On the floor of McKelvey Valley, a little to the southwest of a low pass in the Insel Range; approximately 5.5km SSE from Lake Vashka; the surface is a broad till plain of very low relief with low scattered boulders and is at the western end of till mapped as Insel drift; the soil is very similar to that at site 133 but has some patches of brown soil a little below the surface, which were sampled
Altitude:
825 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
77° 25' S 161° 22' E
Latitude Longitude DD
-77.42 161.367
Latitude longitude precision DD
0.04 0.008
Locality
Victoria Land, Trans-antarctic Mountains; in Barwick 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:
-24
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Tills in this part of McKelvey Valley were mapped by Calkin (1964) as Bull and Insel Drift; the site is on Insel Drift which is considered by Calkin to have originated from eastward flowing ice
Patterned ground:
A stable surface with old subdued inactive patterned ground
Surface weathering or surface features:
Marked fragmentation, abrasion and cavernous weathering of surface boulders; sandstones are strongly stained and dolerite rocks moderately stained; the surface is soft and has a well developed pebble pavement with many well formed ventifacts
Soil
Soil parent material:
Insel Drift till, containing much sandy/silty rock flour like material; the oxidised patches are indicative of increasing soil age
Xerous to subxerous; a dry site but with occasional small snow patches
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
135a
3 – 5 cm
yellowish brown (10YR 5/6) pebbly granular sand occ. in patches often adj. or under stones in the profile, or ass. with patches of coarser textured soil material; weakly cohesive with weakly developed vesicular structure; quartz particles rounded and moderately stained, ferromagnesian rich particles, subrounded and unstained