The w end of Dais, about 750m E of a small hill; a broad gently undulating till covered surface on an even smooth surface and on the S side of the Dais
Altitude:
825 m
Aspect:
S
Slope:
3 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 33' S 161° 9.5' E
77° 33' S 161° 12' E
Latitude Longitude DD
-77.550 161.158
-77.550 161.200
Latitude longitude precision DD
0.008 0.004
0.008 0.008
Locality
Wright Valley, McMurdo Dry Valley region, The Dais
Survey
USGS 1:50,000 Antarctic Topo. Ser. Lake Vanda Quadrangle
Climate
Soil climate zone:
Central Mountain
Estimated mean annual temperature:
-23
°C
Frozen ground depth:
70 > cm
Frozen type:
Dry frozen
Frozen comment:
>70cm
Geology
Geological setting:
Dais is a prominent geomorphic feature formed partly from the dolerite sill influence and also from prolonged erosion; because of the island like geomorphology, the till is not subject to local alpine influences but should represent major glacial activity in Wright Valley; further north some large marble clasts were observed suggesting the possibility of up-valley ice influence
Patterned ground:
Nil
Surface weathering or surface features:
A well developed pebble pavement with occasional small boulders; moderately developed ventiforms and boulder faceting; granites with some cavernous weathering; dolerite with some staining and showing some exfoliation; salts beneath some surface stones
Soil
Soil parent material:
sandy gravel till from predominantly granite with some dolerite
surface pebbles and granular sand; granites weakly stained, dolerite weak to moderately stained, subrounded,
353b
0 – 5 cm
olive yellow (2.5Y 6/6) sandy gravel; moderately cohesive; moderately developed vesicular structure; rock particles subangular and weakly stained but some crumbly; distinct boundary,
353c
5 – 10 cm
light olive brown (2.5Y 5/6) very sandy gravel; moderately cohesive; many small diffuse salt flecks mostly concentrated around stones; rock particles subangular and unstained; indistinct boundary,
353d
30 – 40 cm
light olive brown (2.5Y 5/6) sandy gravel; moderately to firmly cohesive; few scattered salt flecks; rock particles subangular and unstained; indistinct boundary,
353e
60 – 65 cm
olive yellow (2.5Y 6/6) sandy gravel; moderately cohesive; rock particles angular and unstained; indistinct boundary, on sandy gravel