Tezels on the Road

Tag: National Park

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    Grapevine Hills Trail

    Big Bend National Park

    Ranger PamPaw’s Trail Guide

    A Wonderland of Rocks in the Heart of the Chihuahuan Desert

    Balanced Rock formation in Big Bend National Park with desert mountains and blue sky in the background.
    Rock formations along the Grapevine Hills Trail in Big Bend National Park with desert vegetation including a spiky yucca-like plant and prickly pear cactus in the foreground under a clear blue sky.
    Rocky desert hills and jagged outcrops in Grapevine Hills with distant mountains under a clear blue sky in Big Bend National Park.
    Large rounded boulders and rocky desert terrain in Grapevine Hills with layered mountains in the distance under a blue sky in Big Bend National Park.
    A sandy desert wash lined with dry grasses and shrubs between rocky hills in the Grapevine Hills area of Big Bend National Park under a clear blue sky.

    The Grapevine Hills Trail puts you inside the landscape rather than looking at it from a distance. The route follows a sandy desert wash through a tight valley enclosed by towering laccolith spires — ancient igneous formations sculpted by millions of years of erosion — before a short, steep scramble delivers you to Balanced Rock, two enormous boulders poised on a narrow stone pedestal against an open sky. For a two-mile out-and-back, it earns its payoff.

    Trail Facts

    • Distance: ~2.0 miles round trip
    • Elevation Gain: ~200–250 feet (gradual wash, steep scramble at the end)
    • Difficulty: Easy to Moderate
    • Trail Type: Out & Back (sandy wash with rock scramble at destination)
    • Typical Hiking Time: 1–1.5 hours
    • Pets: Not allowed

    The Grapevine Hills Trail is one of Big Bend’s most rewarding short hikes. The approach through the wash is accessible enough for most visitors, and the final scramble — while requiring some agility over large rocks — is manageable for anyone comfortable on uneven terrain. High-clearance vehicles are strongly recommended for the six-mile unpaved Grapevine Hills Road to the trailhead.

    Getting to the Trailhead

    The trailhead sits at the end of Grapevine Hills Road, roughly six miles off the main paved road in the northern section of Big Bend. The road is unpaved and sandy — high-clearance vehicles are strongly recommended. Check conditions at the Panther Junction Visitor Center before heading out. The visitor center is a good first stop regardless, for maps, water information, and orientation to the park’s three distinct zones.

    Big Bend National Park is located in Brewster County in far west Texas, along the Rio Grande at the U.S.–Mexico border. The nearest town with services is Terlingua, about 26 miles from Panther Junction. The park’s remoteness is part of its character — plan fuel, water, and supplies before you arrive.

    Hiking the Trail

    From the small parking area, the route drops into a broad sandy wash and stays there for most of the hike. The wash winds between walls of weathered igneous rock, the Grapevine Hills rising on both sides. Cairns and the worn path through the sand mark the way. You are walking toward the high ground ahead, and the valley narrows as the spires close in around you.

    The character of the hike shifts as the wash tightens. The open desert gives way to something more enclosed and intimate, the rock formations pressing in from both sides. The sandy footing is soft and slow in places, but the grade is gentle the entire length of the wash.

    Near the end of the trail, the wash delivers you to the base of the final scramble — a steep climb over large boulders toward the gap where Balanced Rock sits. Small directional arrows painted on the rocks mark the route; look for them before committing to a line. The scramble requires using your hands in places and takes most hikers five to ten minutes. At the top, the valley opens up behind you and Balanced Rock fills the frame ahead.

    Trail Map

    Highlights Along the Way

    The Sandy Wash

    The wash is both the trail and the experience. Sandy desert washes are common in Big Bend, but the Grapevine Hills version has a particular quality — the walls rise steadily as you move deeper in, and the spires above take on new shapes from every angle. The soft footing slows your pace in a way that turns out to be useful; this is a trail worth walking slowly. There is no shade and no water anywhere on the route, so start early and carry more than you think you need.

    Balanced Rock

    At the top of the scramble, two massive boulders rest on a narrow stone base, balanced at an angle that looks engineered and is entirely geological. The Comanche people who traveled through this country had a name for formations like this: stones left behind by the Great Spirit. Standing in the gap beneath those boulders, looking back down the full length of the valley, that framing feels as fitting as any scientific explanation.

    Laccolith Geology

    The Grapevine Hills are a laccolith formation — magma that intruded between layers of existing rock roughly 30 million years ago without breaking through the surface, doming the overlying material upward. Over time, erosion stripped the outer layers away and exposed the hard igneous core. The result is the landscape you walk through on this trail: rounded, sculpted spires and boulders that look nothing like the sedimentary cliffs and canyon walls elsewhere in Big Bend.

    What Makes This Trail Special

    Most Big Bend trails put you on a ridge or canyon rim and ask you to look outward. The Grapevine Hills Trail works differently. You are inside the formation for almost the entire hike, surrounded by rock at eye level and above, the valley walls holding you in. The sandy wash builds a kind of anticipation that most desert trails don’t generate — you can see the spires the whole way, but you cannot see Balanced Rock until you’ve earned the scramble. That structure gives the trail a narrative shape that makes it memorable in a way a straightforward viewpoint hike is not.

    Tips for Visiting

    • Start early — there is no shade anywhere on this trail, and the Chihuahuan Desert sun is serious even in spring and fall.
    • Carry at least two liters of water per person. There is no water on the trail or at the trailhead.
    • High-clearance vehicles are strongly recommended for Grapevine Hills Road. Check road conditions at the visitor center before heading out.
    • Look for the small directional arrows painted on the rocks at the scramble. They are easy to miss and mark the safest line up to Balanced Rock.
    • Pets are not permitted on this trail.
    • The trail is not heavily signed — pay attention on the return so you exit the right drainage from the wash.

    Big Bend — 30 Million Years in the Making

    Big Bend National Park encompasses 801,163 acres along a sweeping bend of the Rio Grande in far west Texas, protecting one of the most geologically complex and biologically diverse landscapes in the National Park System. The park spans three distinct zones: the river corridor, the Chihuahuan Desert lowlands, and the Chisos Mountains — a sky island rising above 7,800 feet that supports plant and animal communities found nowhere else in the United States.

    The laccolith formations of the Grapevine Hills are one chapter in a geologic story that stretches back over 500 million years. Big Bend is one of the least-visited major national parks in the contiguous United States — its remoteness filters the crowds — which means the landscape you walk through here feels genuinely untrammeled in a way that parks closer to population centers rarely do.

    Tuesdays on the Trail Video

    This trail guide pairs with our Tuesdays on the Trail video episode, where we walk the Grapevine Hills Trail and explore the geology and character of this remarkable corner of Big Bend National Park.

    Final Thoughts

    The Grapevine Hills Trail asks two miles and a short scramble. It gives back a geology lesson, a Comanche origin story, and a view from beneath two boulders that have no business being balanced the way they are. Big Bend is one of the great parks — too far from everything to be convenient, which is exactly why it remains what it is. Go early. Bring water. Watch for the arrows.

    Helpful Links & Resources

    Tezels on the Road

    More trails. More stories. More perspective.

    Tezels on the Road | Tuesdays on the Trail Channel

  • Ranger PamPaw’s Guide

    Lassen Volcanic National Park

    Where the Earth Still Breathes Fire

    Mineral, California  |  Cascade Range  |  Est. 1916

    ▶ A Note from Ranger PamPaw

    I’ve stood on a lot of park ground over the years, but there’s nowhere quite like Lassen. The moment you smell that sulfur drifting up from Bumpass Hell — that sharp, unmistakable reminder that the earth beneath your boots is still alive — everything about geology and deep time snaps into focus in a way no textbook can replicate. Lassen is the place where the Cascade Range reminds you it isn’t finished yet.

    Most visitors have heard of Yellowstone’s thermal features, but far fewer realize that Lassen Volcanic holds the most diverse and active hydrothermal system in the entire Cascade Range. And unlike Yellowstone, you can experience it without fighting the crowds. This is a park that rewards the curious and the patient — the ones willing to slow down, read the landscape, and listen to what it’s telling you.

    — Ranger PamPaw

    ▶ Quick Facts

    DesignationNational Park
    EstablishedAugust 9, 1916 (17th National Park)
    LocationMineral, California — Southern Cascade Range, ~130 miles north of Sacramento
    Size106,589 acres (166 sq. miles)
    Highest PointLassen Peak — 10,457 feet (world’s largest plug dome volcano)
    Volcano TypesAll four types: plug dome, shield, cinder cone, composite (stratovolcano)
    Last Eruption1914–1917 (most recent in contiguous U.S. before Mount St. Helens, 1980)
    Entrance Fee$30 per vehicle (Apr 15–Dec 1); $10 per vehicle (Dec 1–Apr 15). America the Beautiful Pass accepted.
    Park HoursOpen 24/7 year-round; main park road typically open mid-June through late November
    Visitor CentersKohm Yah-mah-nee (SW entrance, year-round); Loomis Museum (NW entrance, summer only)
    Trails150+ miles of maintained trails; 90,000+ acres of designated wilderness
    PaymentCashless only (credit/debit card, mobile pay) since May 2023
    NPS Websitenps.gov/lavo

    ▶ A Landscape Born of Fire

    Three Million Years in the Making

    The story of Lassen Volcanic National Park doesn’t begin in 1916 — or even in 1914, when the mountain first shook itself awake in the twentieth century. It begins roughly three million years ago, when the forces of the Cascade volcanic arc first began shaping this corner of northern California. The heat source driving it all is the Gorda tectonic plate, a remnant of the ancient Farallon Plate, pressing downward beneath the North American plate just off the Northern California coast. As that slab of ocean floor descends into the earth’s mantle, it generates the magma that has been pushing upward through the Southern Cascades ever since.

