For determination of sources and levels of soil contaminants around Scott Base
Description:
SS7 T1; 7.7 m southeast of the south corner of the incinerator building and 1 m from a container; an uneven sloping fill surface
Altitude:
6 m
Aspect:
SE
Slope:
11 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 51' S 166° 46' E
77° 51' S 166° 48' E
Latitude Longitude DD
-77.850 166.767
-77.850 166.800
Latitude longitude precision DD
0.008 0.008
0.008 0.008
Locality
Pram Point, Scott Base
Survey
not recorded
Climate
Soil climate zone:
Coastal mountain
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
40 cm
Frozen type:
Hard ice-cemented
Frozen comment:
40
Geology
Geological setting:
The materials comprise volcanics of the McMurdo Volcanics Formation mainly as scoriaceous lava flows; the surface materials are a thin cover of mainly fractured bedrock with addition of some glacially derived granular and pebble clasts from outside the immediate area; the volcanic bedrock has been considerably fractured by patterned ground freeze thaw; the surface age is probably very late Pleistocene (Ross Sea Glaciation) having been modified by McMurdo Sound filling glacial ice
Patterned ground:
Nil
Surface weathering or surface features:
The surface has not been recently disturbed; some thin patches of salt are present at the soil excavation site
Soil
Soil parent material:
Fill materials derived largely from earlier landsurface scraping and landscape tidying; includes abundant foreign materials including wood, metals, plastic etc.
Previous disturbance:
Mechanical disturbance resulting from land surface reshaping; primarily a built up area