Posted tagged ‘White River Glacier’

Kohnstamm Memorial Trail?

October 27, 2019
Entering the Kohnstamm Memorial Wilderness

When President Barack Obama signed the Omnibus Public Lands Management Act of 2009 into law on March 30, 2009, more than a dozen new pocket wilderness areas and additions to existing wilderness were created around Mount Hood and in the Clackamas watershed. 

Among these, the Richard L. Kohnstamm Memorial Area expanded the Mount Hood Wilderness to the east of Timberline Lodge to encompass the White River canyon, extending from Mount Hood’s crater to about the 5,000 foot level, including a segment of the Timberline Trail and Pacific Crest Trail that traverses the canyon. This wilderness addition was created to “recognize the balance between wild and developed areas in the national public lands system and to create a tribute to the man who saved Timberline Lodge.”

The wilder side of the Timberline area is now the Kohnstamm Memorial Area, an extension of the Mount Hood Wilderness just east of the lodge

Richard Kohnstamm was the longtime force behind the RLK Company, operators of the Timberline Resort, which has a permit to operate the historic Timberline Lodge, which in turn is owned by the American public. 

After his duty as a gunner during World War II, Kohnstamm returned home to earn his masters degree in social work from Columbia University. After college, he moved to Portland to take a job at a local social services non-profit. Soon after arriving here, he made a visit to Timberline Lodge, where he was immediately taken with the beauty of the massive building. 

Richard Kohnstamm at Timberline in 1957 (Oregon Encyclopedia)

But Kohnstamm saw a tarnished jewel, as the lodge had quickly fallen into disrepair following its construction by the Works Progress Administration in 1937. The Forest Service had revoked the operating permit for the lodge and was looking for a new operator, and so began the Kohnstamm era at Timberline. By all accounts, he did, indeed, save the lodge. 

Kohnstamm soon teamed with John Mills to found the Friends of Timberline, a non-profit dedicated to preservation of the history, art and architecture of the remarkable building. The unique partnership between the Forest Service, Friends of Timberline and the RLK Company to preserve the lodge in perpetuity continues to this day, and is known as the Timberline Triumvirate. 

Today, the lodge continues to thrive, and summer resort operations have now expanded to include a controversial bike park centered on the Jeff Flood chairlift. After years of legal challenges, the RLK Company build miles of bicycle trails descending from main lodge to the base of the lift, where cyclists can load themselves and their bikes for a quick ride back to the top. 

The Timberline Resort’s new bike park opened this summer (photo: Timberline)

It’s a high-adrenaline activity made easy, with no hills to climb. But the development of this new attraction underscored the fact that the Timberline resort operators and Forest Service have done little over the decades to enhance the hiking experience around the lodge, despite plenty of demand. 

The reason is pretty obvious: hikers don’t buy lift tickets. Yes, some hikers help fill the hotel rooms in summer, and still more stop by to support the restaurants in the lodge, but filling ski lifts continues to the focus at Timberline.

Bikes riding the Jeff Flood lift back to the lodge (photo: Timberline)

Today, hikers at Timberline are limited to walking along the Timberline Trail or hiking the Mountaineer Trail, a semi-loop that climbs to a lift terminal, where it dead-ends at a dirt service road. Hikers usually follow the steep, dusty road back to lodge to complete a loop.

But perhaps the Richard L Kohnstamm Memorial Area could be inspiration for the Forest Service and RLK Company to bring new trails to the area, and a create a more welcoming trailhead for visitors who aren’t staying at the lodging or paying to ride the resort lifts? In that spirit, the following is a concept for a new trail that would be an instant classic on the mountain, rivaled only by the popular Cooper Spur Trail on Mount Hood’s north side for elevation and close-up looks into an active glacier.

Proposal: Kohnstamm Glacier View Trail

The proposed Glacier View Trail would climb the broad ridge that separates the White River and Salmon River canyons, just east of Timberline Lodge. The new trail would begin just across the Salmon River from the lodge, at a junction along the Timberline Trail, and end at Glacier View, a scenic high point on the ridge between the Palmer and White River glaciers. 

