Sandy Glacier Caves: Realm of the Snow Dragon

The Sandy Glacier is front and center in the classic view of Mount Hood from Lolo Pass

The Sandy Glacier is front and center in the classic view of Mount Hood from Lolo Pass

Oregon Public Broadcasting’s venerable Oregon Field Guide series kicks off it’s 25th season in October with a remarkable story on the hidden network of glacier caves that have formed under the Sandy Glacier, high on Mount Hood’s west flank.

In the video preview (below), Oregon Field Guide executive producer Steve Amen says that “in the 25 years we’ve been doing Oregon Field Guide, this is the biggest geologic story that we have ever done”. This is bold statement from a program that has confronted all manner of danger in documenting Oregon’s secret places!

Glacier caves are formed by melt water seeping through glaciers and flowing along the bedrock beneath glaciers. Over time, intricate networks of braided tunnels can form. Because a glacier is, by definition, a river of moving ice, exploring a glacier cave is inherently dangerous — and this is what makes the upcoming Oregon Field Guide special so ambitious.

Otherworldly scene from Oregon Field Guide's upcoming "Glacier Caves" special (Brent McGregor/OPB)

Otherworldly scene from Oregon Field Guide’s upcoming “Glacier Caves” special (Brent McGregor/OPB)

Cave explorers have been actively exploring and mapping the extent of the Sandy Glacier caves for the past three years. This previously unknown network of caves has been dubbed the Snow Dragon Glacier Cave System by cavers Eduardo Cartaya, Scott Linn and Brent McGregor in July 2011. Cavers have since surveyed (to date) well over a mile of caves in the network, with parts of the cave system nearly 1,000 feet deep.

Ice Cave or Glacier Cave? Here in volcano country, it’s worth noting that a glacier cave is different than an ice cave. Where a glacier cave has roof of glacial ice, an ice cave occurs where persistent ice forms inside an underground, rock cave. In the Pacific Northwest, we have several examples where ice has accumulated inside lava tubes to form true ice caves, such as the Guler Ice Cave near Mount Adams and Sawyer’s Ice Cave in Central Oregon.

To date, the Snow Dragon cave network consists of three caves that intersect, dubbed the Snow Dragon, Frozen Minotaur, and Pure Imagination caves. Within these caves explorers have discovered a fantastic landscape of streams and waterfalls flowing under a massive, sculpted ceiling of ice.

The caves are punctuated by moulins (pronounced “MOO-lawn”), or vertical shafts in the ice formed by meltwater. Some of these moulins are dry, some are still flowing, and a few have have grown to become skylights large enough serve as entry points into the cave system for daring explorers.

Caving expeditions to the Sandy Glacier caves by the National Speleological Society (NSS) in 2011 and 2012 were featured in the February 2013 NSS News, with a dramatic photo of colossal moulin on its cover. These volunteer expeditions included NSS geologists, glaciologists, spelunkers, scuba divers and mountain climbers who spent eight days documenting the cave system from a base camp high atop the Sandy Glacier.

Sandy Glacier caves on the cover of the National Speleological Society News earlier this year

Sandy Glacier caves on the cover of the National Speleological Society News earlier this year

According to the NSS explorers, the Snow Dragon cave complex is the largest ice cave complex in the lower forty-eight states, and one of the largest in the world. To date, these explorers have found icy passages ranging from huge, ballroom-sized open spaces with 40-foot ceilings to narrow, flooded crawl sapces only a few feet high, and passable only with diving gear.

The Oregon High Desert Grotto, an affiliate of the NSS, has posted a series of fascinating maps documenting their explorations on their website.

The Story Behind the Sandy Glacier Caves?

Glacier caves typically form near the snout of a glacier, and explorers simply follow the outflow stream into the cave system. Such was the case with Paradise Ice Caves at Mount Rainier (now disappeared) at the terminus of the Paradise Glacier. More recently, hikers have explored the outflow opening at the Sandy Glacier, as well.

Topographic map of Mount Hood's west flank and the Sandy Glacier

Topographic map of Mount Hood’s west flank and the Sandy Glacier

[click for a larger map]

The Snow Dragon caves under the Sandy Glacier are different, however. While the glacier does have an outflow opening to the cave system, the cave network extends far beyond the terminus of the glacier, apparently reaching almost to the headwall, nearly a mile away and almost 2,500 feet above the terminus in elevation. The scale and scope of these caves seems to be partly the result of the glacier shrinking, and not just the effects of melting near the terminus of the glacier.

