On the lower slopes near the south of the basin like surface at Roberts Massif; glacial surfaces formed following retreat of a tongue of polar ice; a strongly rolling to hilly surface with moraine loops marking retreat stages; site is 4m N of a bouldery moraine loop on a smooth gentle slope
Altitude:
2200 m
Aspect:
NE
Slope:
4 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 33' S 176° 56' W
Latitude Longitude DD
-85.550 -176.933
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:
Younger 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, about 2m high
Patterned ground:
Nil
Surface weathering or surface features:
Dolerite boulders in moraine loop are mainly subangular and moderately stained; pebbles forming a surface pavement are moderately stained, subangular to sub rounded with polish on some clasts; salts beneath some surface stones
Soil
Soil parent material:
Dolerite till with some Beacon Group sedimentary material
light brown (7.5YR 6/4) pebbly sandy gravel; loose; rock particles predominantly subangular, moderately stained and partly altered; distinct boundary,
93b
7
–
15
cm
light brown (7.5YR 6/4) pebbly sandy gravel; moderately to firmly cohesive; abundant salt accumulations forming a discontinuous horizon; rock particles subangular and moderately stained with surface alteration forming a distinct rind; indistinct boundary,
93c
15
–
23
cm
pale brown (10YR 6/3) sandy pebble and cobble gravel; loose; few fine salt flecks; rock particles subangular and weakly stained; sharp boundary, on pale grey till