    What makes Lassen uniquely extraordinary — and uniquely valuable as a scientific resource — is the sheer diversity of volcanic forms it contains. At least 62 volcanic vents have been mapped within park boundaries. The park is the only place in the United States where all four principal types of volcanoes can be found in a single location: the plug dome (best represented by Lassen Peak itself, the largest of its kind in the world), the composite stratovolcano (remnant of ancient Brokeoff Volcano), the shield volcano (Prospect Peak), and the cinder cone (the dramatic, steep-sided formation that lends its name to Cinder Cone National Monument, one of the park’s two predecessor designations). This volcanic diversity within one protected landscape is virtually unmatched anywhere else in the National Park System.

    The People of the High Country

    Long before European explorers set eyes on the peak, four Native American peoples — the Yana, the Yahi, the Atsugewi, and the Mountain Maidu — inhabited the foothills and forests surrounding what would become the park. The high-elevation terrain, brutal in winter, was not a place of permanent settlement, but these communities moved through it seasonally, hunting deer, fishing mountain streams, and foraging for berries, roots, and acorns. They traded resources with each other, and they understood the mountain’s nature intimately. The Atsugewi knew the peak was filled with fire and water, and they believed it would one day blow itself apart. They were not wrong.

    When fur trappers began exploring northeastern California in the 1820s — still Mexican territory at the time — Lassen Peak became a landmark in sporadic written accounts. By the mid-nineteenth century, westward-bound emigrants were using the peak as a navigational beacon. Two of the era’s major overland routes skirted the area: the Lassen Trail, forged by Danish blacksmith and entrepreneur Peter Lassen, and the Nobles Emigrant Trail, blazed by Minnesota artisan William Nobles. The mountain was formally renamed for Peter Lassen, though his trail proved too arduous for most wagon trains and was eventually abandoned in favor of Nobles’ route — portions of which can still be hiked today within the park’s boundaries.

    ▶ The Eruption That Made a Park

    1914–1917: America Watches a Volcano Wake Up

    The park owes its very existence to an eruption. In May 1914, after what geologists calculate as roughly 27,000 years of dormancy, Lassen Peak began venting steam and ash. The activity started small — minor explosions and new craters — but it escalated. On May 22, 1915, the volcano erupted explosively and dramatically. Lava poured from a new vent near the summit and flowed down the mountain’s flanks, triggering a massive avalanche of snow and rock. The resulting debris flow, carrying volcanic rubble and meltwater, tore through the valley below and destroyed several homesteads along area creeks. A pyroclastic surge — a fast-moving wave of superheated gas and ash — swept across the Devastated Area, leaving a stark, treeless scar across the landscape that remains partially visible today. Thanks to warnings from local observers, no lives were lost.

    The eruptions drew national attention — and they drew national policy. President Theodore Roosevelt had already designated Cinder Cone National Monument and Lassen Peak National Monument in 1907, but the active volcanic drama of 1914–1917 accelerated the case for full park status. On August 9, 1916 — while eruptions were still occurring — President Woodrow Wilson signed the legislation creating Lassen Volcanic National Park, making it the 17th national park in the country and one of the very few established while the landscape it was protecting was still actively erupting. The volcanic activity continued intermittently through 1917, with a final significant blast before the mountain fell quiet again. It would remain the most recent volcanic eruption in the contiguous United States until Mount St. Helens exploded in Washington State in 1980.

    Building a Park in a Young Century

    The park’s early decades were not without turbulence. When the United States entered World War I in 1917, livestock operators mounted a serious campaign to open the park to unlimited grazing, arguing that beef production would support the war effort. The newly created National Park Service — itself less than a year old — sent representatives to defend the park’s integrity before local communities. Their argument: that tourist revenue from a preserved landscape would generate more lasting economic value than grazing ever could. The argument prevailed, helped by congressional funding for park development that made the case concrete. By 1925, the grazing threat had dissolved.

    Infrastructure followed. The 29-mile Main Park Road — still the park’s primary corridor — was constructed between 1925 and 1931, just a decade after the eruption it passes through the aftermath of. Near Lassen Peak, the road climbs to 8,512 feet, making it the highest road in the Cascade Mountains. The Loomis Museum, named for photographer Benjamin Franklin Loomis whose images of the eruptions were instrumental in securing park status, opened in 1927 near the northwest entrance. In 2008, a modern facility opened at the southwest entrance: the Kohm Yah-mah-nee Visitor Center, named after the Mountain Maidu word for Lassen Peak.

    ▶ Touring the Park

    The 30-Mile Drive: A Journey Through Eruption History

    Most visitors experience Lassen via its Main Park Road — Highway 89 — a 30-mile arc through the park’s western corridor connecting the Southwest Entrance (near Mineral, California) to the Northwest Entrance near Manzanita Lake. The drive takes as little as two hours at speed, but the better approach is a full day, with stops at the park’s fifteen numbered interpretive pullouts. Most visitors enter from the southwest, visit the Kohm Yah-mah-nee Visitor Center first, then work northward through the park. The drive can also be taken in reverse from the northwest entrance off California Highway 44.

    Key stops along the road include Sulphur Works (the most easily accessible hydrothermal area in the park, just inside the southwest entrance, featuring steaming fumaroles and hissing vents visible right from the road), Emerald Lake (a strikingly green alpine lake colored by algae), Lake Helen (a clear, deep-blue lake with Lassen Peak towering above it — one of the most photographed views in the park), the Bumpass Hell trailhead, the Devastated Area (a landscape still bearing the scars of the 1915 eruption), Chaos Crags and Chaos Jumbles (a massive boulder field left by a rock avalanche roughly 300 years ago), and Manzanita Lake, a serene reflective lake near the northwest entrance with one of the park’s most iconic views of Lassen Peak.

    Must-Do Trails

    Bumpass Hell Trail — This is the one trail that belongs on every visitor’s list, regardless of age or fitness level. The round-trip distance is approximately 3 miles (NPS) with an easy-to-moderate rating, a gradual 300-foot climb followed by a steeper 200-foot descent into the basin. The trail delivers you onto a boardwalk above the largest hydrothermal area in Lassen — and one of the most active in the Cascade Range — where fumaroles roar, mud pots bubble with rhythmic persistence, and mineral-stained soils glow in shades of orange, white, and sulfur yellow. The area takes its name from pioneer Kendall Bumpass, who fell through the thin crust into a boiling pool during an early exploration of the basin and lost his leg to the injury. Stay on the boardwalk. The trailhead is 7 miles from the Southwest Entrance; the parking lot fills quickly on summer mornings. Arrive early.

    Lassen Peak Trail — For those willing to earn the views, the summit climb is 4.84 miles round-trip with 2,060 feet of elevation gain to the top of the world’s largest plug dome volcano at 10,457 feet. The route is strenuous — constant uphill with no shade and high-altitude thin air — but the summit panorama of the Cascade Range, Sacramento Valley, and surrounding volcanic landscape is extraordinary. Allow 2.5 to 5 hours. Start early to avoid afternoon thunderstorms and to secure parking. The trail is typically open July through October depending on snowpack.

    Cinder Cone Trail — Located in the park’s more remote Butte Lake area, this hike climbs steeply to the rim of a textbook-perfect cinder cone through loose volcanic pumice and scoria. From the top, the view of the Painted Dunes — multicolored ash fields oxidized into vivid reds and oranges by heat from the cone’s lava flows — is unlike anything else in the park. The trailhead is reached via a dirt road from Highway 44; plan extra travel time.

    Brokeoff Mountain Trail — A 7-mile round-trip hike for experienced hikers seeking a less-trafficked alternative to Lassen Peak. The trail climbs through forest to an open summit with sweeping views of Lassen and the surrounding valleys. Much of the route is exposed to direct sun; start early.

    Mill Creek Falls Trail — A 3.8-mile round-trip hike (less crowded than Bumpass Hell) to the tallest waterfall in Lassen National Park, winding through forest and open meadow before the falls reveal themselves. A strong choice for a quieter day in the park.

    ▶ Know Before You Go

    Seasons, Roads, and Snow

    Lassen is a four-season park, but the seasons have teeth. The main park road typically opens in mid-June and closes in late November, and snowpack near Lake Helen regularly reaches 40 feet — patches can persist into July. Even in peak summer, temperatures at elevation can drop sharply; bring layered clothing regardless of the forecast at lower elevations. Popular trails like Bumpass Hell may remain closed into early July due to snow and ice hazards. Always check current conditions at nps.gov/lavo before departure.

