assessment of environmental impacts from past human activities at Vanda Station; this site was sampled from a relatively undisturbed area upwind from Vanda Station to allow comparisons to be made with disturbed sites
Description:
approximately 340m southwest of Vanda Station and about 20m to the west of site 703 but on a ridge surface formed from lamprophyre dyke rock
Altitude:
98 m
Aspect:
Slope:
0 °
Location Data
Observer
GGC
IBC
GPS
No
Latitude Longitude DMS
77° 0.0' S 161° 40.0' E
77° 31.76' S 161° 39.60' E
Latitude Longitude DD
-77.000 161.667
-77.52930 161.6600
Latitude longitude precision DD
0.008 0.008
0.00008 0.0008
Locality
Vanda Station, Wright Valley at the eastern end of Lake Vanda
Survey
not recorded
Climate
Soil climate zone:
central mountain
Estimated mean annual temperature:
-20
°C
Frozen ground depth:
35 ~
Frozen type:
dry frozen
Frozen comment:
~35
Geology
Geological setting:
the rocks of the area are granodiorites that have been cut with lamprophyre dykes and form a strongly undulating ridge and gully topography as a result of ice over riding from down-valley and up-valley glaciations and to a lesser extent, subaerial weathering; subsequent to glaciation, the terrain has been subjected to drowning and emergence from fluctuating lake levels from Lake Vanda with some sorting or resorting of surficial materials
Patterned ground:
Surface weathering or surface features:
the surface boulders are predominantly angular and unstained and show only minor abrasion around some edges
Soil
Soil parent material:
fragmented bouldery lamprophyre dyke rock with sand infilling fracture fissures; some algal accumulation near the surface