Art Beacon Heights, between east Beacon and West Beacon, a small alpine cirque valley; the site is located at the valley mouth on a ridge of granitic moraine, near the centre of the valley and on the crest of the ridge
Altitude:
1700 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
IBC
GGC
GPS
No
Latitude Longitude DMS
77° 49.1' S 161° 51.6' E
77° 49' S 160° 53' E
Latitude Longitude DD
-77.8183 161.8600
-77.817 160.883
Latitude longitude precision DD
0.0008 0.0008
0.008 0.008
Locality
Upper Taylor Valley
Survey
USGS, 1:250,000 Ross Island and Vicinity Antarctica 1986
Climate
Soil climate zone:
Inland Mountain
Estimated mean annual temperature:
-30
°C
Frozen ground depth:
15 > cm
Frozen type:
Frozen comment:
>15cm
Geology
Geological setting:
Valley mouth moraines in the Asgard Range of Wright Valley have originated from ice entering the valleys, similar to the more recent invasions of Ross tills into the Lower Taylor and Lower Wright Valleys; at Beacon Heights, the valley mouth moraine has a distinct granite erratic component, similar to that at New Mountain indicating a distant source from a large ice invasion; the local rocks are Ferrar Dolerite and Beacon Sandstone
Patterned ground:
Nil
Surface weathering or surface features:
A moderately developed cobble pavement; dolerite and sandstone clasts are subrounded, moderately ventiformed and strongly stained; some salts beneath surface stones
Soil
Soil parent material:
Predominantly sandstone and dolerite stony till with some granite
surface cobbles, pebbles and granular sand; particles mainly subrounded and strongly stained with some strongly altered,
416b
0 – 5 cm
yellowish brown (10YR 5/8) bouldery sandy gravel; weakly cohesive; some diffuse salt flecks; some sandstone clasts disaggregated; rock particles mainly subangular and weakly stained; indistinct boundary,