    Winter visitors are not without options: Sulphur Works remains accessible year-round near the southwest entrance, and the Manzanita Lake area in the northwest supports snowshoeing and cross-country skiing. The highway between the two visitor centers, however, is not open in winter. The Kohm Yah-mah-nee Visitor Center is open year-round, with reduced hours (Wednesday–Sunday) from November through April.

    Hydrothermal Safety

    This point cannot be overstated: the ground in Lassen’s hydrothermal areas is dangerous. What looks like solid crust can be a thin layer over boiling, acidic water. Visitors who have strayed from marked boardwalks at Bumpass Hell and other thermal zones have suffered severe burns. Stay on boardwalks and designated trails at all times in these areas. This is not a guideline — it is a hard rule enforced by park rangers and enforced by the physics of superheated ground. Children and pets require close supervision. The Big Boiler fumarole at Bumpass Hell has been measured at temperatures exceeding 320°F.

    Getting There, Fuel, and Logistics

    From the west via I-5: take California Highway 44 east from Redding to the Northwest Entrance, or California Highway 36 east from Red Bluff to the Southwest Entrance. From the east via I-80: take U.S. 395 to Susanville, then connect to either Highway 44 (northwest) or Highway 36 (southwest). The nearest commercial airport is Redding Municipal Airport. Gas stations are limited near the park — fuel is available at Manzanita Lake (summer only) and in the communities of Shingletown, Old Station, and Chester. Fill your tank before entering. The park is cashless — credit/debit card or mobile payment only.

    Overnight accommodations within the park are limited to campgrounds (Manzanita Lake, Southwest, Summit Lake, and others) and the historic Drakesbad Guest Ranch in the Warner Valley area. Nearby communities offering lodging include Mineral, Chester, Old Station, and Burney; Redding is a reasonable base for those preferring a full-service city option. Wilderness camping requires a permit ($6 reservation fee plus $5 per person per trip) available through recreation.gov; bear-resistant food canisters are required in the backcountry. Pets are not permitted on backcountry trails or at wilderness campsites.

    The park’s main road includes tight curves and steep drop-offs with no guardrails in sections — drive slowly and keep your eyes on the road, not the views. Pull over at designated pullouts. The speed limit on the park highway is 25 mph.

    Why This Place Matters

    Lassen Volcanic National Park is, at its core, a living laboratory. Nowhere else in the lower 48 states can you stand among all four types of volcanoes, walk above an active hydrothermal system that dwarfs anything in the Cascades, and trace the arc of human stories — Indigenous peoples reading the mountain’s warnings, emigrants navigating by its silhouette, a young nation deciding to protect rather than exploit a landscape still erupting beneath their feet.

    The park also matters because it is underestimated. Consistently overshadowed by Yosemite and Yellowstone, Lassen Volcanic receives a fraction of the attention despite offering comparable geological drama — and with far fewer crowds. The 2021 Dixie Fire burned nearly 70 percent of the park’s area, leaving a stark reminder that even protected landscapes are not immune to the pressures of a changing climate. That scar is now part of Lassen’s story too: a landscape that has survived pyroclastic surges, lava flows, and catastrophic wildfire — and is, by any geological measure, only just getting started.

    Lassen asks the same thing of every visitor: slow down, look closer, and remember that the ground beneath your boots has been building this story for three million years.

    ▶ Park Map

    ▶ First Encounters: Watch the Episode

    Watch Ranger PamPaw’s First Encounters episode for Lassen Volcanic National Park — first impressions, key stops along the park road, and what surprised us most about this underestimated gem of the Cascade Range.

    ▶ Further Exploration

    Official Resources

    Recommended Reading

    • Lassen Volcanic National Park: Auto Tours, Trips & Trails — Larry Eifert (Estuary Press)
    • Hiking Lassen Volcanic National Park — Tracy Salcedo
    • NPS publication: Peak Experiences — free park newspaper, available at both visitor centers

    Listen to the Ranger PamPaw Podcast

    Stories, perspective, and park wisdom from a lifetime in the National Parks.
    Available wherever you listen to podcasts.

    🎙 Listen Now

  • Trail Guide – Great Marsh Trail

    Indiana Dunes National Park

    Ranger PamPaw’s Trail Guide

    Where the Dunes Give Way to the Largest Wetland on Lake Michigan

    Create alt text, title, caption, description, short description, and tags for this image

    Indiana Dunes National Park is famous for its sand dunes and Lake Michigan shoreline — but tucked behind Beverly Shores, away from the beaches, is something most visitors never find. The Great Marsh Trail leads into the largest interdunal wetland in the Lake Michigan watershed: a quiet, flat, one-mile lollipop that delivers open water, migrating birds, spring wildflowers, and one of the most compelling conservation comeback stories in the National Park System. The dunes are the headline, but the marsh is the story you didn’t know you were coming to find.

    Trail Facts

    • Distance: ~1 mile (lollipop loop)
    • Elevation Gain: None — flat throughout
    • Difficulty: Very Easy
    • Trail Type: Lollipop (paved path to observation deck; packed dirt and grass on loop)
    • Typical Hiking Time: 25–30 minutes
    • Accessibility: Paved, wheelchair-accessible trail from the north lot to the observation deck overlook
    • Pets: Allowed on leash (6 ft or shorter)
    • Facilities: No restrooms or potable water at trailhead
    • Hours: Open daily, 6:00 AM – 11:00 PM

    The Great Marsh Trail is one of the most accessible and rewarding short walks in Indiana Dunes National Park. Even visitors with limited time or mobility can reach the observation deck from the north lot on the paved path — and from there, the view across the open marsh is reason enough for the stop.

    Getting to the Trailhead

    The Great Marsh Trail has two parking areas, both located north of U.S. Highway 12 on Broadway Avenue in Beverly Shores, Indiana. The south lot is the main trailhead for the full lollipop loop. The north lot — the one closest to the observation deck — has limited parking (one accessible space and one regular spot) but offers the shortest walk to the marsh overlook. We started from the north lot, which puts you at the heart of the experience almost immediately.

    Indiana Dunes National Park is located along the southern shore of Lake Michigan, roughly an hour southeast of Chicago. Beverly Shores sits near the eastern end of the park. If you’re making a day of it at Indiana Dunes, the Great Marsh Trail pairs naturally with the Dune Succession Trail at West Beach — two very different landscapes within the same park, separated by about fifteen minutes by car.

    Hiking the Trail

    From the north lot, the paved path leads almost immediately toward the marsh. Even before you reach the observation deck, the wetland announces itself — red-winged blackbirds calling from the cattails, the soft sound of water, and on the afternoon we hiked it, the distant bugling of Sandhill Cranes somewhere out in the open water. The path is flat and easy, raised just above the marsh surface, with the wetland pressing close on both sides.

    The observation deck extends out over the edge of the marsh and is the one place on the trail where you step off the raised path and feel truly surrounded by it. The view opens across open water, sedge meadows, and low tree lines in the distance — a wide, quiet panorama that rewards patience and binoculars. We spotted Sandhill Cranes at a distance across the water, along with Swamp Sparrows low in the cattails and Northern Flickers moving through the trees on the return loop.

    From the observation deck junction, the lollipop loop continues east and north through a wooded interior — a quiet contrast to the open marsh. This section feels enclosed and shaded, with early spring light filtering through bare branches and the first wildflowers of the season pushing up through the forest floor. The loop completes and returns you to the junction, where the stem path leads back to the north lot. The whole walk is about a mile, with no elevation change from start to finish.

    Trail Map

    Highlights Along the Way

    The Great Marsh Observation Deck

    The observation deck is the centerpiece of the trail — the one vantage point where the full scale of the marsh opens up in front of you. Bring binoculars. The Great Marsh is a designated birding destination, and the deck is the best spot to scan for Sandhill Cranes, Great Blue Herons, egrets, ducks, and the warblers and blackbirds that move through in force during spring and fall migration. In April, the marsh is particularly active — the spring migration is underway, and the wetland fills with birds pausing on their way north.

    The Wooded Interior Loop

    The loop section of the lollipop winds through a wooded interior that most visitors on a quick out-and-back to the deck never reach. It’s a different character than the open marsh — quieter, more enclosed, with the early spring understory just beginning to wake up. Northern Flickers work the tree trunks, Swamp Sparrows hide in the brush at the woodland edge, and the first wildflowers of the season appear along the path in April. It adds only a short distance to the walk and is well worth completing.

    Spring Wildflowers

    An April visit catches the Great Marsh Trail at a transitional moment — the marsh is waking up, the birds are moving through, and the first blooms of the season are appearing along the trail edges and in the wooded loop. Early spring at the marsh brings marsh marigolds and other wetland bloomers pushing through the wet soil, with more variety following through May and into summer. The combination of open wetland and shaded woodland on this trail supports a wider range of plant life than trails that stay in one habitat type throughout.

    What Makes This Trail Special

    The Great Marsh Trail earns its place not by distance or drama but by what it shows you and what it represents. This is the largest interdunal wetland in the Lake Michigan watershed — a habitat type that once stretched twelve miles along the Indiana lakeshore and was reduced to a fraction of that by draining for farms and development in the early twentieth century. The National Park Service began restoring this portion in 1998, and what you walk through today is the result of more than twenty-five years of patient recovery. The fens, sedge meadows, and wet prairies are thriving again. The birds have returned. The water is cleaner. It is a short walk with a long story behind it.

