Itineraries: Anchorage to Nabesna in the Summer
Truly the Road Less Traveled
Not many folks seem to know about the beautiful, and little traveled route from Anchorage to northern Wrangell-St. Elias National Park & Preserve, that offers numerous spectacular adventure opportunities, diverse cultures, and wide open spaces to just relax and soak in Alaska’s spirit. Having made the journey hundreds of times in nearly 60 combined years, in all of the seasons, we know just where to look for some of the most unforgettable places and the best times to visit them. If you’re looking for a unique and authentic experience that only a small handful of visitors know about, check out this route. You just might find the real, friendly, unscripted Alaska as you make your way around the dancing mountains and into the headwaters country of the legendary Copper River.
Day 1
From Anchorage, head east toward Wrangell-St. Elias, with points of interest along the way:
-- Brief intro/overview of Glenn Hwy history you can go to https://www.alaska.org/guide/glenn-highway-guide
--Matanuska Glacier viewing wayside (outhouse) or privately owned site for glacier hike.
--Check crags above Caribou Creek large paved rest area (no toilet/outhouse, south side of highway) for Dall sheep (great with binoculars), near mile 106-107.
Dall Sheep
--Continue east toward Glennallen, enjoying expansive views of an ancient pre-glacial lake basin.
Wrangell Mountains over the Copper River
--Moving east along the Glenn Hwy you'll see the impressive peaks of the Wrangell Mountains, left to right Mt Sanford 16,237 ft; Mt Drum 12,010 ft; and Mt Wrangell 14,163 ft. The local/native nickname is the "Dancing Mountains" because they appear to trade places as you view them from different places in the basin, as you travel the roads around the mountains.
Nelchina Glacier, Chugach Mountains by Takeshi Sugimoto
--South of the road you'll note the Nelchina Glacier (across from Eureka) and the long Heavenly Ridge off the toe of the glacier; the next glacier visible to the east is Tazlina Glacier. This area was once part of a route miners used to traverse glaciers to Valdez; some folks still make the trek on snowmachines.
--Outhouse rest area near Mendeltna Creek around mile 160 if needed (not on the Bell's map)
Fuel up options: Glennallen Fuel @ mile 187 Glenn Hwy before the junction (south side of hwy, old-timey gas station/garage, pay at the pump 7 days/wk, plumbed restrooms) or Chistochina @ mile 33 Tok Cutoff (summer hours 7am-9pm Mon-Sat) which is much more scenic and "old school" Alaska, and possible lunch stop-
Various outhouses along the way (see Bell's travel map linked above).
--Possible Lunch stop: 4 hours drive from Anchorage puts you around Chistochina where you'll find a really spectacular view of the Wrangells and Chistochina River near its confluence with the Copper River - the best photo spot is from the bridge but the parking area with outhouse is just before the bridge, could be a lunch stop; Posty's Trading Post gas station in Chisto is a "quaint" place with plumbed restrooms, a small general store, and good selection of native AK crafts/beadwork https://www.facebook.com/PostysNativeGiftShop/ with picnic tables on a lawn in summer.
--Interpretive sign and pullout near mile 56 offers exceptional photo opportunities of the Wrangell Mtns and headwaters country of the Copper River; notable views of the Tanada Peaks and Capital Mtn .
The volcanoes of the Wrangell Mountains
Mount Sanford is the tallest of the western Wrangell volcanoes at 16,237 feet (4,949 m), the 13th highest peak in North America. It is a complex shield volcano that first formed about 900,000 years ago. The latest eruption is estimated to have been between 320,000 and 100,000 years ago. Like Drum, Sanford has a large icefield above 8,000 feet (2,400 m) that feeds a series of glaciers.[43] Capital Mountain is located near Mount Sanford, but is much smaller at 7,731 feet (2,356 m) in height. It is a shield volcano, about 10 miles (16 km) in diameter. Its summit has collapsed to form a caldera roughly 2.5 miles (4.0 km) in diameter.
Tanada Peaks on left and Sanford on the right
Skookum Volcano
The Skookum Creek Volcano is a volcanic center that has been heavily eroded. It was active between 3.2 million and 2 million years ago. 7,125 feet (2,172 m) high at its highest point, the old shield volcano has been severely eroded. Its caldera is surrounded by a series of dacite and rhyolite domes. Mount Jarvis is a shield volcano. 13,421 feet (4,091 m) high, with one or more indistinct summit calderas. It is covered with ice and erupted between 1.7 million and 1 million years ago.[46] Mount Blackburn is at 16,390 feet (5,000 m) the highest point in the Wrangells, the 12th highest peak in North America, and the oldest volcano in the range. It is a shield volcano with a filled caldera that was active between 4.2 million and 3.4 million years ago. Mount Blackburn is ice-covered and is the source of Kennicott Glacier and Nabesna Glacier, among others.[46] The Boomerang volcano is a very small shield volcano, only rising 3,949 feet (1,204 m). It is at least one million years old and is overlaid by deposits from Capital Mountain.*
-- Stop at NPS Ranger Station in Slana to pick up audio tour if not already downloaded from: https://www.nps.gov/wrst/learn/photosmultimedia/audio-tours.htm The ranger station is small, with a few interpretive items and usually friendly rangers, and an outhouse nearby.
--Enjoy a leisurely drive of the Nabesna Road (we're developing content to fill in around this text https://www.nps.gov/wrst/planyourvisit/nabesna-road-guide.htm ) with stops at waysides near miles 16 and 17 for a great view of a lake very reminiscent of (Wonder Lake and Denali) with Tanada Peaks and Mount Sanford instead; the wayside at mile 18 to view the geology of the Mentasta Mountains (outhouse).
Trail Creek (approximately 1 mile from the lodge)
Quick (or more leisurely depending on time table) "hike" (walk) and wildlife viewing at Twin Lake / Kendesnii campground. Kendesnii is the Ahtna name of Daisy Nicolai, an Athabaskan woman who had a spring camp with her children in the area for many years near the turn of the 19th-20th century. Much more info on the traditional uses of the land available if you're interested in talking about various points along the Nabesna Road in terms of indigenous and European cultures in the area.
