Ross Sea Region Soil Sites
879000
879
7-Dec-1999
IBC
Near Lake Hoare, Taylor Valley, McMurdo Dry Valley region, Transantarctic Mountains
Long Term Ecological Research (nematode experimental area) site investigation of soil properties; this site |
(LTER 8) was chosen for repeat sampling every 3-4 days to see if there were measurable changes in soil |
moisture with time |
Lake Bonney Quadrangle, Antarctic 1:50,000 Topographic Series, USGS 1975
CS Pro & Lscp
Yes
162.8750
-77.6350
77deg 38.10'S
-162deg -52.50'E
cf. Notes for DESCR below
5
NNE
100
cf. Notes for GEOLAND below
1
11.6
5
7.5
15
0.8
23
-1.4
Xerous to subxerous; surface dry no adjacent snow patches
-20
Coastal mountain
Sandy to silty gravel with the coarse fraction consisting of granite (60%) and gneiss (20%) and dolerite (10%) with minor sandstone (8%) volcanic (scoria 1%) and marble
Nil observed at site, nematodes present in adjacent soil; some green algae beneath marble clasts in the general area
Moderately developed 20m irregular net with 20cm deep troughs, 50cm wide
SURFACE WEATHERING or |
SURFACE FEATURES |
Very weak surface staining on some clasts with no pitting, exfoliation or polish; weak ventifaction on some clasts and moderate rounding; calcium |
carbonate coatings on undersides of many clasts |
Site probably disturbed by foot traffic activity during biological research activities near the site
879a 2-0cm
101
cobbly sandy gravel (<2mm 35% >2mm 65%)
102
loose
103
rock particles unweathered with larger particles subrounded
104
abundant calcium carbonate coatings beneath surface clasts
105
indistinct boundary,
879b 0-2cm
201
light olive grey to pale olive (5Y 6/2 - 6/3) gravelly sand (<2mm 62% >2mm 38%)
202
loose to weakly cohesive with well developed vesicular structure
203
rock particles unweathered with larger rock particles subangular and smaller particles subrounded
204
many carbonate coatings
205
diffuse boundary,
879c 2-15cm
301
light olive grey (5Y 6/2) cobbly gravelly silty sand (<2mm% 62% <2mm% 38%)
302
weakly cohesive with well developed vesicular structure
303
rock particles unweathered and subangular to subrounded
304
carbonate coatings around many clasts
305
sharp boundary,
879d 15-25cm
401
light olive grey to olive grey (5Y 6/2 - 5/2) gravelly sand (2mm% 80% >2mm 20%)
402
moderately cohesive and moist
403
unweathered with rock particles subangular to subrounded
404
many carbonate coatings
405
distinct boundary,
879e 25-30cm
501
light olive grey to olive grey (5Y 6/2 - 5/2) gravelly silty sand
502
firmly cohesive and frosted
503
rock particles unweathered and subangular to subrounded
504
many carbonate coatings
505
sharp boundary,
879f 30-38cm
601
light olive grey to olive grey (5Y 6/2 - 5/2) gravelly sandy silt
602
very hard
603
ice-cemented
604
rock particles unweathered and subangular to subrounded
No
Hard ice-cemented
30
1
(30cm)
Geoland
The deposit is unweathered Ross I till, possibly derived from the Canada Glacier but almost certainly with an up-valley influence because of the presence of |
marble clasts from basement rocks; the tills may be fluvio-glacial owing to complex depositional ice-marginal processes as the sand % generally increases |
downwards while there are noticeably more coarse clasts at the surface |
Descr
About 1.4km SSE of Camp Hoare; 5m north of the LTM Decomposition plot, about 300m south of Lake Hoare among shallow ridge and gully topography on |
the lower part of the valley side; the site is to the east of a low ridge and in a 30m wide hollow on a sloping hillside; it has an uneven slightly hummocky surface; |
this is the second sampling at this site and is designated LTER 8b |
Soluble Salt |
Concentration |
87900001
879a
2-0cm
-2
0
1.97
51.00
0.12
13.80
none
87900002
879b
0-2cm
0
2
1.70
78.00
0.24
17.30
none
87900003
879c
2-15cm
2
15
1.85
80.00
0.45
9.80
none
87900004
879d
15-25cm
15
25
1.73
89.00
1.16
7.00
none
87900005
879e
25-33cm
25
33
83.00
1.75
7.40
none
87900006
879f
33-35cm
33
35
69.00
5.00
31.00
none
12-Dec-2005
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