    Tips for Visiting

    • Bring binoculars — the observation deck rewards them, and birds at the marsh tend to be spread across open water at a distance.
    • Visit in spring or fall for the best birding; migration periods bring the greatest variety of species through the marsh.
    • Complete the full lollipop loop — the wooded interior section is easy to skip if you’re short on time, but it adds worthwhile variety and wildlife.
    • The trail can be wet and muddy after rain; waterproof shoes are a good idea in spring.
    • Check yourself for ticks after the hike — tick season in the dunes area runs from spring through fall.
    • There are no restrooms or water at either trailhead; plan accordingly, especially if combining with other trails in the park.

    A Marsh Restored

    The story behind the Great Marsh is as worth understanding as the marsh itself. During the late nineteenth and early twentieth centuries, this entire wetland system — which once extended from Gary to past Michigan City — was systematically drained through a network of dikes and ditches, converted to farmland and residential lots as the region developed. By the time the National Park Service began acquiring land in the area, the Great Marsh had been reduced dramatically from its original extent.

    Restoration began in 1998 with the removal of drainage infrastructure and the reestablishment of natural hydrology. Over the following decades, the fens, sedge meadows, and wet prairies gradually returned — along with the birds, amphibians, and plant communities that depend on them. The marsh now serves as a natural water filter for the surrounding watershed and as critical habitat for both breeding and migratory birds. Walking the trail with that history in mind changes the experience: what looks like a peaceful wetland walk is also a record of what’s possible when land is given time to heal.

    Tuesdays on the Trail Video

    This trail guide pairs with our Tuesdays on the Trail video episode, where we walk the Great Marsh Trail and take in the sights and sounds of the marsh on an April afternoon at Indiana Dunes National Park.

    Final Thoughts

    The Great Marsh Trail does not ask much — a mile, no hills, half an hour. What it offers in return is a window into one of the most biologically rich and ecologically significant habitats in the Great Lakes region, and a quiet reminder that restoration is possible. Indiana Dunes National Park contains multitudes — dunes, beaches, forests, and wetlands within a few miles of each other — and the Great Marsh Trail is one of the best ways to experience a side of the park that most visitors drive past without knowing it’s there. Plan for an hour. Bring binoculars. Let the marsh be unhurried.

    Helpful Links & Resources

    Tezels on the Road

    More trails. More stories. More perspective.

    Tezels on the Road | Tuesdays on the Trail Channel

  • Ranger PamPaw’s Guide To

    Big Bend National Park

    Brewster County, West Texas  ·  Where the Desert Meets the Sky

    Download This Guide
    Entrance sign for Big Bend National Park along a paved road, featuring a large brown panel with white lettering and a stone base. The sign includes the National Park Service emblem and text noting “Rio Grande Wild & Scenic River” and “A U.S. Biosphere Reserve.” Surrounding the sign are desert plants, rugged hills, and a partly cloudy blue sky.
    Rocky pinnacles and rugged Chisos Mountains landscape viewed from the Lost Mine Trail in Big Bend National Park, Texas.
    Casa Grande Peak rising above the desert landscape in Big Bend National Park beneath a clear blue sky

    ▶   A Note from Ranger PamPaw

    I have a connection to Big Bend that stretches back further than I can remember — literally. In 1964, my family brought me to this park when I was just one year old. My grandparents, who were travelers at heart and had explored parks and landmarks across the country and around the world, made sure Big Bend was on that list. My grandmother captured the whole trip on 8mm film, and I still have that footage today. There is something quietly extraordinary about watching those faded, flickering frames — knowing that the canyon walls and desert skies in the background are the same ones I have returned to dozens of times since.

    In November of 1995, I brought the woman who would become my wife to Big Bend for the first time. We camped in the Chisos Basin, climbed Emory Peak, and wandered every corner of the park we could reach. We have always looked back on that trip as one that brought us together. We have never made it back to Emory Peak — but it remains our spot. Then in 2005, we brought two of our sons on a spring break trip, and watched them discover their own favorite corner of the park: the big sandhill at the mouth of Boquillas Canyon, where they could have played for hours. In 2014, our daughter spent the summer as an intern at Big Bend — another family first, another generation of Tezels finding their footing in this remarkable place.

    There is one image that never leaves me: sitting up in the Chisos Basin as the sun drops toward the horizon, watching the light pour through The Window and spill out into the Chihuahuan Desert below. It is the kind of moment that stops you cold and reminds you exactly why these places exist. Big Bend is not convenient. It is not easy to get to. But I have never once regretted the drive.

    — Ranger PamPaw

    ▶   Quick Facts

    DesignationNational Park
    EstablishedJune 12, 1944
    LocationBrewster County, West Texas
    Size801,163 acres (1,252 sq mi) — larger than Rhode Island
    Entrance Fee$30 per vehicle (7 consecutive days) · $25 per motorcycle · America the Beautiful Pass accepted
    PaymentCashless — credit/debit card only at all entrance stations
    Best SeasonSeptember through early May (avoid summer — desert temps can exceed 115°F)
    Nearest CityAlpine, TX (~80 miles); Midland, TX (~230 miles)
    Park HeadquartersPanther Junction Visitor Center
    UNESCO DesignationInternational Biosphere Reserve · Globally Important Bird Area
    NPS Websitenps.gov/bibe

    ▶   Texas’ Gift to the Nation

    A Park Born from Texas Pride

    Big Bend National Park did not come to be the way most national parks do. It began as a state initiative — in 1933, the Texas Legislature established Texas Canyons State Park in the remote canyon country along the Rio Grande. The name was soon changed to Big Bend State Park, and the Chisos Mountains were added to its boundaries. The National Park Service investigated the site in 1934 and quickly recognized it as, in their own words, “decidedly the outstanding scenic area of Texas.” Congress passed enabling legislation on June 20, 1935, and over the next several years, the State of Texas worked to acquire the land — using public funds, private donations, and the determined efforts of Texas businessman Amon Carter and others who believed this wild, remote country deserved the same protection as Yellowstone or the Grand Canyon.

    On June 6, 1944 — D-Day — Amon Carter personally presented the deed to the park to President Franklin D. Roosevelt on behalf of the people of Texas. Six days later, on June 12, 1944, Big Bend National Park was officially established. President Roosevelt, who had taken a personal interest in the park for years, reportedly felt the nation deserved some good news that week. Texans have called it “Texas’ Gift to the Nation” ever since — and it is a gift that keeps giving, to anyone willing to make the journey.

    A Land of Extraordinary Contrasts

    At 801,163 acres — larger than the entire state of Rhode Island — Big Bend is the largest protected area of Chihuahuan Desert topography in the United States. It is also the only national park in the country to contain an entire mountain range within its boundaries: the Chisos Mountains, rising more than a mile above the surrounding desert floor to Emory Peak at 7,825 feet. The result is an almost theatrical range of environments packed into one park. Temperatures at Rio Grande Village on the river can top 115°F in summer, while the Chisos Basin sits up to 20°F cooler, wrapped in pinyon pine, juniper, and Texas madrone.

    The Rio Grande forms 118 miles of the park’s southern boundary, carving three of the most spectacular river canyons in North America — Santa Elena, Mariscal, and Boquillas — before winding eastward into the Chihuahuan Desert. The park protects more than 1,200 species of plants, 450 species of birds, 56 species of reptiles, and 75 species of mammals. Geological features span millions of years: sea fossils from ancient oceans, dinosaur bones, volcanic dikes, and the slow, layered storytelling of deep time written in stone.

    Ten Thousand Years of Human History

    Long before the park had a name, people had been living in and moving through this landscape for nearly 10,000 years. The Chisos Indians — nomadic hunters and gatherers — inhabited the Big Bend for centuries before the Mescalero Apache pushed through in the early 18th century, followed by the Comanche, who used the famous Comanche Trail on their raids into Mexico. Spanish explorers mapped and named the Rio Grande. Miners, ranchers, and homesteaders came and went, leaving behind ruins, stories, and a deep human texture that is very much part of the park’s identity today. The archaeological record is rich, and the ghost towns and old ranch sites scattered across the desert add a poignant, human-scale counterpoint to the grandeur of the canyons and mountains.

    Why Big Bend Matters

    Big Bend is one of the least-visited major national parks in the country — not because it lacks for grandeur, but because it demands something of you before you arrive. The nearest major city is hundreds of miles away. The roads are long and remote. Cell service is largely absent. But that very remoteness is the point. Big Bend is one of the last places in the lower 48 where you can genuinely feel the scale of the American wilderness — where the sky goes on forever, the river runs free through canyon walls hundreds of feet high, and the silence is something you carry back with you long after you leave.



    ▶   Touring the Park: The Chisos Mountains

    The Chisos Basin

    The Chisos Basin is the heart of the park and the hub for most visitors. Cradled in a volcanic depression in the Chisos Mountains at around 5,400 feet elevation, it offers a cooler refuge from the desert heat, a full-service lodge and restaurant, camping, and access to many of the park’s most beloved trails. The iconic profile of Casa Grande looms over the basin, and The Window — a natural notch in the western rim — frames spectacular sunset views over the Chihuahuan Desert. If you can arrange only one evening in the park, spend it at The Window overlook as the sun goes down.

