At the northern of Marble Point region, approximately 1.9km west of Gneiss Point; on an undulating surface 150m south of a dolerite knoll; an exposure of brown 'golden shale'
Altitude:
55 m
Aspect:
Nil
Slope:
0 °
Location Data
Observer
GGC
IBC
GPS
Yes
Latitude Longitude DMS
77° 24.19' S 163° 39.59' E
77° 24' 19" S 163° 39' 58" E
Latitude Longitude DD
-77.40317 163.65983
-77.4053 163.6660
Latitude longitude precision DD
0.00008 0.00008
0.00015 0.00015
Locality
Marble Point region, western McMurdo Sound just east of the Wilson Piedmont Glacier, between Marble Point and Gneiss Point
Survey
Marble Point Quadrangle, US Geological Survey, 1975
Climate
Soil climate zone:
Coastal Antarctic
Estimated mean annual temperature:
-18
°C
Frozen ground depth:
0 cm
Frozen type:
Frozen comment:
Geology
Geological setting:
A deposit described as Golden Shale occurs over about 100ha and has scattered erratics on the surface; the deposit is not seen in situ but larger fresh fragments occur around an old explosion pit; the material has been determined to be phillipsite, thought to have originated from the deposition of volcanic ash into a saline lake, and is believed to be several million years old, possible of similar age to other phillipsite deposits recorded elsewhere in the Dry Valleys; this deposit is significant as it sets a minimum age for the uplift of Wright Valley Fiord; the material is extremely fissile, has a low density and is distinctly banded
Patterned ground:
Micro cryic features; many rock fragments lying vertically