This broader phenomenon first became apparent when a huge moulin — known informally to many hikers as the “glory hole” and formally named the Cerberus Moulin by cavers — appeared in the glacier a few years ago. The Cerberus Moulin is plainly visible to hikers from nearby McNeil Point, which also serves as the jump-off point for explorers.

The Cerberus Moulin is located along the lower, receding edge of the Sandy Glacier

The Cerberus Moulin is located along the lower, receding edge of the Sandy Glacier

A closer view of the Cerberus Moulin in the Sandy Glacier

A closer view of the Cerberus Moulin in the Sandy Glacier

The following photos of the Sandy Glacier were taken nine years apart, in 2003 and 2012, and show the startling retreat of the glacier over just the past decade. The Cerberus Moulin had not yet formed in the 2003 photo, but is plainly visible in the 2012 image. For reference, the broad moraine to the left of the Cerberus Moulin is labeled as (A) in the photos:

Sandy Glacier in 2003

Sandy Glacier in 2003

Sandy Glacier in 2012

Sandy Glacier in 2012

The photo comparison shows big changes in the activity of the glacier, too. What was once an icefall near the terminus of the glacier (B) in 2003 has since receded to the point that the rock outcrop that was beneath (and formed) the icefall is now exposed in the 2012 image. Likewise, the lower third of the glacier (C) was clearly crevassed and actively moving in the 2003 image compared to the 2012 image, where an absence of crevasses shows little glacial movement occurring today in this section of the glacier.

The rapidly shrinking glacier could be an explanation for the relative stability and remarkable extent of the caves underneath the ice. The increased melting is sending more runoff through and under the glacier, helping to form new moulins feeding into the ice caves.

The slowing movement of the lower portion of the glacier could also help explain why the cave network has become so extensive, as more actively flowing ice would be more likely to destroy fragile ice caves before they could become so extensive and interconnected.

Part of a Larger Story

The Sandy Glacier Caves discovery is really part of the much larger story of Mount Hood’s rapidly shrinking glaciers. After millennia of relative stability, we are witnessing broader changes to the landscape surrounding in response to the retreat of the glacial ice.

The downstream effects in recent years from Mount Hood’s melting glaciers have been startling, and the Sandy Glacier is no exception. Sometime during the winter of 2002-03, a massive debris flow was unleashed from just below the terminus of the Sandy Glacier, and roared down the Muddy Fork canyon. The wall of mud and rock swept away whole forests in its wake, burying a quarter mile-wide swath in as much as fifty feet of debris.

Looking across the 2002-03 Muddy Fork debris flow

Looking across the 2002-03 Muddy Fork debris flow

The view (above) looking across the 2002-03 Muddy Fork debris flow shows toppled trees at the margins, while the forests in the main path of the flow were simply carried away.

The view downstream (below) from the center of the debris flow shows the scope of the destruction, with the debris at least 50 feet deep in this spot where the Timberline Trail crosses the Muddy Fork.

Looking downstream from the middle of the 2002-03 Muddy Fork debris flow

Looking downstream from the middle of the 2002-03 Muddy Fork debris flow

The Muddy Fork has only recently carved its way down through the 2002-03 debris to the original valley floor, revealing mummified stumps from the old forest and visible giving scale to the scope of the event (below).

Seven years after the 2002-03 flow, the Muddy Fork had cut a channel down to its original elevation, revealing the full depth of the flow.

Seven years after the 2002-03 flow, the Muddy Fork had cut a channel down to its original elevation, revealing the full depth of the flow.

These stumps of trees snapped off by the 2002-03 debris flow have reappeared where the Muddy Fork has carved down to the original river level.

These stumps of trees snapped off by the 2002-03 debris flow have reappeared where the Muddy Fork has carved down to the original river level.

With no way to know how long Mount Hood’s glaciers will continue to retreat, catastrophic events of this kind will recur in the coming decades. Runoff from the retreating glaciers will continue to carve away at newly exposed terrain once covered by ice, with periodic debris flows occurring as routine events.

