously made a big impression on me, as I have retained that memory for more than fifty years. And I had a chance to chase down that memory a couple of years ago when my wife and I spent five days exploring southwest Idaho. We spent the first day at Thousand Springs State Park, which consists of seven separate units spread out along the Snake River.

The Malad Gorge unit was our first stop. It’s the most accessible of the seven sections of the park, just off I-84. In what the signs still called Malad Gorge State Park, there is a short trail from a parking area near the park entrance to a viewpoint on the rim of the canyon overlooking the narrow gorge and the 60-foot waterfall and plunge pool known as the Devil’s Washbowl.


The trail continues across a foot bridge 250 feet above the river to another viewpoint a short ways downstream. The road through the park continues from the first parking area to other viewpoints, a large picnic area, and a campground.


Near the campground is another canyon called Woody’s Cove. Although not as impressive as Malad Gorge, the springs at the head of Woody’s Cove were the first of the Thousand Springs that we had a chance to see. (The source of the Malad River is in the Sawtooth Mountains to the north, near Sun Valley, not the Thousand Springs).


There are no trails to the bottom of either Malad Gorge or Woody’s Cove, but the views from the rims of both make the park well worth the five dollar entrance fee. On the other side of I-84 from Malad Gorge is the Kelton Trail section of the park. Here there is a section of the historic Oregon Trail where the wagon wheel ruts can still be seen.


Two of the park’s units are along Billingsley Creek. The lower unit, Billingsley Creek Wildlife Management Area, just north of the town of Hagerman, is an area of marsh and open water that is prime waterfowl and wildlife habitat. Upstream, a few miles east of Hagerman, the Vardis Fisher Day Use Area runs along Billingsley Creek in a narrow valley. The unit is named for the Idaho author of the novel Mountain Man, which was the basis for the 1972 movie Jeremiah Johnson. The ruins of the Fisher home are located in the park unit.

A few miles to the south is the Ritter Island unit of the park. The island was once home to the historic Thousand Springs Dairy Farm run by a locally famous woman named Minnie Miller in the first half of the 20th Century. Ritter Island was also the site of the Payne Lewis Ferry Crossing on the Kelton Road from Boise to Utah. This was an important transportation route in the 19th Century prior to the coming of the railroad.

Some of the structures from the farm and ferry crossing are still standing. There are several miles of hiking trails on the island and, according to the park literature, an abundance of wildlife and wonderful views of the Hagerman Valley. It’s also a good place to kayak, according to the reviews I read. Unfortunately, the island is only open from Memorial Day to Labor Day, and we were there a few days before the island’s opening. It was disappointing that we couldn’t get onto the island, but the springs here made the area worth visiting, regardless.

There are literally hundreds of springs midway up the canyon wall above Ritter Island, and Sand Spring Creek emerges full blown from the cliff face. Much of the water from the springs and the creek have been diverted to a hydroelectric generating plant, and some of the spring water is also diverted to the Ten Springs Fish Hatchery. But there is still lots of water pouring down the canyon walls to a side channel of the Snake River.

The outfall from the fish hatchery tumbles over the cliff face in an impressive waterfall. And below the hatchery there is a Nature Conservancy preserve that has a nice trail along the river below the canyon walls.


Our next stop was the Box Canyon unit of the park (officially the Earl M. Hardy Box Canyon Springs Preserve), a couple of miles south of Ritter Island. The springs at the head of the canyon flow at an impressive 180,000 gallons per minute.

Like at Malad Gorge, there is no trail to the bottom of the canyon here. There is a trail to a viewing platform that overlooks a small waterfall. That trail was closed when we were there, but the views from the canyon rim, here too, were impressive enough.

The final stop on our tour of the Thousand Springs was Niagara Springs, eight miles southeast of Box Canyon. The springs are on the left side of the access road just beyond a fish hatchery. If you have your windows rolled down, you’ll probably hear them before you see them. The roar the springs make is no doubt the inspiration for their name.
There is a short trail to a viewing platform directly below the springs, which flow out of a 150 foot wide section of the canyon wall at a rate of almost 2,000 gallons per second. Just beyond the springs there’s a picnic area and a small tent campground on the right side of the road adjacent to the fish hatchery.


About a mile beyond Niagara Springs you’ll find Crystal Springs and Crystal Lake, which is a popular swimming and fishing spot. But we were there on a Thursday and it was quiet and peaceful, almost deserted. The only swimmers were a pair of white pelicans.

After leaving Niagara Springs and getting a bite to eat in Buhl, we took a short side trip to the rock formation known as Balanced Rock. After climbing up to the base of the rock, we resumed our journey back to Boise, where we were staying. The road from Balanced Rock took us back to Hwy 30 and the Snake River, not far from the Ritter Island area..

I was curious if I could find the spot along the highway that had made such an impression on me on that family vacation so long ago, and I think I did. I’m pretty sure what I saw back then was the springs above Ritter Island. The highway is on the opposite side of the river, but if the hydroelectric plant had not yet been built and none of the spring water was being diverted, there must have been an incredible amount of water pouring out of the canyon wall and tumbling down to the river. No wonder it made such an lasting impression on me. Even with the water diversions, the springs there are still quite a sight from the highway. That was the end of our first day’s outing. Not a bad start, to say the least.


