

This dog is always down for a ride up the canyon.Above photos by - Sean O'brien.
PHOTO MOSAIC AND WANDERING WORDS - By B. Eliot

We happened upon #374 in the mountains just above Sylmar (All of the CA condors are tagged). He soared over us while we were parked and eating a little lunch and so we hopped in the truck and followed. Around a corner, he was just sitting in the road.


The daily commute.


Gi stops in for some liquid relief and relates a disturbing tale of romance gone awry.
Ski skins stick to the bottom of the ski and allow uphill travel using simple friction. The skins have thousands of tiny stiff fibers that lay almost flat, pointing toward the back of the ski.
As you slide the ski uphill, the snow glides over the fibers. When you step down, the thousands of fibers catch and stick (incredibly well) and keep you from sliding down.
For skins to work right, you need a free heel binding, using either telemark skiis, click-in alpine trekkers or AT bindings mounted to alpine skiis. Above, Travis shows off his Marker DUKE AT binding in free heel mode. These things work very well. It's just like uphill cross country skiing.
Bridger Bowl opened it's boundaries this season. Something I had always wished and hoped for when I lived in Bozeman.
The fun begins once you're through. 

Travis skins up to Bradley Meadows. Hidden chute, the Apron and Northwest Passage loom above.


We trekked for about 15 minutes until we arrived about halfway up, to the base of "the ramp," A terrain feature most easily distinguished from within the ski area boundaries. It is a ramp like mountain slope that maintains a moderate pitch, all the way to the top of the ridge.
At the top of our trek, Travis dug an avalanche pit to gauge the quality of the snowpack. 2009 has been a particularily bad snowpack season because the first few snowfalls put about 12 inches of very granular, almost sand like snow as the base layer. This is the worst possible condition for snow pack and avalanches because a granular base layer is like a layer of small ball bearings, just waiting to roll the entire season's snowpack down the hill. This is very dangerous and has been the cause of many avalanche related deaths this year.
The snow at our particular location and slope angle was stable and skiable. We would stick to 40 degrees and less, and stay off exposed and wind battered slopes. Anything steeper than 40 degrees would be much more risky.
Travis dug the pit and isolated the layers of snow. The process is like taking a core sample from antactica, you could see all of the storms that have occured over the course of last 3-4 months. The snowpack measured about 210 cm to the ground.
(You can see the G3 skins on the bottom of my skiis.)

Travis, just before dropping into China bowl. This is the reward.
One week after a storm, we still can find pockets of untracked powder.
And deeper into the trees, its as if we were the only ones on the mountain.
Ahhhh. Can't complain about 6 inches of fresh snow.
Two other guys were busy taking it to the next level. Accessible from "The Ramp" just outside the north boundary, these guys came down above "Northwest" into a chute with two technical rock sections. The first snowboarder that came down didn't leave much snow for his skier buddy. The guy in the picture is the skier, watching his buddy take the sluff and most of the fun with him. 


It was a time to relax, slow down, and hang out with an old friend.

This was taken just minutes before I had some of the most gravitationally challenging moments of my life.