In November 2006, another major flood event in the Sandy River canyon caused damage even further downstream, in the Brightwood area, where private homes line the Sandy River:

Damage from the 2006 flood was still being repaired when yet another major storm burst stormed down the valley in January 2011. During this event, a large section of Lolo Pass road briefly becoming part of the Sandy River, and scores of homes were cut off from emergency responders:

The 2011 event washed out the south approach to the Old Maid Flat Bridge over the Sandy River, forcing the Forest Service to jury-rig a temporary ramp to the bridge. The entire crossing has since been replaced, but like all repairs to streamside roads around the mountain, there is no reason to assume that another event won’t eventually destroy the new bridge, too.

The Old Maid Flat Bridge over the Sandy River was repaired with a temporary approach ramp (on the right in this photo) where the bridge approach had washed out by raging water

The Old Maid Flat Bridge over the Sandy River was repaired with a temporary approach ramp (on the right in this photo) where the bridge approach had washed out by raging water

The two homes in the distance barely survived the 2011 flood event on the Sandy River

The two homes in the distance barely survived the 2011 flood event on the Sandy River

This wider view shows the rebuilt section of Lolo Pass Road that was briefly a channel of the Sandy River during the January 2011 flood

This wider view shows the rebuilt section of Lolo Pass Road that was briefly a channel of the Sandy River during the January 2011 flood

Similar events have occurred over the past several years on the White River, Ladd Creek, East Fork Hood River and the Middle Fork Hood River. The predicted climate changes driving these events give every indication that we will continue to watch similar dramatic changes unfold around Mount Hood in decades to come.

The November 2006 debris flows in the White River canyon buried Highway 35 in boulders (ODOT)

The November 2006 debris flows in the White River canyon buried Highway 35 in boulders (ODOT)

During the 2006 debris flows, the old White River Bridge was completely inundated, leaving an eight-foot layer of boulders on the bridge (ODOT)

During the 2006 debris flows, the old White River Bridge was completely inundated, leaving an eight-foot layer of boulders on the bridge (ODOT)

By late 2012, the Federal Highway Administration had built a new, much larger bridge over the White River designed to survive future debris flows

By late 2012, the Federal Highway Administration had built a new, much larger bridge over the White River designed to survive future debris flows

Just as the wildfires that burned through forests on the eastern and northern flanks of Mount Hood over the past few years have given us new insights into the cycle of forest renewal, the unfolding geological events linked to changing glaciers provide a similar opportunity to better understand these natural processes, too.

While these destructive events are tragic to our sentimental eyes, the rebirth of a forest ecosystem is truly remarkable to witness — as is the discovery of the Sandy Glacier ice caves in the midst of the larger decline of Mount Hood’s glaciers. All of these sweeping events are reminders that we’re just temporary spectators to ancient natural forces forever at work in shaping “our” mountain and its astoundingly complex ecosystems.

So, stay tuned and enjoy, this show is to be continued!
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OPB Airing Dates

Here are the broadcast dates for the Oregon Field Guide premiere:

• Thursday, October 10 at 8:30 p.m. on OPB TV
• Sunday, October 13 at 1:30 a.m. on OPB TV
• Sunday, October 13 at 6:30 p.m. on OPB TV

For fans of the show, a 25th Anniversary retrospective will also be airing on Thursday, October 3rd. You can learn more about OFG and view their video archive on their website.
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October 4th Postscript

Author with Brent McGregor on October 4

Author with Brent McGregor on October 4

In the small world department, I had the honor of meeting epic caver, climber and photographer extraordinaire Brent McGregor on the Timberline Trail this afternoon. He and caving partner Eric Guth had spent the night near the entrance to the Snow Dragon Glacier Cave!

After learning a LOT more about the Snow Dragon cave complex from Brent today (and having my jaw drop repeatedly as I heard about their exploits under the glacier!), I’ve updated the above article — including the more accurate use of the name Cerberus Moulin in lieu of the generic “glory hole” nickname that some hikers have been using.

Brent also pointed me to a couple fascinating new videos from OPB that just add to the anticipation of the Glacier Caves premiere on OPB:

Behind the Scenes of Glacier Caves: Mt. Hood’s Secret World

Special Glacier Caves website from OPB

And finally, one more link: the Glacier Caves OPB documentary will be screened in a free, special preview on October 9th at the Hollywood Theater. Here’s the link to the event Facebook page:

Glacier Caves Special Preview

Thanks for the terrific conversation, Brent – great meeting you and Eric!

