- Introduction
- Chapter 1 Davis County Approaches: Farmington Canyon and Francis Peak
- Chapter 2 Mueller Park and the Bountiful Foothills
- Chapter 3 City Creek Canyon: Urban Gateway to the High Ridges
- Chapter 4 The Salt Lake Foothills: Ensign Peak to Dry Creek
- Chapter 5 Red Butte Canyon and the Wire Mountain Ridge
- Chapter 6 Emigration Canyon and Little Mountain Summit
- Chapter 7 Grandeur Peak and the North Edge of Millcreek
- Chapter 8 Lower Millcreek Canyon: Rattlesnake Gulch and Pipeline Trail
- Chapter 9 Upper Millcreek Canyon: Mount Aire, Desolation Trail, and Dog Lake
- Chapter 10 Mount Olympus: Scrambles and the Western Escarpment
- Chapter 11 Lower Big Cottonwood: Storm Mountain and the S-Curves
- Chapter 12 Lake Blanche and the Twin Peaks Wilderness
- Chapter 13 Broads Fork, Dromedary Peak, and Sunrise Peak
- Chapter 14 Butler Fork and the Mount Raymond Cirque
- Chapter 15 Silver Lake and the Brighton Alpine Basin
- Chapter 16 Guardsman Pass, Bloods Lake, and Clayton Peak
- Chapter 17 Lower Little Cottonwood: Granite Monoliths and the Bells Canyon Reservoirs
- Chapter 18 Lone Peak Cirque: Trails, Quartzite, and the Wilderness Boundary
- Chapter 19 Ferguson Canyon and the Desert Peaks Access
- Chapter 20 White Pine and Red Pine Lakes: Alpine Approaches to the Pfeifferhorn
- Chapter 21 Cecret Lake, Catherine's Pass, and Albion Basin
- Chapter 22 Mount Superior and Monte Cristo: High Line Ridges
- Chapter 23 The Corner Canyon Network and the South Salt Lake Valley Traverses
- Chapter 24 The Traverse Mountain Ridge and Flight Park State Recreation Area
- Chapter 25 Connecting Across the Crest: High Ridge Routes and Valley Transitions
Hiking and Mountaineering Around Salt Lake City: Trails, Peaks, and Access
Table of Contents
Introduction
Few metropolitan areas on earth meet alpine terrain with the stark immediacy of the Wasatch Front. Emerging from the flat floor of the Salt Lake Valley, the western face of the central Wasatch Range rises abruptly, lifting the skyline more than seven thousand vertical feet above suburban avenues and light-rail stations. This is not a distant wilderness that requires a day of highway travel to reach; it is a vertical backyard whose shadows touch city parks and neighborhood rooftops every morning. The juxtaposition creates an extraordinary mountain playground, but it also produces a complex, densely utilized landscape where pristine federal wilderness borders suburban developments, mining remnants, protected culinary watersheds, and rapidly shifting trail systems.
This book is a place-by-place survey of that dynamic corridor. Rather than a selective anthology of marquee photo stops, this volume examines the Wasatch Front as an interconnected continuum of drainages, ridges, peaks, and access corridors. Beginning along the rugged northern flanks of Davis County, the scope moves south through the immediate foothills of Salt Lake City, deep into the historic side canyons of Millcreek and the Cottonwoods, and along the southern terminus where Lone Peak yields to the Traverse Mountains. The goal is to provide a grounded, practical guide that looks at the terrain in its full physical and administrative context, acknowledging the geography that makes these routes compelling and the logistics required to navigate them responsibly.
Understanding this terrain requires an appreciation for its dual nature. The lower reaches of these mountains offer year-round, high-volume trail systems shared by dog walkers, trail runners, and mountain bikers, while the upper cirques and ridgelines demand serious mountaineering competence, route-finding acumen, and respect for severe alpine weather. A hiker may step off a commuter sidewalk into dry scrub oak and, within three hours, find themselves scrambling across exposed granite fins or navigating late-season snowfields along narrow knife-edge crests. This book approaches both extremes with the same unvarnished attention to detail, evaluating the walk-up trails with clarity while offering realistic descriptions of the scrambles, loose gullies, and ridgeline traverses that define high-angle travel in the range.