This viewpoint is already visited by a few intrepid explorers each year for its spectacular views into Mount Hood’s crater and the rugged crevasses of the White River Glacier. The schematic below shows how the new route would appear from Timberline Lodge:

(click image to enlarge)

Another perspective (below) of the proposed trail shows the route as it would appear from further east along the Timberline Trail, where it travels along the rim of White River canyon. This angle also shows the tumbling descent of the White River Glacier and the steep west wall of the canyon that would provide several overlooks from the new trail:

(click image to enlarge)

Thanks to the gentle, open terrain, the new trail would climb in broad, graded switchbacks, eventually reaching an elevation of 8,200 feet. This is just shy of the elevation of Cooper Spur, and would make the Kohnstamm Glacier View Trail the second-highest trail on the mountain.

The viewpoint at Glacier View (below) is already marked by a stone windbreak built by hikers that complements several handy boulders (below) to make this a fine spot for relaxing and taking in the view.

End of the trail at Glacier View (photo: Google)

From the Glacier View viewpoint, Mount Hood’s crater and the upper reaches of the White River Glacier (below) are surprisingly rugged and impressive, given the generally gentle terrain of Mount Hood’s south side. From this perspective, the Steel Cliffs and Crater Rock dominate the view as they tower over the glacier.

Mount Hood’s crater and the upper reach of the White River Glacier from Glacier View (photo: Google)
White River Glacier from Glacier View (photo: Google)

But the scene-stealer is the White River Glacier, which stair-steps down a series of icefalls directly in front of Glacier View (below), providing a close-up look into the workings of an active glacier. Lucky hikers might even hear the glacier occasionally moving from this close-up perspective as it grinds its way down the mountain.

Crevasses in the White River Glacier below Glacier View (photo: Google)

The view to the south from Glacier View (below) features the long, crevasse-fractured lower reaches of the White River Glacier, and below, the maze of sandy ravines which make up the sprawling White River Canyon. The deserts of Eastern Oregon are on the east (left) horizon from this perspective, and the Oregon Cascades spread out to the south.

The view down the White River Canyon from Glacier View (photo: Google)

The hike to Glacier View from Timberilne Lodge on the proposed Kohnstamm Trail would be about 2.5 miles long, climbing about 2,300 feet along the way, and would undoubtedly become a marquee hike on the mountain, if similar trails like Cooper Spur and McNeil Point are any gauge. But the backlog of trail needs at Timberline extend beyond having a marquee viewpoint hike like this. 

The Kohnstamm trail concept therefore includes other trail improvements in the Timberline area that would round out the trail system here. The following schematic (below) include building a new 1.4 mile trail from the upper stub of the Mountaineer Trail to Timberline Lodge, allowing hikers to complete the popular loop without walking the dusty, somewhat miserable service road below Silcox hut, often dodging resort vehicles along the way.

(click image to enlarge)

The broader Kohnstamm trail concept also calls for using the east parking area as a day-hiking hub in the summer months, with clearly marked trailheads that would consolidate the maze of confusing user trails that are increasingly carving up the wildflower meadows here. The new hub would also include restrooms, interpretive displays, picnic tables and other hiker amenities that would make for a better hiking experience.

Time for a makeover? Abandoned lift terminal at the proposed trail hub

A more ambitious element of the concept is to convert the neglected bones of an abandoned lodge structure (above) at the east parking area to become a hiker’s hut where visitors could relax after a hike, fill water bottles or learn about hiking options from Mount Hood’s volunteer trail ambassadors. 

This element might even tempt the Timberline resort operators to help make these trail concepts a reality if it offered an opportunity to provide concessions to hikers. After all, hiking is the fastest growing activity on the mountain (and on public lands), not skiing (or even mountain biking). Creating a hiking hub could be an opportunity for the Timberline operators to evolve their future vision for the resort to better match what people are coming to the mountain for.

What would it take?

Trail building is typically heavy work that involves clearing vegetation and building a smooth tread where rocks and roots are the rule. But the proposed Kohnstamm Trail would be very different, as the entire route is above the tree line and would be on the loose volcanic debris that makes up the smooth south side of Mount Hood. Trail building here would be much simpler, from the ease of surveying without trees and vegetation to get in the way, to actual trail construction in the soft soil surface. For these reasons, much of this work would be ideal for volunteers to help with.

In reality, the greatest obstacles to realizing this concept would likely be regulatory. Convincing the Forest Service to permit a new trail would be a tall hurdle, in itself. But if the Timberline resort operators were behind the idea, it would almost certainly be approved, especially if the resort embraced building and maintaining the trail hub improvements. Who knows, maybe they will even spot this article..?

