Walcott Bay, to the northeast of the Howchin Glacier; approximately 1km east of the Howchin Glacier on a long ridge surface; a rocky knoll about 10m below the crest of the ridge
Altitude:
800 m
Aspect:
SW
Slope:
3 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
78° 11' S 163° 27' E
78° 11' S 163° 24' E
Latitude Longitude DD
-78.183 163.450
-78.183 163.400
Latitude longitude precision DD
0.008 0.008
0.008 0.008
Locality
Royal Society Range; Transantarctic Mountains
Survey
Ross Island & Vicinity, Antarctica, 1:250 000 US Geological Survey, 1986
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-23
°C
Frozen ground depth:
45 cm
Frozen type:
Frozen comment:
45cm
Geology
Geological setting:
Basement rock is gneiss; on some ridge surfaces till is thin or absent; there is strong physical disaggregation along the joint planes which are nearly vertical
Patterned ground:
Nil
Surface weathering or surface features:
Strong joint plane surface crumbling and disaggregation; some weak to moderate surface staining; carbonate coatings beneath some clasts; sand infilling in cracks may aide bedrock fragmentation through wedging processes
Soil
Soil parent material:
Disaggregating and fractured gneissic bedrock with sand infilling along fracture planes
Oceanic subxerous; snow is patchy on the ridge surface; the site is dry but the soil is moist below the surface
Biological activity:
Some green algae in patches beneath light coloured rocks
Profile Description
Horizon
Depth
Description
553a
-2
–
0
cm
surface stones, dominantly tabular forming a moderately developed pavement; larger rock particles angular to subangular and non to weakly oxidised; smaller particles mainly subrounded and unoxidised,
553b
0
–
19
cm
dark greyish brown (10YR 4/2) granular sand in fractured bedrock clefts; loose; some carbonate and a few silt coatings; rock particles varied petrologically; mainly subrounded and unstained; distinct boundary,
553c
19
–
45
cm
very dark greyish brown (2.5Y 3/2 moist) sand with some fragmented bedrock in bedrock clefts; moderately cohesive; smaller particles mainly rounded to subrounded and unstained; sharp boundary, on hard ice-cemented ground