Soil contamination and environmental process evaluation; sampled to determine contaminant movement by heavy metals from surface copper wire
Description:
Old Marble Point construction camp site, approximately 50m north of Surko Stream, in the heavily disturbed area; much of the area has been modified by attempted burial of the trashed camp site
Altitude:
60 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 25' 31" S 163° 41' 20" E
77° 25.31' S 163° 0.00' E
Latitude Longitude DD
-77.4253 163.689
-77.42183 163.0000
Latitude longitude precision DD
0.00015 0.0015
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:
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
Patterned ground:
Nil
Surface weathering or surface features:
Copper artifacts have oxide coating
Soil
Soil parent material:
Sandy gravel till from predominantly marble and gneiss
Previous disturbance:
Considerable ground surface disturbance from tracked machinery during earlier site clean up; a major USA cleanup of the area in 1998/99