Near a dolerite knoll, about 1km W of the Rhone Glacier and 4.5km S of Taylor Glacier; a residual well weathered dolerite surface with scattered rounded bedrock outcrops separated by small flattish surfaces in between
Altitude:
1550 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 41.5' S 162° 1.9' E
77° 42.5' S 162° 10' E
Latitude Longitude DD
-77.692 162.0320
-77.708 162.17
Latitude longitude precision DD
0.004 0.0008
0.004 0.08
Locality
Taylor Dry Valley, McMurdo Dry Valley region, Rhone Glacier
Survey
USGS 1:50,000 Antarctic Topo. Ser. Lake Bonney Quadrangle
Climate
Soil climate zone:
Inland Mountain
Estimated mean annual temperature:
-27
°C
Frozen ground depth:
25 > cm
Frozen type:
Dry frozen
Frozen comment:
>25cm
Geology
Geological setting:
Higher altitude surfaces west of the Rhone Glacier are very old and show strong weathering; bedrock ventiforms are present with exfoliation and wind removal of up to 1m of bedrock; erratics are absent indicating there has been no ice cover for a long time; there are local occurrences of Beacon Sandstone
Patterned ground:
Nil
Surface weathering or surface features:
Surface dolerite boulders are probably bedrock and are well rounded; fine textured dolerite is distinctly pitted; coarse dolerite shows, surface exfoliation; distinct surface staining
Soil
Soil parent material:
Weathering dolerite bedrock with airborne inclusion of siliceous material from Beacon Sandstone
Dry soil but some snow patches nearby; soil is probably moistened occasionally
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
323a
-1
–
0
cm
surface granular sand between rounded bedrock clasts; subangular strongly stained and moderately altered,
323b
0
–
3
cm
brown to dark brown (10YR 4/3) granular gravel; loose to weakly cohesive; rock particles angular, strongly stained and moderately altered; some quartz grains rounded; distinct boundary,
323c
4
–
10
cm
dark yellowish brown (10YR 4/4) sandy granular and pebble gravel; moderately cohesive; abundant diffuse salts; rock particles angular, moderately to strongly stained and weakly to moderately altered; distinct boundary,
323d
10
–
15
cm
brown to dark brown (7.5YR 4/4) granular gravel; loose; rock particles angular, moderately stained and moderately altered; some quartz grains rounded; bedrock clasts angular and firm; distinct boundary,
323e
17
–
25
cm
brown to dark brown (7.5YR 4/4) granular gravel and fractured bedrock; moderately to firmly cohesive; frosted; rock particles subangular subrounded and moderately stained; many subrounded quartz grains; sharp boundary, on fractured angular dolerite bedrock