Buckner Mountain is one of the most majestic and remote peaks located in the heart of Washington State's North Cascades. Towering at an elevation of 9,114 feet (2,778 meters), it holds the distinction of being the highest summit in North Cascades National Park. Surrounded by rugged peaks, glaciers, and alpine wilderness, Buckner Mountain offers an extraordinary mountaineering experience for skilled adventurers. Its natural beauty, challenging terrain, and relative isolation make it a treasured destination for climbers and nature lovers alike.
Reaching Buckner Mountain is no easy feat鈥攊t involves a long approach, often requiring multiple days of hiking and climbing. The two most common approaches are through Cascade Pass via the Sahale Arm or from the Stehekin Valley.
From Seattle, drive east on Interstate 90, then north on Highway 97, and finally west on Highway 20 (North Cascades Highway) to Marblemount. From there, take the Cascade River Road to the Cascade Pass Trailhead. This is the most popular route, leading to Sahale Glacier and eventually Buckner鈥檚 summit.
Alternatively, some climbers access Buckner from the remote village of Stehekin, which is reachable by boat or plane. From there, trails wind through the vast wilderness toward Buckner鈥檚 eastern face.
Buckner Mountain鈥檚 high elevation and glaciated terrain make its weather conditions unpredictable and extreme. Summer (July through early September) is the best time to visit, when snow has melted on lower trails and conditions are most stable. Summer temperatures can range from 40掳F to 70掳F (4掳C to 21掳C) during the day and fall below freezing at night.
In spring and fall, snowfall and avalanches are common. Winter conditions are extremely hazardous due to deep snow, storms, and ice. Always check the current forecast and avalanche risk before attempting an ascent.
The optimal window to climb or visit Buckner Mountain is from mid-July to early September. During this period, trails to Cascade Pass and the Sahale Glacier Camp are usually snow-free, and the glacier conditions are more manageable for mountaineers.
It is essential to start early in the day to avoid sudden afternoon weather changes and to ensure ample daylight for the long ascent and descent. Due to the strenuous nature of the approach and climb, most visitors plan overnight stays at Sahale Glacier Camp or along the trail.
Buckner Mountain is notable for being the tallest peak in the North Cascades National Park and the 16th highest in the state of Washington. Its rugged and remote nature attracts experienced mountaineers looking for solitude and adventure. The peak is flanked by two glaciers鈥擝oston Glacier and Thunder Glacier鈥攅nhancing its alpine beauty.
The mountain is also admired for the views it offers from the summit. From the top, climbers can see a sea of jagged peaks, including Forbidden Peak, Eldorado Peak, Glacier Peak, and even Mount Baker on a clear day. Its prominence and isolated location make it a bucket-list mountain for serious climbers in the Pacific Northwest.
Buckner Mountain lies within the federally protected North Cascades National Park and Stephen Mather Wilderness. There are no entry fees for hiking, but overnight backcountry permits are required for camping. These permits are issued by the National Park Service and should be reserved in advance, especially during the busy summer season.
Parking at the Cascade Pass Trailhead requires a Northwest Forest Pass, available online or at forest offices. Visitors should be aware that there are no services, stores, or cell phone reception in the area, so all food, water, and gear must be carried in.
Buckner Mountain is named after Henry F. Buckner, an early prospector in the North Cascades region. The first recorded ascent of the mountain was made in 1901 by mountaineers Edward S. Curtis and Asahel Curtis, along with Charles A. Gill and others.
Geologically, Buckner Mountain is composed primarily of granitic rock that is typical of the North Cascades. The glaciers that surround it鈥攅specially Boston Glacier, one of the largest in the Cascades鈥攈ave carved its steep faces and ridges over thousands of years. The rugged appearance and vertical relief are classic examples of alpine glacial erosion.