Approximately 2km WSW of Battleship Promontory; a very old dolerite surface with dolerite tors and rounded spheroidal weathering; an undulating surface with small smooth hollows; the site is on the upper side of a hollow where crumbled bedrock outcrops
Altitude:
1500 m
Aspect:
N
Slope:
4 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 54.5' S 161° 03' E
76° 54.5' S 160° 51' E
Latitude Longitude DD
-76.908 161.050
-76.908 160.850
Latitude longitude precision DD
0.004 0.008
0.004 0.008
Locality
Convoy Range, Trans-antarctic Mountains, Alatna valley
Survey
Climate
Soil climate zone:
Central mountain
Estimated mean annual temperature:
-30
°C
Frozen ground depth:
20 cm
Frozen type:
Ice-cemented
Frozen comment:
20cm
Geology
Geological setting:
Ferrar Dolerite forms extensive sills; the surface is an old over-ridden landscape with a mammillated topography;
Patterned ground:
Nil
Surface weathering or surface features:
Dolerite is strongly stained; rock surfaces are exfoliating and rounded; some salts present; fine grained dolerite is strongly pitted; weakly developed pavement
Xerous; scattered small snow patches on adjacent slopes but no indications of soil moistening
Biological activity:
Occasional yellow lichen observed
Profile Description
Horizon
Depth
Description
507a
-2
–
0
cm
surface granular pebbly gravel; rock particles subangular, strongly stained and some partly altered; some thin salt coatings,
507b
0
–
2
cm
strong brown (7.5YR 5/6) sandy granular gravel; weakly cohesive; weakly developed vesicular structure; rock particles subangular and moderately altered with some reddish internal staining; distinct boundary,
507c
2
–
7
cm
strong brown (7.5YR 5/6) granular gravel from in situ rock disaggregation; weakly cohesive; patchy salt accumulations; some ghosts; rock particles angular to subangular, moderately stained and some partly altered with reddish oxide staining; some patches of reddish sandy gravel; distinct boundary,
507d
7
–
20
cm
dark yellowish brown (10YR 3/4) pebbly granular gravel; in situ bedrock fragmentation; rock particles angular and moderately stained; sharp boundary overlying ice-cemented ground,
507e
10
–
15
cm
yellowish red to reddish brown (5YR 4/6 - 4/4) sandy granular gravel; reddish irregular patches form between disaggregating bedrock; rock particles subangular to angular, moderately altered with abundant red iron oxide intergranular pseudomorphs