On the lower slopes near the south of the basin like surface at Roberts Massif; the landscape unit comprises an extensive glacial retreat surface, formed following retreat of a tongue of polar ice; a strongly rolling to hilly surface with moraine loops marking retreat stages; the site is a convex upper slope on the west side of a broad moraine loop ridge
Altitude:
2050 m
Aspect:
SE
Slope:
5 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 33' S 177° 03' W
Latitude Longitude DD
-85.550 -177.050
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:
Young till overlies older till, and dolerite on the lower surfaces at Roberts Massif; north of the ice tongue at Grass Bluff, the till forms a series of retreat surfaces marked by bouldery moraine loops; the surface represents the latest stage of polar ice retreat
Patterned ground:
Nil
Surface weathering or surface features:
Surface boulders are mainly subangular with weak superficial staining; insignificant pavement development
Soil
Soil parent material:
Dolerite till with some Beacon Group sedimentary material and older till material
light yellowish brown (10YR 6/4) bouldery pebbly gravel; loose; dolerite and sandstone rock particles are mainly subangular to subrounded and unstained, but some strongly altered granite particles are present; distinct boundary,
95b
8 – 10 cm
very pale brown (10YR 7/4) sandy cobble and pebble gravel; weakly cohesive; discontinuous salt accumulations forming a weak salt horizon; rock particles mainly subangular and unstained but some subrounded, strongly stained and altered; distinct boundary,
95c
10 – 26 cm
very pale brown (10YR 7/4) sandy cobble and pebble gravel; loose; a few flecks of salt; rock particles mainly subangular and unstained but some subrounded, strongly stained and strongly altered; sharp boundary, on older till