    Lost Mine Trail ⭐ Ranger PamPaw Favorite

    The Lost Mine Trail is, in this guide’s opinion, the single best hike in Big Bend. Beginning at Panther Pass on the Basin Road, the 4.8-mile round-trip trail climbs through pine-oak woodland with sweeping views of the Chisos Mountains and the desert basin opening below. The trail is well-marked and moderately strenuous — a steady climb with a big payoff. The ridgeline views near the summit take in layer upon layer of landscape, from the high peaks to the Rio Grande canyon country far below. Go early to beat the heat and the crowds.

    📺 Watch: Lost Mine Trail | Tuesdays on the Trails | Big Bend National Park

    The Window Trail

    The Window Trail drops 5.6 miles round-trip from the Chisos Basin trailhead down through Oak Creek Canyon to the lip of The Window pour-off — a narrow slot where the canyon floor drops away into the desert below. It is a pleasant descent through shaded riparian vegetation, with the reward of standing at the pour-off edge looking west across the Chihuahuan Desert. Remember: what goes down must come back up, and the return climb in afternoon heat can be demanding. An easier alternative is the Window View Trail, a short, mostly flat 0.3-mile walk from the lodge area that delivers a classic view of The Window from above.

    Emory Peak & The South Rim

    For those with the legs and the time, the High Chisos trails are among the finest backcountry experiences in the Southwest. Emory Peak — the park’s highest point at 7,825 feet — requires a strenuous 9-mile round-trip from the Chisos Basin trailhead, with a short rock scramble near the summit that rewards with 360-degree views across Texas and into Mexico. The South Rim loop (12–14 miles depending on route) offers one of the most dramatic overnight or long day-hike experiences in the park, with sheer cliff views dropping away to the desert thousands of feet below. These trails are best tackled in spring or fall; carry plenty of water and plan your start time carefully.



    ▶   Touring the Park: The Chihuahuan Desert

    Grapevine Hills Trail

    The 2.2-mile round-trip Grapevine Hills Trail is a desert gem and a wonderful introduction to Big Bend’s igneous rock landscape. The trail winds through a jumbled field of rounded granite boulders before arriving at a natural balanced rock formation — two massive boulders wedged between canyon walls, framing a perfect window to the sky. The hike is relatively easy and suitable for most ability levels, making it a great option for families or as a warm-up for longer days. The trailhead is reached via a dirt road off the Maverick Road, so high-clearance vehicles are recommended.

    Tuff Canyon

    Tuff Canyon is one of the most geologically fascinating stops along the Ross Maxwell Scenic Drive, and one of the easiest to visit. About 30 million years ago, violent volcanic eruptions showered this part of the Chihuahuan Desert with ash and rock fragments that accumulated while still glowing hot, welding together under heat and pressure into the pale, layered material called tuff. Blue Creek, fed by rains in the distant Chisos Mountains, has since carved a spectacular narrow gorge through those layers, exposing the volcanic story in the canyon walls. Three railing-protected overlooks — reached via a 0.5-mile loop on the canyon rim — offer vertiginous views straight down into the gorge. For a more immersive experience, a short spur trail descends to the canyon floor, where you can walk between walls pocked with holes left by bats and embedded with darker volcanic clasts. The contrast between the soft pale tuff and the harder dark rhyolite further up the canyon tells the full story of Big Bend’s fiery past. Plan about 30–45 minutes; combine it with Santa Elena Canyon for a full Ross Maxwell Scenic Drive day.



    ▶   Touring the Park: The River Canyons

    Santa Elena Canyon

    Santa Elena Canyon is one of the most dramatic natural features in the entire national park system. At the end of the Ross Maxwell Scenic Drive, the Rio Grande squeezes between canyon walls that rise 1,500 feet straight up — one wall in the United States, the other in Mexico. The 1.7-mile round-trip trail crosses Terlingua Creek (a rock-hop in dry seasons, a wade in wet ones), climbs stone steps into the canyon’s narrow mouth, and delivers a view of sheer vertical limestone that is genuinely humbling. It is a short hike but one of the most memorable in the park. The drive out on the Ross Maxwell Scenic Drive is itself well worth the time.

    📺 Watch: Santa Elena Canyon Trail | Tuesdays on the Trail | Big Bend National Park

    Boquillas Canyon

    On the eastern side of the park, Boquillas Canyon is quieter than Santa Elena but equally stunning in its own way. The 1.4-mile round-trip trail winds through desert scrub before reaching the river and the canyon entrance, where towering limestone walls glow orange and gold in the afternoon light. Just before the canyon mouth, a large sandhill on the Mexican bank has a way of stopping kids in their tracks — it begs to be climbed, slid down, and climbed again. The Boquillas Canyon area is also the location of the park’s international border crossing to the small Mexican village of Boquillas del Carmen, a unique and worthwhile side trip when the crossing is open.

    📺 Watch: Boquillas Canyon Trail | Big Bend National Park | Tuesdays on the Trail (Special Edition)



    ▶   Know Before You Go

    The Remoteness is Real

    Big Bend’s isolation is not an inconvenience — it is a defining characteristic of the park. The nearest major services are in Alpine, roughly 80 miles away, or Midland, more than 200 miles. There are two gas stations within the park, and a couple of small stores where you can pick up basic supplies — but do not count on them for a full resupply. Come prepared. Fill up before you enter, bring more water than you think you need (a gallon per person per day is the minimum recommendation), and plan your meals. The park has a hard time recruiting and retaining staff precisely because of this remoteness, so services inside the park may be limited or unavailable on any given day.

    Cell Service & Connectivity

    Cell service is limited to the area around Panther Junction (park headquarters) and is largely absent everywhere else in the park. Download your offline maps before you arrive, save NPS trail guides to your device, and let someone know your itinerary. This is not a park where you want to rely on a live connection for navigation or emergency communication. Satellite communicators are a worthwhile investment for anyone heading into the backcountry.

    When to Visit

    Big Bend is fundamentally a winter park. The optimal window runs from September through early May, when temperatures in the desert are manageable and the mountains are at their finest. Summers are brutally hot — desert temperatures routinely top 100°F and can exceed 115°F at lower elevations. The Chisos Mountains run up to 20°F cooler than Rio Grande Village, but summer heat in the basin is still serious. Even in the optimal season, avoid holiday weekends and spring break periods if you can — the park can become very busy, and the infrastructure strains under the load. Weekday visits in October, November, February, or March offer the best combination of weather, crowds, and trail conditions.

    Lodging & Camping

    The Chisos Mountains Lodge is the only lodge inside the park, offering motel-style rooms and historic stone cottages originally built by the Civilian Conservation Corps. It books up well in advance during peak season — reserve early. The park has three developed campgrounds: Chisos Basin, Rio Grande Village, and Cottonwood (near Castolon). All three have their own character, and experienced visitors often have a strong preference. For those seeking more solitude, the park offers backcountry road campsites accessible by high-clearance vehicle and true backcountry sites in the Chisos requiring permits. Just outside the park, options like Big Bend Station provide a comfortable base for multi-day visits.

    ▶   Park Map

    Big Bend National Park Map

    ▶   First Encounters

    Before this visit, Ranger PamPaw sat down to share what Big Bend means to him — the first park he ever visited, the first park they visited as a couple, and a place that has woven itself through a lifetime of family milestones. Watch the First Encounters episode before you go.

    Our First Visits to Big Bend National Park | First Encounters Series

    ▶   Further Exploration

    Official Resources

    Tuesdays on the Trail — Big Bend Videos

    ▶   The Ranger PamPaw Podcast

    Hear More About Big Bend

    Big Bend has been a part of Ranger PamPaw’s life longer than just about anywhere else — and it comes up throughout the podcast. Subscribe to The Ranger PamPaw Podcast for stories, perspectives, and park wisdom from a lifetime on the road.

    🎙 Listen & Subscribe
    Download This Guide

  • Trail Guide – Overlook Ridge Trail

    Overlook Ridge Trail

    Fort Bowie National Historic Site • Arizona

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    The Overlook Ridge Trail is the return option that changes how you understand Fort Bowie. Instead of retracing your steps, this route climbs above the fort and rewards you with sweeping views across Apache Pass—showing why this location mattered, and how carefully it was chosen.

    It’s a more exposed and more strenuous way back to the trailhead, but the perspective it provides is hard to match.

    Trail Overview

    • Trail Name: Overlook Ridge Trail
    • Park / Site: Fort Bowie National Historic Site
    • Location: Ridge above the fort ruins; reconnects with the main route to the trailhead.
    • Distance: Third-party estimates commonly place this segment around ~1.2–1.3 miles (varies by mapping source)
    • Difficulty: More strenuous than the main route (steeper, more exposed)
    • Best Use: As a return route to form a loop with the Fort Bowie Access Trail

    Where the Overlook Ridge Trail Fits

    Most visitors reach Fort Bowie by hiking the main access route through Apache Pass. From the fort area, the Overlook Ridge Trail provides an alternate return that climbs above the site and reconnects with the main trail closer to the trailhead.

    Hiking the Ridge

    The climb is where you feel the difference: the route is steeper and more exposed, and the ridge puts you out in the open where sun and wind are part of the experience. In return, you gain the big-picture view—looking down on the fort and across the surrounding landscape.

