Approximately 1km NE of Mt Brooke, on the lower slopes of a tongue of moraine formed by retreat of an alpine glacier on the north slopes of Mt Brooke
Altitude:
2400 m
Aspect:
NW
Slope:
15 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
76° 48.6' S 159° 53.8' E
76° 48' S 159° 52' E
Latitude Longitude DD
-76.8100 159.8970
-76.800 159.867
Latitude longitude precision DD
0.0008 0.0008
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:
-33
°C
Frozen ground depth:
10 cm
Frozen type:
Hard ice-cemented
Frozen comment:
10cm
Geology
Geological setting:
Outcropping rocks on Mt Brooke include Jurassic tuffs and lavas and Ferrar Dolerite, the drift mantle is intermittent and thin or absent in places; till ranges in age from young to very old; young till on lower slopes of Mt Brooke comprises previously weathered rock materials
Patterned ground:
Surface weathering or surface features:
The surface is bouldery; rocks are unstained and mainly angular but some softer rocks are partly rounded and abraded; many rocks are altered from pre-weathering; there are thin white salt efflorescences on the surface of and beneath some stones
Soil
Soil parent material:
Ice-rich young till from previously altered tuffs and lavas
Xerous, recent widespread snowfall with some soil moistening due to thawing
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
487a
0
–
5
cm
surface boulders, cobbles and pebbles; mainly angular and unstained but many are altered by earlier weathering,
487b
5
–
10
cm
brown (7.5YR 5/4) granular cobbly gravel; loose; thin white salt coatings on some rock surfaces; hard rock particles angular and softer particles subrounded and unstained but many are strongly altered and oxidised throughout; distinct boundary,
487c
10
–
15
cm
brown (7.5YR 5/4) granular cobbly gravel; loose to moderately cohesive and frosted; thin salt coatings on some rock surfaces; hard rock particles angular and softer particles subrounded with many strongly oxidised and altered throughout; sharp boundary,
487d
10
–
25
cm
brown (7.5YR 5/4) granular cobbley gravel; extremely hard; ice cemented.