Author’s Confessions…

As a postscript, I thought I’d post a few confessions from days of yore. I grew up in Portland and began skiing at Timberline Lodge as a tiny tot. I continued to avidly ski at the Mount Hood resorts for many years until giving up alpine skiing in the early 90s, largely in response to the expansion of the Meadows resort into lovely Heather Canyon, a deal-breaker for me. I loved the sport, but saw the beauty of the mountain under continual threat from the resort operations — and still do. Today, I make due with snow shoes and occasional trips on Nordic skis, though I do miss the thrill of alpine skiing!

The author skiing Timberline in 1978

An earlier awakening for me came in 1978, with the construction of the Palmer Lift at Timberline. This lift completed Richard Kohnstamm’s vision for year-round skiing on the mountain. But it was the first lift on Mount Hood to climb that far above the tree line, and was an immediate eyesore. Sadly, the conversion of the Palmer Glacier to become plowed rectangle of salted snow (see “Stop Salting the Palmer Glacier!”) that can be seen for miles completed the travesty.

That Palmer Lift debacle was soon followed by an even more egregious lift at Mount Bachelor, one that I wrote about 37 years ago in this (ahem!) riveting bit of self-righteous student journalism! (below)

(click image to enlarge)

When I stumbled across this old clipping from my days as a columnist at the Oregon State University student newspaper, I initially winced at the creative flourishes (…hey, I was 20 years old!). But my sentiments about these lifts — and the Heather Canyon lift at Meadows — remain unchanged. They were a step too far, and represented a real failure of the Forest Service to protect the mountain from over-development.

That said, I do believe the ski resorts can be managed in a more sustainable way that doesn’t harm the mountain. We’re certainly not there yet, and because all three of the major resorts (Timberline, Ski Bowl and Meadows) all sit on public land, I believe we all have a right to help determine that more sustainable future. 

In this article, I’ve made a case for accommodating more than just lift ticket purchasers in the recreation vision at Timberline Lodge. In future articles I’ll make the case for rounding out the mission for the other resorts in a way that meets the broader interests of those of us who own the land.

White River Buried Forest

September 18, 2011

The summer of 2011 will be remembered as the year of the Dollar Lake Fire in the Mount Hood area, as much of the north side is still smoldering from a lightning-caused wildfire that ignited on August 26. Though a calamity to those who loved the verdant forests on Mount Hood’s northern slopes, the fire is a blip on the screen when compared to the many explosive events that have rearranged the mountain’s forests and topography over the millennia.

Among the most recent and fascinating of these events are the Old Maid eruptions. These explosions knocked over entire forests on the mountain’s south side like matchsticks, burying them under a deep layer of ash and volcanic debris. This article describes the Old Maid events, and how to see traces of their aftermath today.

The Old Maid Eruptions

While most tourists at Timberline Lodge on a given day are blissfully unaware that Mount Hood is living volcano, the occasional, heady odor of sulfur fumes blowing down from the crater are a reminder the “quiet” spell we are enjoying is only temporary.

[click here for a larger version]

In geologic terms, the Old Maid eruptions are incredibly recent, finally winding down in our recorded history of the early 1800s. The events are named for Old Maid Flats, the debris plain created by the eruptions in the Sandy River canyon, though the impact on the mountain was much broader.

Scientists have determined the Old Maid eruptive period to have occurred within from about 1760 to 1810 A.D. In fact, when Lewis & Clark described the shallow “quicksand” delta of the Sandy River in 1804-05, they were looking at volcanic sediments that had only recently flooded down the river from the active slopes Mount Hood.

The former floor of the White River canyon is visible as a thin layer of oxidized soil, dotted with mummified trees.

The scientific accuracy of these dates is made possible by thousands of mummified trees swept over by the Old Maid debris flows, and later exposed by streams cutting into the sediments. The White River buried forest is one of the more prominent locations where these flattened forests and the former valley floor can plainly be seen.

The Old Maid eruptions originated in the modern crater of Mount Hood, where sulfur fumes still rise from the vents known as the Devils Kitchen. The massive, 800-foot volcanic dome of Crater Rock, itself, is just 200 years old and formed during these eruptions. The heat of rising magma in the crater eventually sent pyroclastic flows down the Sandy and White River canyons — rolling clouds of super-heated ash and debris that buried the entire landscape.

