The edge of the Polar Plateau at the head of La Prade Valley, 5km SE of Shenk Pk.; an undulating convex dolerite felsenmeer surface
Altitude:
2970 m
Aspect:
SE
Slope:
5 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 14' S 174° 19' W
Latitude Longitude DD
-85.233 -174.317
Latitude longitude precision DD
0.008 0.008
Locality
Shackleton Glacier, Queen Maud Mountains, on mountain slopes to the south of McGregor Glacier at the northern end of the Cumulus Hills
Survey
USGS 1:250 000 1968; Liv Glacier SV 1-10/5
Climate
Soil climate zone:
Central mountain
Estimated mean annual temperature:
-40
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Not determined
Geology
Geological setting:
Ferrar Dolerite which occurs extensively as sills forms erosion resistant caps on many hills; on low relief surfaces, bedrock has been fractured by frost action to form a rubble layer or felsenmeer
Patterned ground:
Hummocky surface with poorly defined small nets
Surface weathering or surface features:
Surface boulders very strongly stained and subrounded to rounded
Xerous; abundant snow patches but no thawing observed
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
64a
0 – 8 cm
yellowish red (5YR 5/6) boulder, cobble and granule gravel; weakly cohesive with some cementing by finer particles; abrupt boundary, on dolerite bedrock