On the south side of Taylor Valley, approximately 4km SE of the Commonwealth Glacier at the eastern end of the Kukri Hills; on a lower steep slope about 100m above the valley floor
Altitude:
350 m
Aspect:
NW
Slope:
30 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 37' S 163° 26' E
77° 37' S 163° 26' E
Latitude Longitude DD
-77.617 163.433
-77.617 163.433
Latitude longitude precision DD
0.008 0.008
0.008 0.008
Locality
East end of Taylor Valley, McMurdo Dry Valley region
Survey
USGS 1:50,000 Antarctic Topo. Ser. Lake Fryxell Quadrangle
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-20
°C
Frozen ground depth:
65 cm
Frozen type:
Hard ice-cemented
Frozen comment:
65cm
Geology
Geological setting:
Basement complex schistose and granite rocks outcrop on valley side thin drift from Late Pleistocene Ross Glaciation ice advances into the valley partly covers the slopes;
Patterned ground:
Minor solifluction terracetts
Surface weathering or surface features:
A few fine surface salt encrustations and carbonate coatings
Soil
Soil parent material:
Granitic gravel over older schistose gravel till, possibly as slope drift or solifluct
Soil dry but evidence of wetness; adjacent snow pockets and periodic summer snowfall
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
301a
0
–
7
cm
pale olive (5Y 6/3) sandy gravel; moderately cohesive and frozen moderately developed vesicular structure; some thick carbonate coatings and some silt coatings; rock particles angular and dominantly unstained; distinct boundary,
301b
30
–
38
cm
pale brown (10YR 6/3) sandy gravel; moderately cohesive to firm and frosted; moderately developed vesicular structure; some thick carbonate coatings and some silt coatings; rock particles subangular and some weakly stained; indistinct boundary,
301c
60
–
65
cm
pale brown (10YR 6/3) sandy gravel; moderately cohesive to firm and frosted; moderately developed vesicular structure; a few thick carbonate coatings and some silt coatings; rock particles subangular and some weakly to moderately stained; sharp boundary, on hard frozen ground