Beyond route logistics, navigating the Wasatch requires understanding the history and stewardship that govern its modern boundaries. The paths we travel today often follow centuries-old game trails, Shoshone and Ute pathways, nineteenth-century logging roads, and mining corridors that once fed silver smelters down in the valley. Today, much of this high terrain is split between the Uinta-Wasatch-Cache National Forest, designated wilderness areas, state recreation parcels, and municipal watersheds that supply drinking water to over a million residents. These distinctions matter on the ground: they dictate where dogs are barred, where campfires are outlawed, which gates are seasonal, and how crowds must be managed. Throughout these chapters, the narrative explains not just where a trail goes, but why access is configured the way it is and how current land-use policies affect your trip planning.
Whether you are a newcomer looking to decipher the canyon network seen from your commute or an experienced mountaineer seeking to link long ridge routes across the alpine crest, this book is designed as a functional field companion and planning reference. It cuts through trail hype to offer direct, plain-prose descriptions of approach roads, trailhead parking realities, route conditions, elevation profiles, and terrain hazards. The Wasatch Front rewards those who approach it with preparation, spatial awareness, and a commitment to tread lightly. Use these pages to plan your lines, understand the ground beneath your boots, and explore the extraordinary wall of stone that anchors the Salt Lake Valley.
CHAPTER ONE: Davis County Approaches: Farmington Canyon and Francis Peak
The northern bastion of the Wasatch Front rises with a singular, wall-like intensity above the cities of Davis County. From Bountiful up through Centerville, Farmington, and Kaysville, the mountainside presents a steep, uniform escarpment of ancient metamorphic rock that seems almost impenetrable to the casual observer. Unlike the deeply incised glacial troughs of the Cottonwood Canyons farther south, the Davis County front is characterized by tight, V-shaped watercourses, precipitous scrub-covered slopes, and a high, undulating ridgeline that hovers near the ten-thousand-foot mark. At the crown of this northern skyline sits Francis Peak, instantly recognizable by the twin, white radar domes that resemble giant golf tees perched on the mountain’s crest.
This high terrain serves as an ideal entry point for understanding the physical geography and human engineering that define the modern Wasatch. The access routes here are a fascinating study in compromise and adaptation. Historically, the steep slopes of Davis County were subjected to intense overgrazing in the late nineteenth and early twentieth centuries, which stripped the native vegetation and triggered devastating mudslides that plowed into the pioneer settlements below. In response, during the 1930s, the Civilian Conservation Corps stepped in to execute one of the most ambitious watershed restoration and mountain engineering projects in western history. The terracing visible on the mountainsides today, along with the narrow roads and trail networks, are direct products of this historical effort to tame the slopes.
For modern hikers, peakbaggers, and trail runners, the Farmington Canyon corridor and the access routes to Francis Peak offer an exceptional introduction to the dramatic vertical transitions of the region. Within a short drive or a stout day’s hike, one can transition from the suburban fringe of the Great Salt Lake basin, through dense groves of gambel oak and bigtooth maple, up into high-alpine meadows of sage and wildflower, and finally onto the windswept, rocky ridges of the main Wasatch crest. The views from these northern summits are unparalleled, offering expansive panoramas that stretch across the shimmering expanse of the Great Salt Lake, the desert islands to the west, and the rolling green ridges of the Backman and Morgan County hills to the east.
The Farmington Canyon Road Corridor
Navigating the transition from valley floor to alpine ridge in Davis County is most directly accomplished via the Farmington Canyon Road, designated as Forest Road 007. This dirt-and-gravel mountain passageway is an engineering marvel in its own right, carving a precarious line up the canyon walls. The road is typically open to passenger vehicles from late spring, after the winter snowpack melts, until the first heavy snows of autumn. For those planning a trip, the canyon entrance is easily accessed from Lagoon Drive in Farmington. Almost immediately after leaving the suburban asphalt, the road turns to dirt and begins its steep, winding ascent, hugging the northern cliffs of the canyon.
