Gore-Tex, we’ve all heard of it, but what exactly is it, and do we really need it? It has become almost a generic term for a line of advanced technology fabric systems, that when it comes to ski jackets and pants, is one reason why “shells” are now so popular. Because of materials like Gore-Tex, layering, or the ability to add or shed inner layers, translates to all day comfort. Since the outer shell is your first line of defense, it only makes sense to choose something that will not only keep you warm, but also cool. Thankfully, some relatively new high-tech fabrics known as microporous membranes provide just the solution.
While bindings aren’t nearly as sexy to talk about as skis or boots, they are your direct connection to the ski and the only piece of gear, besides a helmet, that is engineered with your safety as the foremost concern. Like everything else these days, they have become ever more complicated with a confusing array of applications, styles, and choices. Modern binding designs now accommodate a variety of different on-hill applications. These designs offer a range of boot movement from none on alpine bindings, to always on telemark bindings, and everything in between. So to help sort it all out, consult Binding Tech 101 and become the expert!
You are likely most familiar with standard alpine “Din” style bindings. These bindings are designed to offer zero boot mobility and have independent heel and toe pieces which are either mounted flat or integrated. This means they are screwed directly onto the ski or mounted on a sliding platform or track integrated into the ski and sold as a package by the manufacturer. There are pros and cons for each. Flat mount can be lighter, tighter, closer to the ski, and you can use the binding of your choice. Integrated bindings can usually offer a bit of fore/aft mounting flexibility and no drilling means easy set-up, easy to move, and easy to sell with no holes. As far as height off the ski goes, height is considered good and riser plates are sometimes added on narrow carving skis for added leverage and to avoid “boot out” where the edge of the boot can actually come in contact with the snow at high edge angles. Lower is usually considered better on wider skis.

Ever wonder how steep the slope is you’re skiing or riding? There’s a good chance it’s not even close to how steep you think it is.
Read more courtesy of www.onthesnow.com…
Tuesday 2/26/13 is travel day. Planes, trains, and automobiles. Okay, maybe just an airport train, but three of us make the trip to Mt.Bachelor, OR from Phoenix, AZ. Although connecting flights are available to Redmond, near the resort, we plan to meet in Eugene and take the two hour drive from there. Ron A. gets a head start and takes United through San Francisco. He grew up in Eugene and raced at Bachelor for his high school ski team back in the ‘70s. Ron L. and I take USAirways to Portland where you can connect with numerous 30 min. shuttle flights to Redmond or Eugene. After a bite to eat and groceries in Eugene, we hit the gas pedal and head for the high country.
Sitting in the Cascade Range just west of Bend, Mt. Bachelor is actually an active volcano with numerous steam vents that can be seen around the runs. It is basically a 3,365’ high cratered cone, about 60% above timberline, with a very consistent fall line. According to wikipedia, with a total lift-accessible area of 3,683 acres, it is the second largest single-mountain ski resort in the US behind Vail, and the sixth largest of all ski resorts in the nation. The resort boasts a lift-served vertical drop of 3,300’ with ten chairlifts, seven of which are express quads with slick electronic scanning systems.