A closer look at the buried valley floor reveals mummified trees.

The Old Maid eruptions deposited about one hundred feet of debris throughout the upper White River canyon, filling the formerly U-shaped glacial valley with a flat fan of volcanic boulders, cobbles and fine ash. The outflow from the White River Glacier has since carved deeply into the debris flow, revealing the old valley floor and some of the thousands of mummified trees knocked over by the Old Maid event.

A flat-topped ridge in the middle of the White River canyon known as Mesa Terrace (see earlier schematic) is a remnant of the debris flow that shows the original depth of the debris above the valley floor.

Close-up of an entire tree, tipped over and buried where it fell on the former valley floor.

Two types of debris flow swept down the southern slopes of Mount Hood during the Old Maid eruptions. The most destructive were the pyroclastic flows, which many of us are familiar with from the colossal Mount St. Helens eruption of May 18, 1980.

In addition to the hot pyroclastic flows, cooler mudflows from flash-melted glaciers and snowfields also swept down Mount Hood’s south slopes during the Old Maid events. We know the buried forests at the bottom of White River Canyon fell victim to these mudflows, as pyroclastic flows would have instantly incinerated the standing timber. Instead, the cooler debris flows simply knocked the forests over, and buried them under layers of mud and debris.

Scientists believe these trees were partially buried, then broken off by subsequent flows.

Scientists believe the old valley floor now being revealed by erosion was of glacial origin, dating back to the last major glacial advance of the White River Glacier some 10,000 years ago. Thus, forests grew undisturbed along the former valley floor of the White River for a very long time.

Hiking to the Overlook

Hiking to the White River buried forest overlook is easy and scenic, as well as historic and iconic: it follows Mount Hood’s famous Timberline Trail for 0.7 miles to the impressive rim of the White River canyon. This section of trail also serves as the Pacific Crest Trail, the 2,000-mile epic trek from Mexico to Canada.

To find the trailhead, park in the lower, overflow lot located to the east of Timberline Lodge. Park near a gated dirt on the west side of the parking area. Follow this old road steeply uphill for about 200 yards to an obvious junction with the Timberline Trail, and turn right (or, if you’re coming from the lodge, follow any of the trails beyond the lodge uphill to the Timberline Trail and turn right). The Timberline Trail quickly traverses into a side-canyon, crossing the headwaters of the Salmon River.

Next, the Timberline Trail rambles across pumice-covered slopes and soon reaches a sign marking the Richard L. Kohnstamm Wilderness, created in 2009 as an addition to the wilderness complex that encircles Mount Hood. Kohnstamm was the resort operator responsible for resurrecting a struggling Timberline Lodge in the 1950s, and setting the resort on the successful path that it continues to enjoy today.

[click here for a larger, printable map]

Beyond the wilderness boundary, the trail descends across another pumice slope, then drops more steeply on a surface of loose glacial till as it traces the west moraine of the White River canyon. Soon, you will reach the overlook where the Timberline Trail follows the moraine crest, and arrives at a stand of trees. This is a good spot to stop and take in the scenery, and especially to pick out the signs of the buried forest, at the bottom of the canyon, below.

The south-facing slopes and open terrain can make this a hot, dusty hike in late summer, so be sure to carry water. You will also want a pair of binoculars to view the buried forest details more closely. If you have the time and energy after visiting the buried forest overlook, you can retrace your step to the dirt access road, then turn right and follow it to Silcox Hut, about 0.8 miles from the trailhead. The hut was the original upper terminal for the first Magic Mile ski lift in the late 1930s, and today is maintained as an historic structure.

New Glaciers on Mount Hood?

July 19, 2009

WhiteRiverNewGlacier01

It seems implausible, but climate change may be creating new glaciers on Mount Hood — but not in the usual way that glaciers are created. A close look at the retreating White River Glacier on the sunny south flank of Mount Hood reveals two stranded arms that are now separate glacier. As marked by (1) and (2) on the photo, above, a pair of truncated mini-glaciers have been cut off from the main flow of the White River Glacier by a previously hidden moraine that is now being exposed by the rapidly retreating ice.