The lower section of the road is narrow, often single-lane with occasional turnouts, and features dramatic drop-offs that will quickly command the attention of any driver. While passenger cars can routinely make the trip to the top when conditions are dry, high-clearance vehicles are highly recommended to negotiate the occasional ruts, washboards, and fallen rock that characterize this active mountain corridor. It is also a shared-use road. On any given weekend, drivers will share the dust with mountain bikers, trail runners, off-highway vehicle riders, and hikers aiming for the higher trailheads. Caution, moderate speeds, and a willingness to yield at narrow passing spots are mandatory virtues here.
As the road climbs, it reveals the intricate geology of the Farmington Canyon Complex. This rock unit consists of highly metamorphosed gneiss, schist, and migmatite, some of which is among the oldest exposed rock in Utah, dating back over 1.7 billion years. The glittering flakes of mica and the dark, swirling bands of quartz and feldspar in the roadside outcrops are silent witnesses to the immense tectonic pressures that have repeatedly shaped this margin of the North American continent. At approximately four miles up the canyon, the road passes the ruins of old CCC camps and various stream-monitoring stations, reminding visitors of the ongoing scientific effort required to manage this critical municipal watershed.
The Farmington Creek Trail and Waterfall Canyon
For those who prefer to explore the canyon on foot rather than behind a steering wheel, the Farmington Creek Trail offers an exceptional riparian hike that contrasts sharply with the dry, exposed slopes above. The trail can be accessed from the lower canyon road parking area, near the canyon mouth, or from various pullouts along the first few miles of the road. Following the active stream corridor, the trail winds through a dense canopy of cottonwood, box elder, and willow trees, providing a cool, shaded retreat even during the height of the summer heat.
The path is well-defined but rugged in places, requiring hikers to navigate slick boulders, exposed tree roots, and occasional muddy patches near the creek. Along the way, the trail passes several historical relics, including the rusted remains of vintage automobiles that tumbled into the canyon decades ago, now slowly being reclaimed by the forest. The highlight for many day hikers is the spur trail leading to the Farmington Canyon waterfall. This impressive cascade drops over a polished cliff of metamorphic rock, spraying a cool mist into the surrounding alcove. Reaching the base of the waterfall requires a short, slippery scramble over wet rocks, and hikers should exercise extreme caution, especially during the spring runoff when the water volume is high and the rocks are exceptionally slick.
Beyond the waterfall, the main Farmington Creek Trail continues its upward climb, eventually connecting with the upper shelf of the canyon near the Sunset Campground. This campground, nestled in a grove of mature conifers and aspens at an elevation of nearly 7,500 feet, provides a peaceful midpoint for longer excursions and serves as an excellent basecamp for those wishing to explore the higher-elevation trail networks without committing to a single-day push from the valley floor.
The Ascent to Francis Peak: The Skyline Drive
From the upper basin of Farmington Canyon, the road transforms into the famous Skyline Drive, a high-altitude ridge road that runs north toward Bountiful and south toward Ogden, tracing the very spine of the Wasatch Range. It is along this scenic crest that the approach to Francis Peak reaches its climax. The peak itself stands at 9,560 feet above sea level, and the final approach along the ridge is nothing short of spectacular. The road is carved directly into the crest, meaning that drivers and hikers alike are treated to double-sided exposure, with the vast Salt Lake Valley dropping away to the west and the rolling, pastoral valleys of Morgan County stretching out to the east.
For hikers who wish to summit Francis Peak without driving the entire distance, a popular and challenging option is to park at the Bair Canyon trailhead in Kaysville or the Adams Canyon trailhead in Layton and climb the steep, uncompromising western face of the range. These trails are not for the faint of heart; they are direct, vertical grunts that climb upwards of 4,000 vertical feet in just a few miles. The vegetation transition along these western approaches is dramatic. Hikers begin in dry, sun-baked scrub oak, climb through pockets of Douglas fir and white fir in the mid-elevation bowls, and finally emerge into the subalpine meadows of the crest, where stunted limber pines and alpine wildflowers cling to the rocky soil.