Proposal: Viento Bluff Trails

Looking west from the summit of Viento Bluff

Looking west from the summit of Viento Bluff

This is the third in a series of new trail proposals for Oregon State Parks land in the Columbia Gorge. This article follows previous proposals for a Bridal Veil Canyon Trail and Angels Rest Loop. All three have the potential to fit into the Oregon State Parks and Recreation (OSPRD) master planning for the Columbia Gorge that is happening right now.

Like the Angels Rest Loop and Bridal Veil Canyon proposals, this trail would be aimed at families, vacationing visitors to the region and those trying out hiking for the first time. Unlike the earlier proposals, the Viento area is little known to most who visit the Gorge. For a moderate effort, this proposal would provide explore the unique, transitional ecosystem found in the mid-section of the Gorge, as well as some sweeping views and towering cliffs.

Trail map of the proposal

Trail map of the proposal

(Click here for a larger map)

The Viento proposal stitches together several rustic service roads that already exist with new trail segments that would take hikers to three separate, cliff-top viewpoints. All three viewpoints rise high above the popular campgrounds at Viento State Park, and would provide an excellent, moderate hiking challenge for campers and day-visitors, alike.

The map above shows the proposed network of trails, and the oblique view, below, gives a sense of the steep topography that would make the Viento area so interesting as a hiking destination.

Perspective view of the proposal

Perspective view of the proposal

(Click here for a larger map)

The proposed Viento Bluff trails would also build on a planned extension of the mostly-complete Historic Columbia River Highway (HCRH) State Trail, providing bike-and-hike opportunities along this emerging, world-class facility. A six-million dollar extension of the trail will soon extend east from the Viento Trailhead to Perham Creek, completing another link in a route that will eventually extend from Troutdale to The Dalles.

A bit of history on the name “Viento” is in order. While the word means “windy” in Spanish — an often fitting name for this narrow spot in the Gorge — the name was actually coined in the 1800s for an early railroad stop in the area using the first two letters from the surnames of railroad builder Henry Villard, one of his investors, William Endicott, and a local railroad contractor named Tolman (the origin of the name and other local history can be found on an interpretive display near the entrance to Viento State Park).

The following is a detailed description of the three viewpoints that make up the Viento Bluffs and proposed trails that would lead to them.

Viento Bluff Trail

Viento Bluff is a familiar landmark to those traveling I-84

Viento Bluff is a familiar landmark to those traveling I-84

The main focus of the proposed trail network is Viento Bluff, the most prominent of the rocky outcrops that rise above Viento State Park, and a familiar landmark to travelers passing through the Gorge.

While Viento Bluff rises as sheer, 300-foot vertical wall on its north face, the steeply tilted basalt flows that form the bluff have a relatively gentle, meadow-covered south slope. The proposed summit trail would circle the bluff to reach this southern approach.

Historic CCC path along Viento Creek

Historic CCC path along Viento Creek

The trail would begin at the existing day use parking area at the Upper Viento Campground, initially traveling on an existing footpath that follows Viento Creek into its shady, forested canyon. Here, the project would consist of a new footbridge connecting the existing trailhead to the old footpath, and improving the existing tread to basic trail standards.

Historic CCC path

Historic CCC path

The existing footpath appears to be one of the many vestiges of the Civilian Conservation Corps (CCC) in the Viento area. The CCC was created by Franklin D. Roosevelt as part of his Great Depression-era “New Deal” to put young men to work making infrastructure improvements to public lands across the country.

Several stone retaining walls in the area, the original (upper) Viento campground and a collapsed campground water house still remain from the CCC period. The surviving footpath originally led to the water house, but now terminates at its moss-covered ruins, along a pretty section of Viento Creek.

Remains of the old CCC water house along Viento Creek

Remains of the old CCC water house along Viento Creek

From near the end of the existing footpath, the proposed route would turn east, climbing the slope to Viento Bluff in an easy traverse along a heavily used game trail. The deer and elk have done a find job in this section, with a grade that works well as a hiking trail!

Game trail leading from Viento Creek to the bluff

Game trail leading from Viento Creek to the bluff

Soon, this game trail reaches a forested saddle behind Viento Bluff, and enters one of the most lush, abundant stands of poison oak anywhere in the Gorge — one of the few obstacles to realizing the Viento Bluffs trail.

