About 150m northeast of the old Marble Point camp site; a largely boulder free knoll
Altitude:
65 m
Aspect:
W
Slope:
4 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 25' 12" S 163° 41' 42" E
77° 25.12' S 163° 0.00' E
Latitude Longitude DD
-77.4200 163.6950
-77.41867 163.0000
Latitude longitude precision DD
0.00015 0.00015
0.00008 0.0008
Locality
Marble Point region, western McMurdo Sound just east of the Wilson Piedmont Glacier, between Marble Point and Gneiss Point
Survey
Marble Point Quadrangle, US Geological Survey, 1975
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
54 cm
Frozen type:
Hard ice-cemented
Frozen comment:
54cm
Geology
Geological setting:
The land surface is an undulating till plain formed by retreat of the Wilson Piedmont Glacier; The Marble Point region is an old landscape, as evidenced by deposits of phillipsite, buried soils and oxidised gneiss, which have been covered by advances of the grounded Ross Ice Shelf; later ice retreat and glaciological features have been controlled by changes in the stranded Wilson Piedmont Glacier; the till mantle is patchy and dominated largely by locally occurring rocks; gneiss bedrock outcrops locally
Patterned ground:
Nil
Surface weathering or surface features:
Some oxide staining on surface gneissic boulders; subrounded and exfoliating
Soil
Soil parent material:
Marble/gneiss till over gneissic bedrock; upper horizons pale but lower horizons somewhat browner, perhaps related to bedrock weathering