Upon reaching the summit ridge near Francis Peak, the immediate landscape is dominated by the massive FAA radar domes. These structures, built during the Cold War era and still operational today, assist in tracking commercial and military air traffic across the Intermountain West. While the immediate summit area surrounding the radar installations is fenced and restricted for security and safety reasons, the surrounding high points along the ridge are open to the public. Standing on the rocks just outside the facility fence, one can enjoy a panoramic view that, on a clear day, encompasses the Uinta Mountains to the east, the Stansbury and Cedar mountain ranges to the west, and the distant peaks of southern Idaho to the north.
The Great Western Trail and High Ridge Traverses
Francis Peak and Farmington Canyon are central nodes in the Utah section of the Great Western Trail, an ambitious, continuous trail system designed to run from Canada to Mexico. Along the Davis County ridge, this trail is exceptionally well-maintained and offers hikers the opportunity to plan extensive backpacking trips or long-distance trail runs without ever descending into the valleys. The trail winds along the eastern side of the crest, ducking into shaded bowls of aspen and fir before climbing back onto the open, windswept ridges.
One of the most rewarding day hikes along this system is the traverse from Francis Peak north toward Thurston Peak, which, at 9,706 feet, is the highest point in Davis County. This route keeps hikers consistently above 9,000 feet, providing constant, unobstructed views and a true alpine feel. The terrain along the ridge is characterized by open scree fields, grassy meadows, and low-growing sagebrush. Because of the high elevation and lack of tree cover, wind is a constant companion along this route, and weather conditions can change with terrifying speed. Afternoon thunderstorms are a common summer hazard, and hikers must be prepared to retreat down the eastern slopes if lightning begins to develop.
Water is scarce along the high ridge routes, as most of the winter snowpack drains rapidly into the deep canyons on either side of the crest. Hikers planning to spend a full day or an overnight on the Great Western Trail near Francis Peak must carry ample water, as the few springs that do exist are often seasonal and require descent into the steep bowls to locate. Despite these challenges, the high ridge traverse remains one of the premier wilderness experiences on the northern Wasatch, offering a sense of isolation and grandeur that belies its close proximity to the bustling cities below.
Environmental Stewardship and Safety on the Northern Front
The heavy multi-use nature of the Farmington Canyon and Francis Peak areas requires a high level of environmental awareness and adherence to local regulations. Because these canyons serve as primary municipal watersheds for the cities of Davis County, strict water-quality protections are in place. Camping is restricted to designated areas like the Sunset Campground, and visitors are required to pack out all trash and properly manage waste. Dogs are allowed on most of the trails in Davis County, unlike the protected culinary watersheds of Salt Lake County to the south, but they must be kept under control to protect local wildlife and prevent erosion along the fragile stream banks.
Safety on the Farmington Canyon Road and the high ridges is largely a matter of preparation and respect for the terrain. The road is subject to washouts during heavy spring rains, and early-season visitors should always check with the US Forest Service office in Logan or Salt Lake to ensure the gates are open and the road is passable. Cell phone service is surprisingly spotty in the deep cuts of the canyon, though it is excellent once you reach the summit ridge. If you are hiking the steep western face trails like Bair or Adams Canyon, carrying trekking poles is highly recommended to save your knees on the punishing descent, and early morning starts are essential to avoid the intense afternoon heat on these west-facing slopes.
As the northern gateway to the Wasatch, the Davis County approaches provide a rugged, historically rich, and visually stunning introduction to the range. Whether you are navigating the tight switchbacks of the canyon road, cooling off in the spray of the Farmington Creek waterfall, or walking the windswept crest under the shadow of the Francis Peak radar domes, this section of the front sets a dramatic tone for the miles of mountain trails that lie to the south.
This is a sample preview. The complete book contains 27 sections.