Snow Observations List

Got ECTP10/11 in a pit on an east facing slope at 9100'. The snowpack is about 60cm deep, with 30cm of facets and 30cm of fist to 4 finger hardness new snow . The test failed at the interface of the old facets and new snow. 

We decided to keep the skiing to below 30 degrees. After skiing one slope and skinning back up, we noticed widespread cracking around our ski tracks (image), but luckily the terrain was mellow enough that nothing moved. 

From IG on 12/10: "2 slides we triggered remotely in tepee yesterday"

We (a group of 4) skinned up Lionhead Ridge from the ID/MT border and found troubling conditions. Several small whoomphs were observed in the shallower, bushy snow at lower elevations, and we had a massive (~100-foot propagation) whoomph on the ridge proper where the cornice met the ridge. Accompanying those whoomphs, we observed shooting cracks at multiple low-angle locations. We performed 3 separate pits, the shallowest of which was 48cm @8113' and had an ECTP10. The next two pits were 65cm deep and the SnowPilots are attached. Every single pit had sizeable (~3mm) basal faceting and a pencil-hard ice layer sandwiched with more facets above in the lower snowpack. While cutting a PST, the entire column propagated (Q1) above the ice layer at 25cm from the ground. Be careful out there, the snowpack is super touchy. 

From text message: "The attached picture is a little slide that went off when I was doing small turns on an adjacent slope. That's Beaver Slide! There was more small slides south in the trees. Heard whumphing here and there."

Was splitboarding up near lions head ridge today. Made some bad decisions and kicked off a good slide in a NE facing chute. Was with 2 buddies, 1 of which skied the line 3 weeks ago.  Underneath about a foot of new powder snow there was a firm crust that seemed like it was old  hard windslab in the gut of the chute, and I think a sun crust on the riders left side(East aspect). We had 2 spots where we were planning to re group at, first was a small cubby area right before a slight rollover about 75 ft from the top. I dropped first, made some turns down toward the pulloff, as I pulled in, I triggered a good size slab that propagated maybe 40-50 ft across, at the rollover as I carved into the pulloff.  Pulled  all snow  out of the chute down to the ground. Seemed to have failed on sugary facets on ground/ice crust close to the ground... 

Went into the Lightning/Taylor Creek area of the Southern Madison’s in search of some powder skiing with the new snow. On our ascent toward Woodward Mountain via the backside, we found fresh snow varying from 2 inches at the trailhead to foot deep lightly drifted areas in the upper elevations. In the protected low angle gully we ascended this new snow sat atop either rocks or a very stout wind crust. The latter of which made for great skiing. We descended Woodward top down and assessed the possibility of thin (3”) wind slabs being reactive on the stout wind crust as the Woodward side seemed to have received a lot more loading from the storm’s E winds. As we rolled over to slightly steeper terrain, I noticed the snow stiffening just below my skis and gave it a few hops where I intentionally popped the pictured slab. With this information, we decided to carefully traverse to more protected trees and descend via a less wind loaded and hazardous route. We ski cut from tree to tree triggering a few more of these very small slabs before finding wonderful powder skiing lower on the mountain where the wind had significantly less effect. 
 

All of the slabs were 1 to 4 inches deep and propagated 5 to 15 feet wide. None of them possessed the mass or were on steep enough terrain to overcome and slide over the stauch wall. Overall was a great lesson in mitigating hazard and we were rewarded with some great turns. 

Went for a ski tour in the Southern Madison's up Lightning Creek in search of a deeper snowpack. Our tour brought us up Woodward Mountain via the E sub-ridge with a plan to ski in the bowl to the north on a NE aspect. The snowpack varied immensely due to sun effect/wind loading but overall found 50-60 cm of snow in the deeper locations. We performed 3 CTs in representative locations of our intended ski line and had results of CT21 Q2, CT15 Q2, and CTN. The columns broke on a layer of 4F facets midway down from the surface. Combining this data with a lack of other signs of instability (cracking, whumpfing, recent avalanches, recent loading), we decided to ski our intended line. 

Snow quality on the ascent and decent varied from "ripple pow" to breakable wind crust to unbreakable wind crust. Overall, was a great day in the BC getting familiar with our early season snowpack even though good ski conditions lacked.