    Trail Map

    Highlights Along the Way

    • High-angle views looking down on the fort ruins.
    • Wide views across Apache Pass and surrounding mountain ranges.
    • A stronger sense of why this site was strategically located.

    What Makes This Trail Special

    The Overlook Ridge Trail is about perspective. The main route brings you into the story through artifacts and landscape; the ridge brings you above the story and shows you the geography that shaped it. Together, the two trails make a loop that feels complete. [1](https://www.mypacer.com/routes/oi4b6v/overlook-ridge-trail-hiking-bowie-arizona)

    Tips for Visiting

    Watch the Trail on Tuesdays on the Trail

    We used the Overlook Ridge Trail as our return route from Fort Bowie, highlighting the views and the context it adds to the hike.

    Helpful Links & Resources

    Explore More with Tezels on the Road

    Find more trail guides, videos, and travel stories from our journeys through national parks and public lands.

    Visit TezelsOnTheRoad.com

  • Trail Guide – Fort Bowie Access Trail

    Fort Bowie Access Trail

    Fort Bowie National Historic Site • Arizona

    The Fort Bowie Access Trail is one of those hikes where the walk is inseparable from the place you’re visiting. Fort Bowie is a hike-in historic site reached on foot through Apache Pass, and that approach puts the story in the landscape long before you reach the fort ruins.

    Along the way, you pass layers of history—including the ruins of the Butterfield Overland Mail stage station and a small cemetery—before arriving at the broad hillside of fort foundations and interpretive areas.

    Trail Overview

    • Trail Name: Fort Bowie Access Trail
    • Park / Site: Fort Bowie National Historic Site
    • Location: Near Bowie, Arizona (Apache Pass)
    • Distance: ~1.5 miles one way to the fort / visitor center (about ~3 miles round trip)
    • Difficulty: Easy to Moderate (sun exposure; uneven footing in places)
    • Trail Type: Out & back (or combine with Overlook Ridge for a loop option)
    • Typical Hiking Time: ~2–3 hours round trip plus time exploring the ruins

    Getting to the Trailhead

    Getting to the Fort Bowie trailhead is part of the experience. From the highway, you follow an unpaved road through Apache Pass to the parking area. From there, Fort Bowie is reached on foot.

    Tip: Cell service can be limited in remote areas. Download maps ahead of time, start earlier in the day, and carry water—especially in warmer months.

    Hiking the Trail

    The walk in is about a mile and a half one way, and it does something few park sites do: it slows you down and places the story in the landscape before you ever reach the ruins.

    Along the trail, you pass the remains of the Butterfield Overland Mail stage station—an important stop along a transcontinental route—and then the post cemetery, a quiet reminder of the human cost of life and conflict in this place.

    Fort Bowie was established to protect Apache Pass and Apache Spring, a reliable water source that made this area strategically important. The fort and surrounding landscape became central to the conflict between the U.S. Army and the Chiricahua Apache during the Apache Wars.

    Trail Map

    Highlights Along the Way

    • Apache Pass landscapes and big-sky desert views.
    • Butterfield stage station ruins (wide views and close detail)
    • Post cemetery and interpretive waysides
    • Fort foundations spread across a broad hillside

    History & Context

    Fort Bowie preserves the story of a landscape shaped by travel, water, and conflict. Today, the National Park Service describes the fort and visitor center as accessed by a three-mile scenic loop hike through the historic ground of Apache Pass.

    What Makes This Trail Special

    The Access Trail makes Fort Bowie feel earned. The approach builds context—stage route ruins, cemetery, water source, and landscape—so when you finally stand among the foundations, the place makes sense in a deeper way.

    Tips for Visiting

    • Water & sun: carry water and sun protection—shade can be limited.
    • Footing: expect uneven sections and desert wash crossings.
    • Time: allow extra time for waysides, ruins, and the visitor center area.

    Watch the Trail on Tuesdays on the Trail

    This trail guide pairs with our Tuesdays on the Trail episode on Fort Bowie—walking the route through Apache Pass and exploring the ruins.

    Helpful Links & Resources

    Explore More with Tezels on the Road

    Find more trail guides, videos, and travel stories from our journeys through national parks and public lands.

    Visit TezelsOnTheRoad.com

    “

  • Untitled post 6121

    Ranger PamPaw’s Guide

    Gila Cliff Dwellings National Monument

    Ancient Rooms in Living Stone

    Silver City, New Mexico  ·  Gila Wilderness  ·  Est. 1907

    A wooden ladder leads into the cliff dwellings tucked inside a natural sandstone alcove at Gila Cliff Dwellings National Monument
    Ancient Mogollon masonry walls preserved inside the cliff alcoves at Gila Cliff Dwellings National Monument, New Mexico
    View from inside a cliff alcove looking out over the wooded canyon at Gila Cliff Dwellings National Monument
    The cliff dwelling trail winds through Cliff Dweller Canyon in the Gila Wilderness of southwestern New Mexico
    The forested canyon approach to Gila Cliff Dwellings National Monument along the West Fork of the Gila River

    ▶ A Note from Ranger PamPaw

    “Getting to Gila is a commitment. The drive alone — 44 miles of mountain switchbacks north of Silver City — tells you something about this place before you ever see a single stone wall. The park service isn’t wrong when it says getting here is half the adventure.”

    Most people planning a Southwest trip think Chaco, Mesa Verde, Canyon de Chelly. Gila rarely makes the short list — and that’s exactly why it should be on yours. There are no shuttles, no visitor trams, no gift shop crowds. You hike in. You walk through actual rooms built by actual people more than 700 years ago. You look out through the same cave opening they looked out of. The forest in the canyon below looks almost exactly as it did when those families were living up here.

    This is also one of the least visited sites in the entire National Park System — which I find baffling, given what it offers. If you’re willing to make the drive, you’ll have one of the most intimate archaeological experiences available anywhere in the country. Slow down. Read the walls. Let it land.

    — Ranger PamPaw

    ▶ Quick Facts

    DesignationNational Monument
    EstablishedNovember 16, 1907 — proclaimed by President Theodore Roosevelt
    LocationCatron County, New Mexico — 44 miles north of Silver City via NM-15
    Size533 acres, surrounded by the 3.3-million-acre Gila National Forest
    Elevation5,700–7,300 feet above sea level
    The Dwellings46 rooms across five natural cliff alcoves; occupied late 1270s–approx. 1300
    AdmissionFree — no entrance fee
    Visitor Center HoursOpen daily; closed Thanksgiving, Christmas, and New Year’s Day — check nps.gov/gicl for seasonal hours
    TrailsCliff Dwelling Trail (1-mile loop); Trail to the Past (¼ mile, accessible)
    AdministrationJointly managed by the National Park Service and U.S. Forest Service
    Phone(575) 323-2904
    NPS Websitenps.gov/gicl

    ▶ The Mogollon and the Cliff Dwellings

    700 Years in the Gila Wilderness

    People have moved through the canyons of the upper Gila River for thousands of years. Nomadic groups used the natural cave alcoves above Cliff Dweller Canyon as temporary shelter long before anyone thought to build permanent walls inside them. What makes Gila Cliff Dwellings unusual — and what earned it national monument status in 1907 — is the brief, concentrated moment in history when one particular group decided to stay.

    Those people were the Mogollon — specifically the Tularosa branch of the Mogollon culture, a group that blended hunting, gathering, and farming in the mountain valleys of what is now southwestern New Mexico and southeastern Arizona. The Mogollon had been present in this region for more than a thousand years by the time they built the cliff dwellings, farming the fertile bottomlands along the West Fork of the Gila River — raising corn, beans, and squash in growing seasons that averaged 140 days — while also hunting deer, elk, and turkey in the surrounding forest.

    The cliff dwellings themselves were built rapidly. Tree-ring dates from the original wooden beams — still in place in the caves — show construction spanning from the 1260s through the 1280s. Archaeologists believe 10 to 15 families, perhaps 40 to 60 individuals, occupied the five alcoves, which contain 46 identified rooms. The rooms were built from local stone and mud mortar, fitted into the natural contours of each cave. Wooden beams supported roofs and floors between levels. The workmanship is deliberate and skilled, built to last — and it has.

    Why the Caves? Why Here?

    The choice of cliff alcoves for permanent dwellings — rather than mesa tops or river bottomlands — was not unique to the Mogollon of the Gila. Across the Southwest in the late thirteenth century, many cultures made similar moves toward elevated, defensible positions. Whether the cause was regional conflict, climate pressure, social change, or some combination of all three, the pattern was widespread. At Gila, the natural alcoves offered deep shade, shelter from weather, and sightlines over the canyon below — practical advantages that made them attractive both for temporary use over centuries and ultimately for permanent construction.

    By approximately 1300, the Mogollon had moved on. There is no evidence of catastrophic abandonment — no signs of violence or sudden departure. The rooms were left intact. The community simply dissolved and dispersed, likely joining other populations elsewhere in the region. Where they went, and who their descendants are today, remains an active area of research connecting modern Pueblo peoples and other communities to the culture that built these walls.

