Soil contamination and environmental process evaluation; sampled to determine contaminant at the site of a rubbish fire
Description:
100m north of Surko Stream at the old Marble Point construction camp site, on the northeastern side, light to moderate surface disturbance, possibly related to ground scraping and permafrost retreat; the site of an old rubbish fire
Altitude:
60 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 25' 23" S 163° 42' 22" E
77° 25.21' S 163° 0.00' E
Latitude Longitude DD
-77.4231 163.7060
-77.42017 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:
57 cm
Frozen type:
hard ice-cemented
Frozen comment:
57cm
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
Patterned ground:
Nil
Surface weathering or surface features:
Considerable salt precipitation at the soil surface; nails and other artifacts are oxidised
Soil
Soil parent material:
Sandy gravel till from predominantly marble and gneiss with ashy material at the soil surface
Previous disturbance:
Probably some ground scraping and disposal of debris by burning