Approximately 5km NNE of Mt Brooke, on a broad undulating ridge surface with outcrops of dolerite and Beacon Group sediments; the surface is elevated and is dominated by bedrock exposures; the site is a small flattish bench, or old felsenmeer surface, formed by a dolerite sill
Altitude:
2100 m
Aspect:
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 46.9' S 159° 57' E
76° 48' S 159° 54' E
Latitude Longitude DD
-76.7817 159.950
-76.800 159.900
Latitude longitude precision DD
0.0008 0.008
0.008 0.008
Locality
Coombs Hills in the Convoy Range, Trans-antarctic Mountains, between the Odell and Cambridge Glaciers
Survey
Climate
Soil climate zone:
Central mountain
Estimated mean annual temperature:
-31
°C
Frozen ground depth:
0 cm
Frozen type:
Dry frozen
Frozen comment:
Geology
Geological setting:
Dolerite sills and dykes intrude through Beacon Group sediments; the surface is apparently devoid of till deposits although scattered erratics of hard pitted dolerite overly sandstone in places; on this old surface, there is a patchy regolith largely comprising shallow deposits of fragmental bedrock;
Patterned ground:
Nil
Surface weathering or surface features:
Surface boulders show some rounding and wind abrasion; surface exfoliation is strongly developed on coarser grained dolerite clasts; fine grained dolerite clasts are polished, strongly stained and well pitted; where bedrock is at the surface, dolerite shows strong spheroidal weathering with as much as 30cm removed by erosion; where fragmental material has accumulated in hollows, a stone pavement is strongly developed
Xerous, a patchy cover of snow from a recent fall but little thawing
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
492a
0
–
2
cm
brown (7.5YR 5/4) granular pebbly gravel; loose; salt accumulations around some rock particles; rock particles angular, moderately to strongly stained and strongly altered; distinct boundary,
492b
2
–
6
cm
strong brown (7.5YR 5/6) granular pebbly gravel forming a wedge like deposit in a bedrock cleft; moderately cohesive; rock particles mainly angular, weakly stained and moderately altered; sharp boundary, on dolerite bedrock