Approximately 600m SW of the S end of the Marble Point runway and 75m N Surko Stream; at the old Marble Point camp site; on ground that had been bulldozed to remove debris from the old camp site; the sample location was at the N edge of a crushed lead acid battery and 30cm further away
Altitude:
60 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
Yes
Latitude Longitude DMS
77° 25.19' S 163° 41.04' E
77° 25.5' S 163° 42.0' E
Latitude Longitude DD
-77.41980 163.68400
-77.425 163.700
Latitude longitude precision DD
0.00008 0.00008
0.004 0.008
Locality
Marble Point, western McMurdo Sound
Survey
USGS Antarctica Topographic Series 1:50,000; Marble Point, Antarctica
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 surface is a gently undulating till plain formed by retreat of the Wilson Piedmont Glacier; the Marble Point region is an old landscape, with 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; granodiorite, granite, marble, gneiss, and dolerite; the surface has been disturbed by mechanical activity
Patterned ground:
Nil
Surface weathering or surface features:
Some white salts beneath battery fragments
Soil
Soil parent material:
Sandy gravel till, probably disturbed from predominantly gneiss, marble and granodiorite with artefacts from earlier site occupation
Previous disturbance:
Widespread disturbance from camp site activity and subsequent attempts at site clean up; this site previously sampled on 23/1/1990
Nil at site but mosses and cyanobacteria abundant in moist sites nearby
Profile Description
Horizon
Depth
Description
643a
0 – 5 cm
Edge of crushed lead battery; olive (5Y 5/3) sandy gravel; loose; rock particles angular to subangular, some weakly stained; a few carbonate coatings indistinct boundary,
643b
10 – 15 cm
olive (5Y 5/3) gravelly sand; loose; rock particles angular to subrounded; indistinct boundary,
643c
20 – 30 cm
olive (5Y 5/3) sandy gravel; loose to weakly cohesive; weakly developed vesicular structure; rock particles angular to subrounded 30cm away,