Our trip continued in the following days with visits to Bruneau Dunes State Park, the Snake River Birds of Prey National Conservation Area, and the World Center For Birds of Prey in Boise. We also spent time exploring downtown Boise and the parks and trails of the Boise River Greenbelt. Check out the rest of our southwest Idaho exploration:
Balanced Rock and Bruneau Dunes
The Snake River Canyon and Birds of Prey

Originally posted June 16, 2019. Most recently updated March 31, 2025.
All photos © Alan K. Lee


The park can be very crowded on summer weekends, but gets much less use after Labor Day. Even on a sunny October day there were just a few people fishing from the river bank and some out for a hike or just enjoying the sunshine. This section of the river is popular with kayakers and rafters in the summer, but we didn’t see anyone on the river other than one family that floated by on stand up paddle boards.
The Sandy River flows from its headwaters on Mount Hood to the Columbia River at Troutdale. Two sections of the river totaling 25 miles are designated Wild and Scenic, including the section of the river that runs through Oxbow Park.
In 2007 the Marmot Dam on the Sandy River was demolished, making the river free flowing for its entire 57 mile course for the first time in nearly a century, and opening up miles of restored spawning grounds for salmon and steelhead. A smaller dam on the Little Sandy River was also demolished.
One of the more popular events at Oxbow is the annual
Most of the visitor activity at the park takes place along the banks of the river. The upland trails through the mixed conifer and hardwood forest get much less use. But the forest is beautiful, quiet, and peaceful. If you’re looking for tranquility, head away from the river. On our visit when these photos were taken, we hiked some of the forest trails and saw almost no one.
To get to the park, take I-84 east from Portland to Exit 17 at Troutdale. Turn right onto Graham Road, then left onto the Historic Columbia River Highway. In two blocks, turn right onto Buxton Road. Follow Buxton (which becomes South Troutdale Road) to Division Street. Turn left on Division and follow the signs to the park.
One of the great things about the Pacific Northwest is that there are so many beautiful places like this that are within a half hour drive of even the biggest cities. Just one of the reasons that I think this is one of the best places in the world to live.
If you’ve never been to Point Defiance, check out the park’s 

There is a wide, paved, ADA accessible path (the Promenade) connecting the beach with the marina area of the park and the Point Ruston Waterwalk, giving unhindered pedestrian and bicycle access to the park from the Tacoma waterfront. And a construction project completed in 2022 expanded the parking lot, created new entry and exit paths for pedestrians and cyclists separated from the vehicle roadway, a new beach pavilion, new restrooms, a new ADA accessible children’s playground, new ADA accessible plazas and pathways, and a renovated WPA-era picnic shelter.
The outer loop of the Five Mile Drive provides numerous waterfront access points with views across Dalco Passage to Vashon Island and across The Narrows to the
The outer loop is closed to vehicular traffic part of the day to give cyclists, runners, and pedestrians access to the northern half of the park free from conflicts with motor vehicles. On our most recent visit it was closed after 2:00 pm, but on our previous visit it was, I believe, closed in the morning. Check the Point Defiance Park website (linked above) for the current schedule if you plan to visit the park.




On both of our recent visits our final, and longest, stop was at the botanical gardens area near the entrance to the park. Here there is a large pond with a waterfall, an herb garden, a large rose garden, a dahlia garden, an iris garden, and a Japanese garden. We could easily have spent even more time here than we did on either visit. And if you visit the
Point Defiance Park is one of the largest, and best, city parks in the Pacific Northwest. The park is similar in many ways to Vancouver, BC’s Stanley Park. Point Defiance is, without question, one of Tacoma’s top attractions.
Originally posted May 19, 2019. Most recently updated February 18, 2025.
My wife and I have visited the small community of Stehekin at the head of Lake Chelan in central Washington several times. Our most recent visit came on a week-long escape during the pandemic in 2021.






























The highlights of the trip were the two hikes we did on the Skyline Trail. The first was the four mile out and back hike to Panorama Point. The second was the roughly four mile Skyline-Golden Gate loop. Both are listed as “moderate” hikes, but both have significant elevation gains (1700′ and 1400′ respectively). We did both hikes early in the day during the week, but we were far from the only ones on the trail, especially on the hike to Panorama Point. But the area above Paradise is so incredibly scenic that the crowds didn’t diminish the experience much.


Close to Paradise Inn, the Jackson Memorial Visitor Center, named after long-time U.S. Senator Henry M. Jackson, offers general information, exhibits, a park film, guided ranger programs, a book/gift store and a cafeteria. Unfortunately, all visitor centers in the park are currently closed due to the ongoing pandemic.

