8.5km SW of the western end of the Northwind Glacier on an extensive bench-like or terrace surface; the surface is extremely variable with patches of dolerite felsenmeer, strongly oxidised and less oxidised areas, patterned and non-patterned ground etc.; the site is 2m away from site 499
Altitude:
140 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 45.1' S 160° 45' E
76° 43' S 160° 56' E
Latitude Longitude DD
-76.7517 160.75
-76.717 160.933
Latitude longitude precision DD
0.0008 0.04
0.008 0.008
Locality
Convoy Range, Trans-antarctic Mountains, in the valley of the Northwind Glacier
Survey
Climate
Soil climate zone:
Central mountain
Estimated mean annual temperature:
-28
°C
Frozen ground depth:
30 cm
Frozen type:
Hard ice-cemented
Frozen comment:
30
Geology
Geological setting:
Dolerite and Beacon Group sediments occur locally and the regolith mantle appears to be from local materials; this profile is browner that soil 499 and possibly has less sandstone/more dolerite in the parent material
Patterned ground:
Poorly defined old nets, currently probably inactive
Surface weathering or surface features:
A well developed pavement with rounded surface dolerite cobbles and pebbles; some weak to moderately ventiform clasts, unstained on up-wind sides and well stained on down-wind sides; staining ranges from strong to weak depending on the degree of abrasion; some pitted rocks are present; exfoliation skins on surface clasts are well developed; a well developed oxidation rind is present beneath some surface clasts
Xerous; no local snow patches but the soil is moist below 7cm
Biological activity:
Occasional patches of yellow lichen in exfoliation cracks
Profile Description
Horizon
Depth
Description
500a
0
–
7
cm
yellowish brown (10YR 5/4) pebbly granular sand; loose; salt accumulations around some rock particles; rock particles subangular, weakly to moderately stained and moderately altered; sharp boundary,
500b
7
–
15
cm
strong brown (7.5YR 5/6) sandy cobbly to granular gravel; moderately cohesive; abundant salts in patches across the horizon; rock particles rounded to subrounded, moderately stained and moderately to weakly altered; distinct boundary,
500c
15
–
22
cm
yellowish brown (10YR 5/4) sandy cobbly to granular gravel; weakly cohesive; salt accumulations between disaggregating rock particles; rock particles subangular, moderately to strongly stained and strongly altered; distinct boundary,
500d
22
–
25
cm
olive (5Y 4/3) granular sand; weakly cohesive; rock particles mainly rounded quartz grains with some subangular weakly stained dolerite; sharp boundary, on frozen ground