Until fairly recently in geologic time, the White River Glacier extended far beyond its current extent, flowing down the rugged canyon shown in the photo for several miles to a terminus far beyond where Highway 35 now crosses the glacial outwash plain. But the glacier is retreating rapidly, destabilizing the canyon and changing its shape as it shrinks.

A closer look at two mini-glaciers on Mount Hood

A closer look at two mini-glaciers on Mount Hood

A closer look at the two mini-glaciers reveals why a glacier is different from a static field of ice. Glaciers flow under their own weight, sending waves of ice sliding downward as more snow is added, above. Huge cracks known as crevasses form at stress points in the river of ice, and these are a defining feature in identifying a glacier. Both of these sheets of ice have crevasses, and thus are moving glaciers.

A look at the topographic map shows how the extent of the White River Glacier has changed as recently as the 1960s, when the map was surveyed. The mini-glacier marked as (1) was clearly an arm of the White River Glacier until very recently, but surprisingly, the second mini-glacier (2) appears to already have separated from the main glacier before the surveys were done — though it is clearly a truncated lobe of the main glacier, as well.

WhiteRiverNewGlacier03

Another defining feature for this pair of mini-glaciers is that the emerging moraine that divides them from the main glacier also divides their outflow. They feed a separate branch of the White River from the main stem – another argument for recognizing these glaciers as discrete, perhaps?

It is logical to assume that these little glaciers are doomed by the same forces of climate change that created them, but there is a twist that just might keep them flowing — and perhaps thriving — as a result of climate change. While scientists believe that snow levels will rise in the Cascades over the next century, they also believe that precipitation will increase.

That could mean that in the highest elevation areas where winter precipitation still falls mainly as snow could actually see glaciers grow in depth, but perhaps not in length, since freezing levels would be higher. Therefore, if these mini-glaciers are high enough on the mountain, they may well survive, or possibly even grow, thanks to increased snowfall at this elevation.

If these glaciers are new, and independent of the White River Glacier, they deserve some respect, since all known glaciers in Oregon have been formally named. And that brings us to a bit of history surrounding this flank of the mountain. For here, on the upper slopes above these little glaciers, the first attempts on Mount Hood’s summit were made by early white settlers.

A close-up view of the mini-glaciers reveals classic crevasses

A close-up view of the mini-glaciers reveals classic crevasses

The first man in this story is Thomas Jefferson Dryer, the colorful publisher of the Weekly Oregonian in the mid-1800s (pictured below, on the left). Dryer claims to have been the first white man to climb the mountain, in August 1854. Dryer’s description of the climb makes it clear that he did not reach the true summit, though he may well have reached the top of the Steel Cliffs, only a few hundred feet below the summit — and an amazing achievement for the day.

Dryer complicated his case by embellishing the story with outrageous exaggerations — being able to see Mount Shasta (not possible) and peaks in the Rockies (definitely not possible), and his climbing companion bleeding form his skin from the extreme altitude (not very likely). But Dryer was also the first white man to climb Mount St. Helens, so his story must be taken with some degree of faith.

Dryer’s account wasn’t challenged until three years later, when one of his employees, Henry Lewis Pittock, made the first documented ascent of Mount Hood on August 6, 1857. The Pittock party made the climb along what is now the traditional southern route, skirting the west edge of the White River Glacier, and climbing through the crater. When Pittock’s party made claim to being the “first” to summit the mountain, it set off a dispute with Dryer over the veracity of his own account that continues to this day.

Thomas Jefferson Dryer (left) and Henry Lewis PIttock

Thomas Jefferson Dryer (left) and Henry Lewis PIttock

In 1861, Dryer was tapped to serve in the Lincoln administration, and turned the Weekly Oregonian over to Pittock, to whom he owed a significant debt in the form of back pay. Pittock, in turn, converted the weekly into a daily and was soon publishing the predominant newspaper in the region, today’s daily Oregonian.

Pittock is now recognized as the first white man to summit Mount Hood, but like Dryer, doesn’t have a landmark in his name to record his place in history (though Portlanders are quite familiar with the iconic mansion he built atop the West Hills).

So I offer a modest proposal: honor both men for their historic climbs, with the western mini-glacier (1) named for Pittock, representing his more westerly approach, and the eastern mini-glacier named for Dryer, who may have even walked on this ice sheet in his own attempt at the summit. Both men deserve to be remembered for their part in Mount Hood’s history, and these little glaciers deserve some respect, too.