    The Apache Connection

    The story of people in this landscape did not end with the Mogollon. The Gila Wilderness was — and remains — part of the traditional homeland of the Eastern Bands of Chiricahua Apache, whose oral traditions, history, and cultural identity are intertwined with these canyons and mountains. The visitor center at the monument includes exhibits on the Chiricahua Apache alongside the Mogollon archaeology, a deliberate acknowledgment that this is not a place with a single cultural story but many layers of human presence across time.

    The TJ Ruin: The Other Site

    The cliff dwellings get nearly all the attention, but the monument also protects the TJ Ruin — a small pueblo on TJ Mesa overlooking the Gila River, inhabited from roughly A.D. 900 to 1150, predating the cliff dwellings by more than a century. The TJ site is near the visitor center and largely unexcavated. It represents a different phase of Mogollon-related occupation in the same landscape, adding depth to the human timeline of this canyon system.

    ▶ Visiting the Cliff Dwellings

    Start at the Visitor Center

    The joint NPS/Forest Service visitor center sits near the base of the canyon, approximately a mile below the cliff dwelling trailhead. Stop here first. The museum displays Mogollon artifacts excavated from the cliff dwellings and surrounding areas — pottery, tools, and personal objects that bring the archaeological record down to a human scale. A 15-minute introductory film provides context for what you’re about to walk through. Rangers can advise on current trail conditions and seasonal access. Pick up the self-guiding trail pamphlet before heading to the trailhead.

    The Cliff Dwelling Trail

    The self-guided Cliff Dwelling Trail is a one-mile loop that climbs 175 feet from the canyon floor up to the cave level. The trail is rated moderate — the elevation gain is manageable, but the route includes wooden ladders, uneven stone steps, and passages that require ducking or careful footing. Allow approximately one hour for the loop at a comfortable pace, more if you plan to read the interpretive signs carefully (which you should).

    The trail brings you directly into the five cave alcoves in sequence. Inside each one, original stone walls and wooden beams are within arm’s reach — this is not a roped-off, view-from-a-distance experience. You walk through the rooms. You look out the doorways. You stand where families once stood, in a canyon that has changed very little in 700 years. That intimacy is rare in the national park system and it is the defining quality of a visit to Gila.

    Trail to the Past (Accessible)

    For visitors unable to manage the ladders and steep sections of the main trail, the Trail to the Past offers a quarter-mile accessible route from the Lower Scorpion Campground to a small Mogollon alcove dwelling and a large pictograph panel. This trail is paved and flat, providing genuine archaeological access without the physical demands of the cliff dwelling loop.

    ▶ Know Before You Go

    The Drive In

    New Mexico Highway 15 north from Silver City is the primary route to the monument, and it earns its reputation. The 44-mile drive takes approximately 1.5 to 2 hours — it is paved throughout but features steep grades, sharp curves, and stretches where the road narrows considerably. Large vehicles and trailers face real challenges; RVs and vehicles over 20 feet should check current NPS guidance before attempting this road. Plan for the drive to be part of your day, not a quick approach. The scenery — climbing through the Gila National Forest from high desert into pine and fir mountain forest — is genuinely worthwhile.

    Seasons and Weather

    Spring and fall are the most comfortable seasons — moderate temperatures, manageable crowds, and good trail conditions. Summer days can be warm even at elevation, and the monument sits squarely in New Mexico’s monsoon belt: expect powerful afternoon thunderstorms from July through September, with lightning that can develop quickly over the canyon walls. Winter brings cold nights and occasional snow, but the monument typically remains accessible year-round. Always check current conditions before you leave Silver City.

    Cell Service and Logistics

    Cell service is extremely limited to nonexistent in the monument and along most of NM-15. Download offline maps before you leave Silver City. Fuel is available in Silver City — do not assume you can top off closer to the park. The monument has no food service; bring water and any food you need for the day. Campgrounds along the creek (Lower Scorpion and Upper Scorpion, managed by the Forest Service) offer sites for those wanting to stay overnight, making a two-day trip genuinely practical and worth considering.

    Pets and Trail Access

    Pets are not permitted on the Cliff Dwelling Trail. They are allowed in the surrounding Gila National Forest and at campgrounds on leash. If you’re traveling with a dog, plan accordingly — someone will need to stay back at the trailhead or campground during the cave loop.

    Suggested Visit Plan

    Allow a full day. The drive from Silver City takes most of the morning. Plan for 30 minutes at the visitor center, 1–1.5 hours on the Cliff Dwelling Trail, and time to decompress and take in the canyon before the return drive. Staying overnight at one of the Forest Service campgrounds turns this into a more relaxed two-day experience — the canyon in the evening, after the day-trippers have left, is something else entirely.

    Why This Place Matters

    The Gila Cliff Dwellings are one of the most accessible and intact examples of Mogollon architecture in the United States — and yet they remain one of the least-visited sites in the entire national park system. That combination is increasingly unusual. The rooms you walk through have not been reconstructed or heavily restored. The original wooden beams placed by Mogollon builders in the 1270s are still in the walls. The views from inside the alcoves look out over a canyon that has changed very little in seven centuries.

    The monument also sits inside the Gila Wilderness — the first area in the United States to receive formal federal wilderness designation, in 1924. The landscape surrounding the cliff dwellings is protected from roads, permanent structures, and most forms of development not just by monument status but by the wilderness designation itself. What you see when you hike into that canyon is as close to the original landscape as anywhere in the Southwest. That is not an accident. It is the result of almost a century of intentional protection — and it is worth the drive.

    ▶ Park Map

    Official NPS map of Gila Cliff Dwellings National Monument showing the visitor center, cliff dwelling trailhead, campgrounds, and surrounding Gila Wilderness

    ▶ First Encounters

    Watch Ranger PamPaw’s First Encounters episode for Gila Cliff Dwellings National Monument — first impressions of the canyon, the approach trail, and what it feels like to walk through 700-year-old rooms still standing in the cliff above the Gila River.

    ▶ Further Exploration

    The Ranger PamPaw Podcast — Tezels on the Road

    Listen to the Ranger PamPaw Podcast

    Stories, perspective, and park wisdom from a lifetime in the National Parks. Available wherever you listen to podcasts.

    🎙 Listen Now

  • Ranger PamPaw’s Guide

    Chiricahua National Monument

    Arizona’s Wonderland of Rocks

    Willcox, Arizona  ·  Dos Cabezas Mountains  ·  Est. 1924

    Towering rhyolite rock pinnacles rise above the trail in the Wonderland of Rocks at Chiricahua National Monument, Arizona
    Narrow rock corridor and balanced stone formations along the Echo Canyon Loop Trail at Chiricahua National Monument
    Wide view across the Wonderland of Rocks from an overlook at Chiricahua National Monument in southeastern Arizona
    Shaded rock grottoes and pinnacle formations inside the Echo Canyon area of Chiricahua National Monument
    Rhyolite spires and volcanic rock formations seen from the Bonita Canyon Drive in Chiricahua National Monument

    ▶ A Note from Ranger PamPaw

    “Chiricahua stops people in their tracks. There’s nowhere else in the park system quite like it.”

    Welcome to Arizona’s Wonderland of Rocks — a sky-island landscape of volcanic pinnacles, balanced rocks, and deep natural and cultural history. This guide supplements our First Encounters episode on Chiricahua, offering everything you need to plan your own visit.

    Few national monument units reward a slow visit more than this one. The drive in, the hike through the formations, the quiet of the campground at night — Chiricahua is the kind of place that earns a return trip before you’ve even left.

    — Ranger PamPaw

    ▶ Quick Facts

    DesignationNational Monument
    EstablishedApril 18, 1924 — to protect the volcanic rock formations and cultural history of the Dos Cabezas Mountains
    Location12856 E Rhyolite Creek Rd, Willcox, AZ 85643 — southeastern Arizona, ~120 miles east of Tucson
    Size11,985 acres within the Coronado National Forest
    Why It’s FamousThousands of rhyolite rock pinnacles, balanced rocks, and spires known as the “Wonderland of Rocks”
    AdmissionFree — no entrance or parking fees
    Visitor Center HoursOpen daily 8:30 a.m. – 4:30 p.m.; closed Christmas Day — check nps.gov/chir for seasonal updates
    Trails17+ miles of maintained trails; Echo Canyon Loop (3.3 mi), Heart of Rocks Loop (7 mi), Massai Point Nature Trail (0.5 mi)
    CampgroundBonita Canyon — 23 sites, reservation-only via recreation.gov; vehicle length limit typically 29 feet
    PetsLeashed pets permitted in parking areas and on the Bonita Canyon Drive; not permitted on trails
    NPS Websitenps.gov/chir

    ▶ How the Wonderland of Rocks Was Made

    The Turkey Creek Caldera

    Approximately 27 million years ago, a massive volcanic eruption — centered on what geologists now call the Turkey Creek Caldera — blanketed this region of southeastern Arizona in a thick layer of ash and volcanic debris. That material compressed and hardened over millions of years into rhyolite tuff, a relatively soft volcanic rock. Then erosion went to work: water, frost, and wind slowly carved the tuff into the improbable landscape visible today — columns, spires, balanced rocks, and pinnacles that seem to defy gravity at every turn.

    The formations are concentrated in the upper reaches of Bonita Canyon, where the geology produced the densest and most dramatic clustering of pinnacles in the monument. This is the heart of what visitors and writers have long called the Wonderland of Rocks — a name that understates the place just enough to let the reality of it land as a genuine surprise.

