Observation: Provo Peak 3/2/2010

Observer Name: 
Patterson
Region: 
Provo
Provo Canyon
Provo Peak
Observation Date: 
03/02/2010
Location or Route: 
Sqauw Peak Road-Provo Peak
Weather
Sky: 
Broken
Wind Direction: 
South
Wind Speed: 
Light
Weather Comments: 

 High clouds all day with patches of blue sky above.  Winds were light out of the South.  warm.  measured +1C around 1pm.  Sun was not getting through and affecting snow surface.  heating kept in check by high clouds.  

Snow Characteristics

Snow Surface Conditions: 
Dense Loose
Wind Crust
Snow Characteristic Comments: 

 Mixed bag out there.  most aspects had a temp/sun crust except due north where some small grained 1-2mm surface hoar existed and dense settled pow.  

Primary Concern

Primary Concern: 
Persistent Slabs
Probability: 
Moderate
Aspect: 
North
Elevation: 
Mid
Low
Trend: 
Same
Primary Concern Comments: 

 Mostly concerned with the lingering surface hoar instabilities out there.  2 buried layers from the 10th and 17th of February are a concern in the Provo area mountains.  I was curious to see which layer was more reactive today.  

snow_profile_location: 
Comments - Photos - Videos (group 1)

 On my way in to Provo Peak i noticed what appeared to be a natural on an east aspect at a lower elevation.  It didn't look like a very deep avalanche, but what was interesting was how far it propagated.  It's speculation, but likely that surface hoar was the culprit.  

DSC02068.JPG
Printer-friendly version
Comments - Photos - Videos (group 2)

 Dug a hole around 9800', NNW aspect, 34 degrees.  I was able to pop out a surface hoar layer with a tilt test easily.  Now the question was whether it was the 2/17 layer or the 2/10 layer?  A compression test pulled it out again with 14 taps, Q1, and when the block slide out, a clean shear broke out beneath it.  Easy to see that the upper layer was the 2/17 SH, and the lower one the 2/10 layer, both 2-3mm crystals.  Continued tests revealed the 2/17 layer to be more reactive, mostly with Q2 failures.  This follows with what I have been seeing in the Provo area mountains over the last couple of weeks.  Good propagation as well on the 2/17 layer, with an ECTP17 Q2.  The structure here is poor due to these surface hoar layers, but they don't feel completely reactive right now.  That could change if the forecasted Thurs/Fri. storm verifies.  The question looms...do these layers exist up high?  

Slide1.jpg
Comments - Photos - Videos (group 3)

 Visual of the 2/17 and 2/10 surface hoar layers from a second compression test

DSC02087.JPG
Comments - Photos - Videos (group 4)
DSC02079.JPG
Observed Danger Rating: 
Moderate
Forecast Danger Rating: 
Moderate

Site Built by Dharmatech
Site Refresh by Flint Creative