Medicine Bow Nordic Ski Patrol
Patrol Log: Sunday, February 29, 2004: R. Howell
On Sunday February 29 Bob Howell skied the Libby Creek Loop. I met two
other people along the trail, although, from the tracks it was clear
several others had covered the loop earlier in the day, after last night's
snow.
Conditions were mostly overcast, with the wind initially almost calm, but
strong by mid afternoon. The trail was in good shape with approximately 4
inches of new snow overnight. The snow stake near the start of the trail
showed 39 inches. A few rocks were close to the surface on the part of the
trail which descends to Libby Creek after the hairpin turn.
I dug a snow pit at 13T 397980 4576751 (NAD 27) at an elevation about 9640
ft, slightly uphill from the lower part of the trail, below the open slopes
and cliffs on the north side of Libby Creek. It was on a 22 deg. slope
facing 142 degrees (SE).
The snow depth was 120 cm and the air temperature was -5C (23F).
layer height Temp. Hardness Crystal structure
# cm C
------ 120-----------------------------------------------------------------
9 110 -3.0 fist fresh 1.0 mm A few dendrites, but
powder mostly cemented clusters
of 0.1 mm crystals or
spheres (rime?)
----- 103-----------------------------------------------------------------
8 100 -3.0 pencil ice crust 3.0 mm welded ice crystals
----- 98-----------------------------------------------------------------
7 4 fingers hoar? 1.0 mm slightly rounded
more faceted than #6
----- 94-----------------------------------------------------------------
6 90 -3.0 2 fingers 1.0 mm rounded grains,
slightly faceted
----- 81-----------------------------------------------------------------
5 80 -2.5 2 fingers icy 2.5 mm welded ice crystals
----- 76-----------------------------------------------------------------
4 4 fingers 1.5 mm faceted, with edges
slightly rounded
----- 73-----------------------------------------------------------------
70 -2.0 1.5 mm faceted, with edges
3 60 -2.0 2 fingers slightly rounded
----- 51-----------------------------------------------------------------
2 50 -1.5 3 fingers softer hoar? 1.5 mm faceted
----- 47-----------------------------------------------------------------
40 -1.5
30 -1.0 depth hoar 3.0 mm faceted
1 20 -1.0 1 finger but consolidated
10 0.0
------ 0 -0.5 ---------------------------------------------------------
Shovel stability test: It required very light force to cause the top layer
of powder to slide on the icy surface of layer #8. Once that ice layer was
cut through it required moderately light force to produce a shear at the
top of the next major ice layer (#5) at 81 cm. Finally, it required
moderate force to produce shear at the top of layer #1 at 47 cm.
Summary: Several ice crust layers have developed because of periods of
little snow, especially #8 at 98-103 cm. and they represent potential
sliding surfaces. Some type of soft hoar has also developed below the ice
layers. Right now the unconsolidated powder on top of the upper most ice
layer (#8) is relatively shallow, but with continued accumulation and
drifting that could change.
The car counts were as follows. The Corner Mountain and Little Laramie Lot
counts are for 8:45 AM. The others are from 10:00 AM, as I spent some time
with the First Aid class at the Ski Area before the above patrol.
with without
trailers trailers
Corner Mountain Lot 0 0
Little Laramie Lot 0 0
Below Cattleguard 25 1
Cattleguard to Turnaround 27 0
Green Rock Picnic Gnd. Lot 0 4
P. G. to Snowy Range Lodge 18 8
Total 70 13
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Page last modified March 1, 2004
Comments/Additions/Corrections to hamannj@trib.com