    The Sky Islands

    Chiricahua sits within one of the most ecologically rich corners of North America — the Sky Islands of southeastern Arizona and northern Mexico. These isolated mountain ranges rise dramatically from the surrounding desert, each one functioning as an ecological island. The elevation gradient within the Chiricahua Mountains alone spans desert scrub at the base to pine, fir, and Douglas-fir forest at the upper elevations, supporting a remarkable diversity of plant and animal life compressed into a relatively small area. Rare birds, including elegant trogons and sulfur-bellied flycatchers, draw birders from across the country.

    The Faraway Ranch and the Erickson-Riggs Legacy

    The monument’s human story is anchored in the Faraway Ranch, homesteaded by Swedish immigrant Neil Erickson in the 1880s. His daughter Lillian, who married Ed Riggs, spent decades advocating for protection of the rock formations she had grown up exploring. The Riggs family developed early tourist facilities in the canyon and lobbied persistently for national monument designation — which came in 1924. Faraway Ranch is listed on the National Register of Historic Places and remains within the monument boundary. The historic district is currently under renovation, but the grounds are accessible and worth a walk.

    The Chiricahua Apache Connection

    These mountains were the stronghold and homeland of the Chiricahua Apache — the same people at the center of the conflict at nearby Fort Bowie. The Chiricahua Mountains gave Cochise’s band both refuge and identity. The landscape that visitors walk through today for its geology was, not long ago, the terrain that shaped one of the most consequential chapters in the story of the American Southwest. That history is present here, woven into the place itself.

    ▶ Touring the Monument

    The Bonita Canyon Drive

    The 8-mile Bonita Canyon Drive is the monument’s primary corridor, climbing from the visitor center at the entrance through oak, pine, and cypress forest to Massai Point at the upper end. The drive takes about 20 minutes at speed but rewards a slower pace — pull-outs offer increasingly dramatic views of the formations as the road ascends. At Massai Point, an overlook delivers 360-degree views of the Wonderland of Rocks and the surrounding mountains, including the Dragoon Mountains to the northwest where Cochise’s Stronghold is located. This is a strong orientation stop before committing to a hike.

    Hiking Options

    Echo Canyon Loop (3.3 miles, moderate) — The essential first-visit hike. The loop descends into Echo Canyon through narrow corridors and shaded grottoes, passes through the Grottoes formation, and transitions to the Hailstone Trail before climbing back via the Ed Riggs Trail. The variety of terrain — tight passages, open overlooks, changing vegetation — makes this the most complete single hike in the monument. See our dedicated Echo Canyon Loop Trail Guide for the full breakdown.

    Massai Point Nature Trail (0.5 miles, easy) — A short loop from the upper parking area at Massai Point through the formations with interpretive signage. Strong option if time or energy is limited; the views justify the drive regardless.

    Heart of Rocks Loop (7 miles, strenuous) — The longer, more demanding route through the monument’s most remote formations, including named features like Punch and Judy, Big Balanced Rock, and Camel Head. Best suited to a second visit or for experienced hikers with a full day. The payoff is solitude and access to formations that most visitors never reach.

    Echo Canyon Grottoes (1 mile, easy-moderate) — A shorter out-and-back that captures the signature grottoes and slot-canyon passages of Echo Canyon without the full loop commitment. A practical choice for families or those short on time.

    ▶ Know Before You Go

    Getting There

    Chiricahua is located about 120 miles east of Tucson via I-10 and AZ-186. The approach road is paved to the visitor center. Large vehicles should note that the Bonita Canyon Drive has some tight curves; the campground has a 29-foot vehicle length limit. The monument is about 25 miles from Fort Bowie National Historic Site — the two parks make a natural two-day combination along this stretch of southeastern Arizona.

    Seasons and Fire Restrictions

    Spring and fall are the most comfortable seasons for hiking — mild temperatures and lower crowds. Summer brings warm days and afternoon monsoon thunderstorms from July through September. Chiricahua frequently experiences spring fire restrictions limiting campfires and stoves at campsites; check current fire conditions at nps.gov/chir before your visit. Winter is generally mild at lower elevations but can bring occasional snow and ice on the upper trails and drive.

    Camping at Bonita Canyon

    The Bonita Canyon Campground offers 23 shaded sites with flush toilets and potable water. Reservations are required through recreation.gov. There are no hookups or dump station. The 29-foot vehicle length limit is enforced — verify your vehicle dimensions before booking. Staying overnight is strongly recommended; the canyon in the early morning, before day visitors arrive, is a different experience entirely from a day trip.

    Pets and Trail Access

    Pets are not permitted on monument trails. Leashed pets are allowed in the parking areas, picnic areas, and campground. Plan accordingly if you’re traveling with a dog — the surrounding Coronado National Forest has trails where pets are permitted on leash.

    Why This Place Matters

    Chiricahua protects one of the most visually distinctive landscapes in the entire National Park System — and one of the least visited. The volcanic geology that created these formations is found nowhere else in the country in this concentration or scale. But the geology is only one layer. The Sky Island ecology, the Chiricahua Apache cultural history, and the ranching heritage of the Faraway Ranch give this place a depth that most visitors only begin to appreciate on a second or third visit.

    The combination of free admission, a scenic drive that works for any ability level, and one of the best moderate hikes in Arizona makes Chiricahua an extraordinary value as a travel destination. Give it a full day — and if you can stay the night, do it. This is a place that rewards the people willing to slow down and let it work on them.

    ▶ Park Map

    Official NPS map of Chiricahua National Monument showing Bonita Canyon Drive, Massai Point, Echo Canyon trailhead, Faraway Ranch, and the Bonita Canyon Campground

    ▶ First Encounters

    Watch Ranger PamPaw’s First Encounters episode for Chiricahua National Monument — first impressions of the Wonderland of Rocks, the Bonita Canyon Drive, and what it’s like to hike into a landscape unlike anything else in the National Park System.

    ▶ Further Exploration

    The Ranger PamPaw Podcast — Tezels on the Road

    Listen to the Ranger PamPaw Podcast

    Stories, perspective, and park wisdom from a lifetime in the National Parks. Available wherever you listen to podcasts.

    🎙 Listen Now

  • Trail Guide – Cliff Dwelling Trail

    Cliff Dwellings Trail

    Gila Cliff Dwellings National Monument • New Mexico

    The Cliff Dwellings Trail at Gila Cliff Dwellings National Monument may be short, but it is one of the most memorable walks in the National Park System. This easy-to-moderate loop trail is the only way to see the monument, leading visitors through a shaded canyon and into ancient cliff dwellings built more than 700 years ago.

    Trail Facts

    • Distance: ~1 mile
    • Elevation Gain: ~180 feet
    • Difficulty: Easy to Moderate (ladders required)
    • Trail Type: Loop
    • Typical Hiking Time: ~1 hour

    This trail is the only way to access the park. While there are steps and ladders to access the cliff dwellings, most people, including families, should be able to hike at least part of the trail.

    Getting to the Trailhead

    Reaching Gila Cliff Dwellings National Monument is part of the experience. From Silver City, a winding mountain road leads deep into the Gila Wilderness, the first designated wilderness area in the United States. By the time you arrive at the trailhead at the end of Cliff Dwellings Road, the landscape already feels remote and quiet.

    Hiking the Trail

    The trail begins by entering Cliff Dweller Canyon, following a creek through a shaded corridor of cottonwoods and sycamores. The cool, sheltered environment is a striking contrast to the desert landscapes found elsewhere in the region.As you hike deeper into the canyon, the sound of water and birds replaces road noise. Before long, you begin to spot stone walls tucked into natural caves above the trail. Even from a distance, the dwellings blend seamlessly into the surrounding rock.

    Trail Map

    Highlights Along the Way

    History and Context

    In the late 1200s, people of the Mogollon culture built these dwellings and lived here for one or two generations. They constructed rooms from stone and mortar, raised families, and relied on the natural shelter provided by the caves.

    Exploring the Cliff Dwellings

    A series of ladders allows visitors to climb into the dwellings themselves. Walking through these rooms is the highlight of the hike, offering views across the canyon and a powerful sense of connection to the people who once lived here.

    What Makes This Trail Special

    The Cliff Dwellings Trail is more than a short walk. It combines natural beauty, cultural history, and a strong sense of place, all within the setting of the Gila Wilderness. Though brief, the experience leaves a lasting impression.

    Tips for Visiting

    • Wear sturdy shoes with good traction.
    • Take your time exploring the dwellings.
    • Visit earlier in the day for cooler temperatures and fewer crowds.
    • Follow posted rules to help protect these fragile structures.

    Tuesdays on the Trail Video

    This trail guide pairs with our Tuesdays on the Trail video episode, where we walk the Cliff Dwellings Trail and explore the dwellings themselves.

    Final Thoughts

    The Cliff Dwellings Trail may only be about a mile long, but it delivers one of the most meaningful trail experiences in southwestern New Mexico. For visitors willing to make the drive, it offers a rare chance to walk through history in a quiet, beautiful setting.

    Helpful Links & Resources

    Tezels on the Road

    More trails. More stories. More perspective.

    Tezels on the Road
    Tuesdays on the Trail Channel

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