On a steep NW sloping talus slope, about mid slope
Altitude:
1900 m
Aspect:
NW
Slope:
33 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
86° 33.7' S 147° 58' W
86° 33.7' S 147° 58' W
Latitude Longitude DD
-86.5617 -147.967
-86.5617 -147.967
Latitude longitude precision DD
0.0008 0.008
0.0008 0.008
Locality
Scott Glacier region, southern Trans-antarctic Mountains on Ackerman Ridge
Survey
US Geological Survey 1:250 000, 1968, Mount Blackburn
Climate
Soil climate zone:
Inland Mountain
Estimated mean annual temperature:
-38
°C
Frozen ground depth:
0 cm
Frozen type:
Dry frozen
Frozen comment:
Geology
Geological setting:
Steep slopes in this locality have the appearance of scree slopes but in reality may be thin till deposits in some places overlying stagnant ice; weakly expressed moraine ridges cross the slopes in places; the debris is very loose and unstable and readily slides on the underlying smooth ice surface where it is present; the absence of rock material from ridgetop exposures strongly suggests a moraine origin for these slope materials
Patterned ground:
Nil
Surface weathering or surface features:
Some weak staining on upper surfaces of boulders but most rocks are angular and unstained