soil moisture investigation of lake edge wetting front
Description:
80 m southwest of the Vanda Station Mess building on the small island on which the two disused helo pads are located, 6.9m from the lake edge; this site is the uppermost of 4 sites across the lake edge wetting fringe
Altitude:
92 m
Aspect:
SE
Slope:
7 °
Location Data
Observer
GGC
IBC
GPS
No
Latitude Longitude DMS
77° 0.0' S 161° 40.0' E
75° 50' S 166° 45' E
Latitude Longitude DD
-77.000 161.667
-75.83 166.75
Latitude longitude precision DD
0.008 0.008
0.08 0.04
Locality
Vanda Station, Wright Valley at the eastern end of Lake Vanda
Survey
not recorded
Climate
Soil climate zone:
coastal 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:
surface clasts are mainly angular and unstained
Soil
Soil parent material:
fractured, mainly lamprophyre dyke rock forming a sandy gravel mantle