Both Paradise Inn and the National Park Inn have full service restaurants, but both were operating on a reduced scale due to the pandemic when we were there in August. The National Park Inn dining room was closed, but take out meals could be ordered and picked up at the reception desk in the lobby. The dining room at Paradise Inn was open for dinner only for most of our visit, but closed (unexpectedly) for the season on our last day there. Paradise Inn also has a limited service cafe, and there is a cafeteria at the Jackson Memorial Visitor Center that is open daily during the summer season and on most weekends and holidays in the winter (depending on road conditions). The National Park Inn restaurant is open year round.
The nearby Snow Lake Trail is an easy and worthwhile hike. To the east, the Stevens Canyon area has a number of interesting areas, including Box Canyon, a 180 foot deep slot canyon, and a number of roadside waterfalls.
The Longmire area has some interesting history, a museum, nice hiking trails, and the National Park Inn offers both lodging and dining options for the visitor. The road to Longmire is also plowed in the winter, so it’s a year round destination. (The road from Longmire to Paradise is open in winter when the weather allows.)
In the Ohanapecosh area in the southeastern corner of the park, the Grove of the Patriarchs Trail is a good family friendly outing. And the nearby Silver Falls Trail is a must for waterfall lovers. In the northeastern section of the park, the Sunrise area offers beautiful views of the eastern side of the mountain and has an abundance of hiking trails.


The Lake
Crater Lake is 1943 feet deep, making it the deepest lake in the United States, second deepest in North America, and ninth deepest in the world. It is also one of the cleanest and clearest lakes in the world. It’s that combination of depth and clarity that results in its intense deep blue color.
The caldera that Crater Lake occupies was formed 7700 years ago when the summit of 12,000 foot tall Mount Mazama collapsed after a massive eruption. Over time rain and snow filled the caldera to its present level. The lake has no outlet. The level of the lake remains nearly the same because the amount of evaporation from the surface of the lake closely matches the amount of precipitation falling on it in any given year.
Wizard Island formed sometime after the eruption that formed the caldera. It rises 770 feet above the surface of the lake, 2713 feet above the deepest point in the lake. It last erupted about 5000 years ago, but it is considered dormant, not extinct. Conceivably, it could erupt again at any time. Merriam Cone also erupted after the caldera was formed, but never reached the lake surface. Its summit lies almost 500 feet below the average lake level.
Phantom Ship, a remnant of an eruption 400,000 ago, rises 170 feet above the lake surface. Its formation predates that of Mount Mazama itself.
The Park
Crater Lake Lodge
My wife and I recently spent three nights at the lodge. Although it lacks the amenities of a luxury hotel, our room was comfortable, with a private bathroom, and the location more than makes up any lack of luxuries.
The Rim Drive
You’ll want to stop at all of the viewpoints. Maybe combine the drive with a hike down to Cleetwood Cove and a boat tour of the lake. You can get off at Wizard Island and hike to the summit and then catch a later boat back.
For a more adventurous day, hike to the summit of Mount Scott, the highest point in the park. It’s a two mile hike to the summit with 1250 feet of elevation gain, so it’s not an easy hike (All Trails rates it “moderate”), but the view might just be worth the effort.
Hiking Trails
The Pacific Crest Trail passes through the park, but does not ascend to the rim of the caldera. Hikers on the PCT can take the Dutton Creek Trail that climbs up to the Rim Village, then hike the trail that parallels the West Rim Drive and reconnect with the PCT north of the lake.
The Pinnacles
Practical Info
There are two lodges in the park, Crater Lake Lodge in the Rim Village and The Cabins At Mazama Village that are open for the summer season. Crater Lake Lodge has 71 rooms, starting at $246/night. The Cabins At Mazama Village has 40 rooms, all at $160/night. Prices listed are for the 2024 season. Note that the concessionaire that operates both lodges is changing, so prices may also change. Check the park website (linked above) for current information.
There are two campgrounds in the park. Mazama Campground has 75 RV sites, 18 tent sites with electricity, and 121 tent sites without electricity. Tent sites start at $22. RV sites run from $32 to $44 per night. Mazama Campground is usually open from early June through late to September. Lost Creek Campground, located on Pinnacles Road, is a primitive tent only campground with 18 sites, operated by the park service. Lost Creek Campground is currently closed and will not be open for the 2024 season. Backcountry camping is allowed in the park by
Dining options in the park are somewhat limited. The dining room at Crater Lake Lodge is open to all visitors, but reservations can only be made by people staying in the park. The Rim Village Cafe offers “grab and go” sandwiches and salads (I had a pulled pork sandwich from there on our recent visit that was very good). It is open from 9am to 8pm in the summer and 10am to 5pm in the winter. The Annie Creek Restaurant in Mazama Village is open from 7am until 9pm. The Mazama Village Store sells packaged sandwiches and snacks.
Summer park entrance fees are $30 for private vehicles and $25 for motorcycles. Winter fees are $10 less. Snowmobilers, bicyclists, and pedestrians are charged $15 per individual. All entrance fees are good for seven days. Entry reservations do not need to be made.
Originally posted September 13, 2021. Most recently updated April 6, 2024.


























For hikers, there are more than 45 miles of trails in the canyon. You could easily spend days in the canyon and not hike all of the trails. For those that do want to spend multiple days hiking or sightseeing, 

First Impressions
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.
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 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
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.
Visitor Center



Conclusion
Originally posted July 10, 2021. Updated July 21, 2024.
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.