While it’s an ominous sight for anyone sensitive to poison oak, routing a trail to the bluff through this section would be less difficult than appearances might suggest. The open, meadow-covered south slope of the bluff is only about 20 yards beyond the poison oak section, so the exposure would be no more than many trails in the Gorge that pass through poison oak patches. But it would need to be built carefully, and maintained accordingly.

Poison Oak heaven in the saddle south of Viento Bluff!

Poison Oak heaven in the saddle south of Viento Bluff!

From the saddle, the route reaches the stuff of a dirt service road approaching from the east (more about that in a moment), and from this point, the proposed summit trail would begin an exceptionally scenic ascent of Viento Bluff’s south slope, traversing a steep meadow in switchbacks through scattered White Oak and Ponderosa Pine.

The south slope of Viento Bluff as viewed from the East Bluff

The south slope of Viento Bluff as viewed from the East Bluff

The summit of Viento Bluff is exposed on three sides, with vertical drops into the forest below. If this were a remote wilderness viewpoint, simply terminating the viewpoint trail at the top would be safe enough. But because it’s a state park with families and less-experienced hikers, some sort of cable or wood railing would probably be needed here. The wood railings at the Bridal Veil State Park overlook might be a good model for this site, and easily constructed here.

Gorge panorama from Viento Bluff

Gorge panorama from Viento Bluff

The view from the summit of Viento Bluff is impressive, especially given the relatively moderate climb required. The rocky slopes of Dog Mountain dominate the view across the Columbia River, and the sweeping panorama extends as far west as Table Mountain and east to Mitchell Point and the town of White Salmon, beyond.

The summit is quite spacious, providing room for visitors to sit and spend some time taking in the scene or having a trailside picnic. It is also far enough above the busy river corridor to be largely beyond the noise of traffic, while still allowing for interesting views of trucks, trains and barges passing by in the busy transportation corridor provided by the Columbia River Gorge.

East Bluff Trail

The East Bluff as seen from Viento Bluff

The East Bluff as seen from Viento Bluff

The second trail in this proposal would lead from the Upper Viento Campground and trailhead to the East Bluff, an impressive basalt outcrop that is nearly as imposing as Viento Bluff. The East Bluff rises directly above I-84, yet is oddly less visible from the freeway, and therefore less familiar to travelers.

The route to the East Bluff would begin along the proposed extension of the HCRH State Trail, east of the Upper Viento Campground. From a point along the State Trail route, about one quarter mile beyond the campground, a primitive service heads south, climbing the steep ravine between the East Bluff and Viento Bluff. This spur road soon reaches in the power line corridor that crosses the saddle to south of the two bluffs.

Mitchell Point and White Salmon in the distance from the East Bluff

Mitchell Point and White Salmon in the distance from the East Bluff

From the saddle, one fork of the service road heads to the right, to Viento Bluff, as mentioned previously in this article. Along with the proposed new trail from Viento Creek, this route would create a loop hike to Viento Bluff, and a connection to the East Bluff (see map).

The left fork of the service road heads toward the East Bluff. This proposal calls for a new trail here, leaving the service road and traversing the open south slopes of the East Bluff in switchbacks.

The view west toward Dog Mountain and Stevenson from the East Bluff

The view west toward Dog Mountain and Stevenson from the East Bluff

The views from the East Bluff are expansive, encompassing the same stretch of the Gorge as the view from Viento Bluff, but including a unique perspective of Viento Bluff, itself.

The true summit of the East Bluff has a brass 1939 U.S. Geological Survey marker stamped “Viento”. The survey marker dates to the year when Bonneville Dam had just been completed, along with the old power line corridor behind the bluffs that took power from the new dam to Hood River and points east — likely the reason for a survey marker in this spot.

USGS marker on the summit of the East Bluff

USGS marker on the summit of the East Bluff

The summit of the East Bluff is quite broad, and even somewhat brushy in spots. But several dramatic viewpoints ring the edges — much like Angels Rest in the western Gorge, but with a lot less effort. Like Viento Bluff, the cliffs are extremely exposed, and would require some sort of cable or wood fencing, given the location in a state park and relatively easy access.

The loop connection to the proposed Viento Bluff trail (from Viento Creek) would allow for both summits to be included on a longer hike, or simply a hike around Viento Bluff for those who don’t want to climb the actual summit.

