A young surface at the north of Roberts Massif near Everett Nunatak
Altitude:
1950 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 29' S 177° 10' W
Latitude Longitude DD
-85.483 -177.17
Latitude longitude precision DD
0.008 0.08
Locality
Head of Shackleton Glacier at Roberts Massif, Queen Maud Mountains, on the edge of the Polar Plateau
Survey
USGS 1:250 000 1968; Liv Glacier SV 1-10/5
Climate
Soil climate zone:
Inland mountain
Estimated mean annual temperature:
-45
°C
Frozen ground depth:
0 NoObs
Frozen type:
NoObs
Frozen comment:
NoObs
Geology
Geological setting:
Dolerite and Beacon Group sediments outcrop on overridden surfaces while deposits of old lithified till containing Ferrar Dolerite also occur; the older lithified till may be Sirius Formation, considered to be related to the onset of glaciation in Antarctica in Oligocene or Miocene times;
Patterned ground:
Nil
Surface weathering or surface features:
Pockets of disaggregated older till are present where the surface is protected from erosion by wind
Soil
Soil parent material:
Pale greyish white disaggregated older lithified till
Previous disturbance:
Nil
Soil weathering stage:
6
Soil moisture status:
Ultraxerous, some patches of drift snow mainly behind larger boulders but no thawing
Biological activity:
Nil observed
Sample Data
Physical Data
Sample name
Depth description
Top (cm)
Base (cm)
Bulk Density
Dry Bulk Density
Gravimetric Moisture
Vol. Moisture (BD=2)
84
Sample solution chemistry
Sample name
pH
Na meq/100g
Ca meq/100g
Mg meq/100g
K meq/100g
Cl meq/100g
SO4 meq/100g
NO3 meq/100g
EC mmho/cm
Soluble Salt
Notes
84
7.9
2.5
1.4
1.4
0.01
0.0
2.6
2.6
.
0.56
Particle size distribution
Sample name
< 2 mm
2 - 0.5 mm
0.5 - 0.25 mm
0.25 - 0.1 mm
0.1 - 0.05 mm
0.05 - 0.02 mm
0.02 - 0.002 mm
< 0.002 mm
Fe2O3
CaCO3
Notes
84
NA, sample crushed to <2mm for analysis
12.4
6.3
15.2
7.8
13.6
28.1
16.3
0.33
.
Clay Mineralogy
Sample name
Mica
IHM
HIV - IHM
ICHL
VT
HIV
CHL
SM
CHL SM
FE - CHL
HT
QTZ
FLD
HB
CAL
Notes
84
.
.
.
.
.
.
.
.
.
.
.
20.0
5.0
.
traces of 14 A mineral, otherwise largely non-crystalline