I went out to McGee Mountain and skinned up the low angle east facing panel above round valley. The goal was to track the 3/19 interface to 9000′ and see if the same problemtaic layering that has been reported from areas south of Bishop is present.
Clear skies, calm winds, cool temperatures.
9000′:
NE: Ski 5cm, Boot 20cm, HS 335cm, 3/19 interface down 50cm no MFcr. No persitent grains at interface. Interface unreactive in Compression Test. All results resistant planar
E: Ski 0cm, Boot 10cm, HS > 300cm, 3/19 interface down 70cm Strong 10cm MFcr. No persitent grains at interface. Interface unreactive in Compression Test. All results resistant planar
ENE: Ski 15cm, Boot 25cm, HS >300cm, 3/19 interface down 55cm. Weak MFcr. No persitent grains at interface. Interface unreactive in Compression Test. All results resistant planar
8000′:
NE: 5- 10cm breakable wind board over 10cm decomposing and fragmented precip. particles. Secondary grain type is rounding near surface facets. 1mm max size.
SE: Wafer thin sun crust on the surface of the wind board.
N: Effcient travel in 10cm of settled snow with a bit of recrystallization.