West Bluff Loop Trail

West Bluff from the Viento interchange

West Bluff from the Viento interchange

The third piece of the Viento proposal is a short loop trail to the west bluff, a basalt wall rising 250 feet above the Viento interchange and Upper Viento Campground trailhead.

The purpose of the West Bluff trail is to provide a more approachable destination for less ambitious or able-bodied hikers and families with small children. While not as imposing as Viento Bluff and the East Bluff, the West Bluff still delivers impressive views of the Columbia Gorge and an interesting, almost aerial view into the Viento Campground and interchange area, directly below.

This service road would form the east leg of the West Bluff trail loop

This service road would form the east leg of the West Bluff trail loop

The east leg of the loop would follow an existing dirt service road south from the existing trailhead, then fork uphill along a second service road that crosses within a few hundred yards of the West Bluff crest. A spur trail would climb the last stretch to the cliff-top viewpoints. Like the other summits, some sort of fence or railing would be in order here, as the cliffs drop over 200 feet to the trailhead below.

The west leg of the loop would be a new trail climbing a ravine directly below the West Bluff, connecting to the new summit spur. The complete West Bluff loop would cover less than a mile, and gain less than 300 feet elevation, yet give hikers a real sense of achievement. The West Bluff loop would also be the closest of the proposed trails to the main Viento Campground, so well situated to serve campers interested in a modest hike.

An interesting option for the West Bluff trail would be a barrier-free route. While this would be a much more substantial undertaking, it would be one of the few viewpoint trails in the Columbia Gorge available for visitors with limited mobility.

What would it take?

Much of this proposal builds on the repurposing of existing service roads to become wide trails — at least most of the time. The idea is to allow utility workers to access these roads when needed, but functioning as wide trails as their primary purpose. The service roads are owned and maintained by the Bonneville Power Administration (BPA), and see little use by the agency, so a shared purpose might be a way for the BPA to partner with Oregon State Parks to enhance and maintain these routes.

Historic retaining wall at Viento from the CCC era

Historic retaining wall at Viento from the CCC era

There are also several new hiking trail segments in this proposal. All would be straightforward to build, with few topographic or environmental obstacles. Because they are located in a highly accessible area (access from I-84), these new trails could be excellent candidates for construction by volunteer groups like Trailkeepers of Oregon.

Upper Viento Campground restroom is within a few yards of the trailhead

Upper Viento Campground restroom is within a few yards of the trailhead

The HCRH State Trail already has a major trailhead at Viento

The HCRH State Trail already has a major trailhead at Viento

One of the advantages of expanding hiking opportunities in the Viento area is the potential to take advantage of the existing recreation infrastructure: two campgrounds, a day use area, a large supply of trailhead parking, restrooms within a few yards of the trailhead, access to the HCRH State Trail and direct freeway access to I-84. Adding new trails to the area would simply make better use of these existing amenities in addition to enhancing the camping experience at Viento State Park.

What can you do..?

If you like this proposal, there is a unique opportunity to weigh in right now and make your voice heard: share your comments with Oregon Parks & Recreation Division (OPRD), the state agency that operates Viento State Park, and the sole agency responsible for trail planning in the park.

Seldom-seen rubber boa spotted along Viento Creek

Seldom-seen rubber boa spotted along Viento Creek

Over the next year the state is conducting a long-range planning effort to scope future recreation needs in the Gorge. [url]You can weigh in with your thoughts over here.[/url] So far, the State Parks have had fairly light participation in their public outreach, so it’s important to make your views known!

Please consider including links to the Veinto Bluffs, Bridal Veil Canyon and Angels Rest Loop proposals in this blog when you comment — here are the quick links to paste into your message:

https://wyeastblog.org/2012/01/15/proposal-bridal-veil-canyon-trail/

https://wyeastblog.org/2013/08/31/angels-rest-loop-one-way-trip-to-heaven/

https://wyeastblog.org/2013/09/22/proposal-viento-bluff-trails/

And as I’ve pitched in previous articles, please consider supporting Trailkeepers of Oregon, a non-profit, grass-roots organization that offers meet-up trail stewardship projects in the Gorge and around the region (full disclosure: the author is a founding and current board member of TKO and number one fan of the organization!)