Soil material examined in cracks in a very large granite boulder on rising undulating moraine on the north east side of Inexpressible Island
Altitude:
150 m
Aspect:
NE
Slope:
7 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
74° 53' S 163° 42' E
Latitude Longitude DD
-74.883 163.700
Latitude longitude precision DD
0.008 0.008
Locality
Inexpressible Island, Terra Nova Bay
Survey
USGS 1:250 000 1968; Mt Melbourne SS 58-60/9
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
0 NoObs
Frozen type:
Frozen comment:
NoObs
Geology
Geological setting:
Glacial till derived mainly from Granite Harbour Intrusives occurs extensively; a very large boulder, either bedrock or till derived, contained fine particle-sized material in rock cracks
Patterned ground:
Nil
Surface weathering or surface features:
Some fracturing of large boulders and slight wind rounding; some slight surface staining
Soil
Soil parent material:
Coarse sand and granule sized granite (with some metasedimentary) rock particles in a rock crack