Meyer Hills in the southeast of the Heritage Range, Beaudoin Peak, about 5m below the top on a steep slope
Altitude:
975 m
Aspect:
E
Slope:
30 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
79° 48' S 81° 00' W
79° 48' S 81° 00' W
Latitude Longitude DD
-79.800 -81.00
-79.800 -81.00
Latitude longitude precision DD
0.008 0.08
0.008 0.08
Locality
West Antarctica in Ellsworth Land at the southern end of the Ellsworth Mountains
Survey
US Geological Survey, 1:250 000, 1967, Union Glacier
Climate
Soil climate zone:
Inland/Coastal Mountain
Estimated mean annual temperature:
-25
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
The Ellsworth Mountains comprise a thick sequence of folded metasedimentary rocks comprising limestones, conglomerates and quartzites dating to Precambrian; the West Antarctic Ice Sheet is believed to have fluctuated greatly in response to global sea level changes and evidence of these fluctuations should be present in the tills and soil weathering record; the Meyer Hills are predominantly quartzitic sandstones
Patterned ground:
Nil
Surface weathering or surface features:
Bedrock exposures are strongly fractured and surface fragmental detritus is angular but strongly oxidised
Soil
Soil parent material:
Fragmented quartzitic bedrock
Previous disturbance:
Nil
Soil weathering stage:
6
Soil moisture status:
No adjacent snow patches, site is dry with little sign of soil moistening
Biological activity:
Nil observed
Profile Description
Horizon
Depth
Description
462a
0
–
5
cm
brown (10YR 5/3) granular gravel; moderately cohesive; salt precipitations on rock fragments; rock particles subangular and many distinctly stained with some partly altered; indistinct boundary,
462b
5
–
10
cm
brown (7.5YR 5/4) granular gravel; loose; rock particles angular and moderately stained