On the upper northwest slopes above the lower lying Roberts Massif basin; a high bench formed by Beacon group sediments with a thin cover of drift material; a flat smooth surface
Altitude:
2400 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 32' S 177° 11' W
Latitude Longitude DD
-85.533 -177.183
Latitude longitude precision DD
0.008 0.008
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 cm
Frozen type:
Dry frozen
Frozen comment:
Geology
Geological setting:
Beacon group sediments outcrop in a few places but dolerite is the predominant rock type in the area; in places, the sediments are argillised and altered by dolerite intrusion; where dolerite drift material is present, a soil cover has formed; where no dolerite drift is present, sandstone rock outcrops
Patterned ground:
Weakly developed polygons on flattish sites
Surface weathering or surface features:
Dolerite surface pebbles and boulders are strongly stained, well rounded and distinctly ventiform; some cavernous weathering (pitting) is present on upper surfaces of clasts
yellowish brown (10YR 5/4) granular sand; loose to weakly cohesive; salt flecks diffused throughout; some dolerite rock particles strongly altered with distinct weathering rinds; sharp boundary,
92b
5
–
13
cm
white (5Y 8/2) crystalline salt horizon; cohesive; sharp boundary,
92c
13
–
23
cm
pale yellow (2.5Y 7/4) silty sand; cohesive; abundant salt flecks in patches; soil colour is light yellowish brown (2.5Y 6/4) where salt is absent, on sandstone rock