Eastern end of the Brown Hills, about 2km NE of the top of Diamond Hill, on an uneven, sloping, broad bouldery ridge surface near a dark coloured granodiorite outcrop
Altitude:
1000 m
Aspect:
NE
Slope:
8 °
Location Data
Observer
IBC
GPS
No
Latitude Longitude DMS
79° 51' S 159° 15' E
Latitude Longitude DD
-79.850 159.25
Latitude longitude precision DD
0.008 0.04
Locality
Victoria Land, Trans-antarctic Mountains; at the southern end of the Cook Mountains in the Brown Hills region of the Darwin Glacier
Survey
USGS 1:250,000 1963; Carlyon Glacier ST 57-60/13*
Climate
Soil climate zone:
Coastal mountain
Site temperature profile
Depth (cm)
Soil temp (°C)
Notes
0
-7
air overcast
0
1
surface
3
0
10
0
20
-1
30
-3
Estimated mean annual temperature:
-25
°C
Frozen ground depth:
30 cm
Frozen type:
Hard ice-cemented
Frozen comment:
30cm
Geology
Geological setting:
Granodiorite of the Granite Harbour Intrusives outcrops more extensively on the upper slopes of Diamond Hill with till being more abundant on the lower slopes; there is no obvious till mantle but some dolerite fragments in the soil are indicative of the presence of residual till
Patterned ground:
Active patterned ground movement with coarser textured more oxidised material in the cracks and finer less stained material near the centres
Surface weathering or surface features:
Surface boulders are disaggregating by exfoliation; also some cavernous weathering is present; accumulations of salts occur beneath some surface stones; surface rocks are subrounded and moderately stained
Soil
Soil parent material:
Largely locally derived disaggregated granodioritic bedrock with minor till drift
Oceanic subxerous; some snow patches on ridges and light a light recent snowfall which quickly ablated; the surface 1cm of the soil was slightly moist
Biological activity:
Patches of black and greenish lichen
Profile Description
Horizon
Depth
Description
118a
0 – 3 cm
yellowish brown (10YR 4/4) granular sand; loose; rock particles subangular to subrounded and moderately stained, some particles with red staining throughout; sharp boundary,
118b
3 – 8 cm
yellowish brown to light yellowish brown (10YR 5/4-6/4) sandy pebbly gravel; weakly cohesive; many particles coated with fines forming a weakly developed siltball structure; salts diffused throughout and concentrated beneath some stones; rock particles subangular and moderately stained with some partly altered; indistinct boundary,
118c
12 – 18 cm
light yellowish brown (10YR 6/4) pebbly gravelly sand; moderately to firmly cohesive (ice cementing); rock particles mainly subangular and weakly to moderately stained; sharp boundary, on frozen ground