A gully, approximately 2km east from the NE end of Lake Bonney with surface salts precipitation
Altitude:
300 m
Aspect:
NW
Slope:
4 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 42' S 162° 35' E
77° 42' S 162° 25' E
Latitude Longitude DD
-77.700 162.58
-77.700 162.42
Latitude longitude precision DD
0.008 0.04
0.008 0.04
Locality
Taylor Dry Valley, McMurdo Dry Valley region near Lake Bonney
Survey
USGS 1:50,000 Antarctic Topo. Ser. Lake Bonney Quadrangle
Climate
Soil climate zone:
Central Mountain
Estimated mean annual temperature:
-23
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
Glacial deposits in the area are formed from a complex interaction of advances from the Taylor Glacier with nearby alpine glaciers; granitic rocks are common and intruded by dolerite and dyke rocks but there are also numerous small volcanic cones which post-date glacial episodes; some shallow gullies mark the sites of ephemeral past water flows from thaw waters from the Marr Glacier; occasional surface salt precipitations may be due to evaporation of excess water