For determination of sources and levels of soil contaminants around Scott Base
Description:
SS14 T3; 8m southwest of the pump shed and 1.5m from the wet lab on a disturbed fill surface
Altitude:
6 m
Aspect:
NE
Slope:
2 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
77° 51' S 166° 46' E
Latitude Longitude DD
-77.850 166.767
Latitude longitude precision DD
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:
30 cm
Frozen type:
Ice-cemented
Frozen comment:
30
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:
Some small salt efflorescences; foreign materials include wood fragments, nails and various other debris
Soil
Soil parent material:
Fill materials from local volcanic materials formed for the purpose of landsurface reshaping and general landscaping
Previous disturbance:
The land surface has been reshaped for the purpose of landscaping and improving accessibility around Scott Base