On a broad undulating slightly concave surface on the north slopes of Roberts Massif, about 2km south of a small ice tongue, just south of Everett Nunatak,
Altitude:
2100 m
Aspect:
W
Slope:
3 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 31' S 177° 04' W
Latitude Longitude DD
-85.517 -177.067
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:
Till occurs extensively on the lower slopes of Roberts Massif forming mainly shallow deposits over dolerite, Beacon Group sediments and tillite which outcrop in places; the younger unconsolidated tills increase in age away from the ice front and in places form distinctive ridges or loops 1-2m high that mark pauses in ice recession
Patterned ground:
Nil
Surface weathering or surface features:
Surface boulders are rounded on edges; moderately stained and show only slight exfoliation; between boulders, a pebble pavement is moderately developed; salts are extensive beneath surface stones
pale brown (10YR 6/3) sandy pebble gravel; loose; rock particles mainly subrounded, moderately stained, and moderately to strongly altered; abrupt boundary,
86b
3
–
7
cm
light brown (7.5YR 6/4) sandy pebble and cobble gravel; loose; rock particles mainly subrounded, moderately stained and moderately to strongly altered; sharp boundary,
86c
7
–
13
cm
pink (7.5YR 7/4) gravelly sand; moderately cohesive; profuse salts forming a continuous salt horizon; rock particles subrounded, moderately to strongly stained and moderately altered; abrupt boundary,
86d
13
–
25
cm
light yellowish brown (10YR 6/4) sandy pebbly gravel; loose; rock particles mainly subangular and unstained to weakly stained; abrupt boundary, on consolidated old tillite.