About 7km NW of Lake Vida, near the junction of Upper Victoria Valley and Barwick Valley; on a surface mapped as Vida Drift by Calkin (1964) comprising low moraine ridges or loops with flat areas between; the site is on a flat surface
Altitude:
580 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
77° 20.7' S 161° 34.5' E
Latitude Longitude DD
-77.3450 161.575
Latitude longitude precision DD
0.0008 0.004
Locality
Victoria Land, Trans-antarctic Mountains; in Upper Victoria Valley, part of the McMurdo Sound Dry Valley system
Survey
USGS 1:250 000 1986; Ross Island and Vicinity, Antarctica
Climate
Soil climate zone:
Central mountains
Estimated mean annual temperature:
-23
°C
Frozen ground depth:
60 cm
Frozen type:
Hard ice-cemented
Frozen comment:
60cm
Geology
Geological setting:
Tills in this part of Upper Victoria Valley were mapped by Calkin (1964) as Vida Drift derived from the Upper Victoria Glacier; they are marked by the occurrence of numerous large sandstone boulders
Patterned ground:
Weakly developed large polygonal nets
Surface weathering or surface features:
Sandstone or quartzite boulders are up to 5m in diameter, are partly decomposed and have some cavernous weathering; some fragmentation of dolerite; larger clasts subangular to subrounded; moderate development of a pebble pavement
Soil
Soil parent material:
Bouldery till with common Beacon Group sandstone boulders
Xerous to subxerous; the site is dry with moisture derived only from snow fall
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
138c
-110 – 20 cm
yellowish brown (10YR 5/6) sandy pebbly cobbly gravel with some small brighter patches around some stones; weakly cohesive; salt flecks scattered through the horizon and also some larger concentrations; larger rock particles subangular and unstained with smaller particles rounded and weakly to moderately stained; distinct boundary,
138a
0 – 3 cm
light yellowish brown (10YR 6/4) pebbly granular sand; weakly cohesive forming a weakly developed surface crust; moderately developed vesicular structure; larger rock particles subangular and unstained with smaller quartz particles subrounded to rounded and weakly to moderately stained; distinct boundary,
138b
4 – 8 cm
yellowish brown (10YR 5/4) sandy pebbly gravel; loose; larger rock particles subangular and unstained with smaller quartz particles subrounded to rounded and weakly to moderately stained; indistinct boundary,
138d
30 – 40 cm
brownish yellow (10YR 6/6) sandy pebbly cobbly gravel; loose to weakly cohesive; rock particles mainly subrounded to rounded and weakly to moderately stained; indistinct boundary,
138e
50 – 55 cm
light yellowish brown (10YR 6/4) sandy gravel; loose; larger rock particles subangular and unstained with smaller particles subrounded to rounded and weakly to moderately stained; sharp boundary, on ice cemented ground