Approximately 1.5km east of Wiest Bluff on an uneven ice- cored till surface; on the side of a patterned ground mound
Altitude:
2100 m
Aspect:
NE
Slope:
5 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
85° 24' S 176° 14' W
Latitude Longitude DD
-85.400 -176.233
Latitude longitude precision DD
0.008 0.008
Locality
Shackleton Glacier, Queen Maud Mountains, at the southern end of the Cumulus Hills, just north of Zaneveld Glacier junction with Shackleton Glacier
Survey
USGS 1:250 000 1968; Liv Glacier SV 1-10/5
Climate
Soil climate zone:
Inland mountain
Estimated mean annual temperature:
-40
°C
Frozen ground depth:
25 cm
Frozen type:
Stagnant glacial ice
Frozen comment:
25cm
Geology
Geological setting:
Dolerite outcrops widely in an undulating ice overridden landscape; cover deposits are patchy varying from bouldery felsenmeer regolith to intermittent till patches; surface age is variable owing to remnant snow fields which behave as local nevee glaciers possibly reworking older surface deposits; the drift mantle is young
Patterned ground:
Ice cored moraine with low (<1m) mounds, in places forming low ridges
Surface weathering or surface features:
Mainly subangular weakly and moderately stained dolerite boulders with slight surface exfoliation
Soil
Soil parent material:
Gravelly till including weathered dolerite (alongside site 77)
Ultraxerous, intermittent snow cover and adjacent snow patch but no thawing observed
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
78a
0
–
3
cm
pale brown (10YR 6/3) pebbly granular silty sand; moderately cohesive; many fine salt flecks with salt coatings on some stones; moderately developed vesicular structure; finer rock particles mainly subrounded, moderately stained and strongly altered; distinct boundary,
78b
3
–
13
cm
light yellowish brown (10YR 6/4) gravelly silty sand; weakly cohesive; many salt flecks diffused through the horizon; finer rock particles strongly altered, mainly subrounded and moderately stained; distinct boundary,
78c
13
–
25
cm
pale brown to very pale brown (10YR 6/3-7/3) gravelly sandy silt; loose; rock particles mainly subangular and weakly stained but smaller particles subrounded and strongly altered; sharp boundary, on ice