About 20m west of the Marble Point air facility building, near the edge of a bulldozer track and near the edge of a pond which receives wastewater runoff
Altitude:
75 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 25' 25" S 163° 41' 2" E
77° 24.85' S 163° 0.00' E
Latitude Longitude DD
-77.4236 163.6840
-77.4142 163.0000
Latitude longitude precision DD
0.0009 0.00015
0.0004 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:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
The land surface is a gently 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; the pond may be an artificial feature that receives local thaw runoff
Patterned ground:
Nil
Surface weathering or surface features:
Precipitated deposit
Soil
Soil parent material:
A single surface sample of precipitated salt like material with a yellowish colour from near the edge of the pond
Previous disturbance:
Vehicle tracking and chemical contamination from site activity
Soil weathering stage:
Soil moisture status:
Oceanic subxerous,
Biological activity:
Nil observed at site
Profile Description
Horizon
Depth
Description
576a
0 – 5 cm
yellow (5Y 7/8) gravelly sand with abundant crystalline precipitate,