Approximately 3km S of Sponsors Pk and 5.5km NE of Lake Vashka; a broad sloping surface forming part of a ridge and gully complex formed in an exposure of marble bedrock
Altitude:
1025 m
Aspect:
SE
Slope:
8 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
77° 18.6' S 161° 23' E
Latitude Longitude DD
-77.3100 161.383
Latitude longitude precision DD
0.0008 0.008
Locality
Victoria Land, Trans-antarctic Mountains; in Upper Victoria Valley, part of the McMurdo Sound Dry Valley system
Survey
USGS 1:250 000 1986; Ross Island and Vicinity, Antarctica
Climate
Soil climate zone:
Central mountain
Estimated mean annual temperature:
-26
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Marble and hornfels dikes of the Ross Supergroup outcrop in the lower Barwick Valley above the level of Insel Drift; the surface cover is mainly thin disaggregated bedrock although occasional dolerite erratics are present
Patterned ground:
Surface weathering or surface features:
Marble outcrops have a thin crumbly surface; some cavernous weathering on bedrock; carbonate coatings occur beneath some surface stones;
Soil
Soil parent material:
Disaggregated marble with some inclusion of dolerite and sandstone aeolian or drift material
Xerous to subxerous; site is dry with little available moisture
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
144a
0 – 3 cm
strong brown (7.5YR 5/6) sandy granular pebble, mixed lithology gravel; weakly cohesive with a weakly developed surface crust; weakly developed vesicular structure; rock particles mainly subrounded and moderately stained; some marble fragments very soft; abrupt boundary,
144b
3 – 5 cm
strong brown (7.5YR 5/8) sandy granular pebble, mixed lithology gravel; loose; rock fragments subrounded to subangular and moderately stained; distinct boundary,
144c
6 – 15 cm
yellowish brown (10YR 6/8) granular marbley sand; sharp boundary, on compact marble