Accident: Yamaha Hill 12/30/2008

Observer Name: 
Craig Gordon
Observation Date: 
12/31/2008
Occurrence Date: 
12/30/2008
Occurrence Time: 
Unknown
Region: 
Yamaha Hill
Moffit Basin
Uintas
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Location

40° 52' 19.1568" N, 110° 58' 26.4576" W
Avalanche Characteristics
Elevation: 
10100'
Aspect: 
Northeast
Slope Angle: 
36
Trigger: 
Snowmobiler
Trigger: additional info: 
Unintentionally Triggered
Avalanche Type: 
Hard Slab
Weak Layer: 
Facets
Depth (avg): 
4'
Width: 
600'
Vertical: 
500'
People Involved
Caught: 
1
Carried: 
1
Fully Buried: 
1
Killed: 
1
Accident & Rescue Info
Accident & Rescue Summary: 

Details are still being sifted through, but what we know is this- a father and his three sons left the Bear River Service trailhead and rode their snowmobiles towards the Moffit Basin and ultimately landed near Yamaha Hill. Hayden Ellingford waited at the bottom of the slope as one of the riders from the group took a bite low on the slope above him, triggering a large avalanche. An organized outside rescue party found the man at approx. 17:54. He was not wearing a beacon nor did any members in his party have rescue equipment.

Terrain Summary: 

Yamaha Hill is a Northeast facing, open slope with very little vegetation in the main part of the bowl. The starting zone averages 32 degrees in steepness with several small mid slope breakovers measuring 36 degrees. The terrain is typical of many slopes in the western Uintas. Broad, flat windward ridges allow winds to transport a tremendous amount of snow even while it’s relatively calm in neighboring mountain ranges.

Weather & Avalanche History: 

Avalanche Data: The avalanche averaged 4’ in depth, was 600’ feet wide, running for about 500’ vertically. Classified as a HS-AM-D2-R3-O/G. The avalanche failed on a thin layer of faceted snow above the Thanksgiving raincrust.

Weather and Snowpack History: The western Uinta snowpack is historically plagued by cold temperatures, shallow snow depths, very weak snow and strong winds… at face value, this year was no different. October was unusually dry and warm, though winter got rolling with an Election Day storm which deposited several feet of snow to the upper elevations. A warm, dry November followed rapidly settling total snow depths to about a foot. All south facing aspects shed their winter coat and reverted back to grass and bare rock. Two inches of snow fell on the evening of Friday November 29th.  However the bigger news was November went out with a bang of sorts. A moist, misty northwest flow moved into the region on the afternoon of November 30th and rain fell to the highest peaks forming an unusually stout raincrust which still plagues our snowpack.  

A colder northwest flow followed, ushering in December with a small storm depositing 3” of snow and strong ridgetop winds on Dec. 2nd followed by another quick hitting system on Dec. 8 with 8” of snow. Very strong prefrontal southwest winds raked the upper elevations on the evening of Dec. 12, gusting into the 70’s along the high ridges and peaks. Nearly a foot of light density snow fell overnight, overloading the fragile weak layers of the pack. The Dec. 13 advisory warned of the possibility of slabs breaking to the ground  on old layers of snow and test slopes confirmed our suspicions. Another 8” of snow fell on Dec. 16th.  An Avalanche Warning went into effect on the morning of Dec. 20 as new snow and hurricane force prefrontal winds continued to overload the structurally challenged snowpack. While the warning expired, a HIGH avalanche danger remained at the upper elevations, especially on north facing slopes that held snow during the November dry spell. A powerful Pacific system moved into the region on the 22nd depositing 16” of snow, followed by the Christmas storm which walloped the area with an additional 2’. Water totals were just over 2” in seven days. The Avalanche Warning remained in place through Dec. 27th and was downgraded to a Special Avalanche Advisory on the 28th. However, we strongly worded the advisory cluing people into the severity of the conditions and the consequences of triggering large, dangerous and possibly unsurvivable slides on slopes approaching 30 degrees in steepness.

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