Bromley, Gordon RM; Hall, Brenda L; Stone, John O; Conway, Howard; Todd, Claire E (2010): (Table 3) Sedimentology and weathering characteristics of drift units at Reedy Glacier [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.808061, In supplement to: Bromley, GRM et al. (2010): Late Cenozoic deposits at Reedy Glacier, Transantarctic Mountains: implications for former thickness of the West Antarctic Ice Sheet. Quaternary Science Reviews, 29(3-4), 384-398, https://doi.org/10.1016/j.quascirev.2009.07.001
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Median Latitude: -85.992233 * Median Longitude: -129.850000 * South-bound Latitude: -86.066700 * West-bound Longitude: -132.500000 * North-bound Latitude: -85.920000 * East-bound Longitude: -126.050000
Minimum Elevation: 800.0 m * Maximum Elevation: 2160.0 m
Event(s):
Caloplaca_Hills * Latitude: -86.066700 * Longitude: -131.000000 * Elevation: 800.0 m * Location: Transantarctic Mountains * Method/Device: Multiple investigations (MULT)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Lithologic unit/sequence | Unit | Bromley, Gordon RM | drift unit | ||
6 | Lithology/composition/facies | Lithology | Bromley, Gordon RM | CsD: clast-supported diamicton; MsD: matrix-supported diamicton; (ms): moderately sorted; (us): unsorted; (sr): silt-rich; (sd): sand-rich; (cr): clay-rich; (sr/sd): (silty-sandy); (gr): gravel rich | ||
7 | Depth, relative | Depth rel | m | Bromley, Gordon RM | weathering depth | |
8 | Layer thickness | Thickness | m | Bromley, Gordon RM | deflation pavement | |
9 | Comment | Comment | Bromley, Gordon RM | |||
10 | Observation | Obs | Bromley, Gordon RM | cavernous weathering of surface boulders | ||
11 | Observation | Obs | Bromley, Gordon RM | planed boulders | ||
12 | Observation | Obs | Bromley, Gordon RM | patterned ground | ||
13 | Observation | Obs | Bromley, Gordon RM | ghosts (highly rotten clasts lacking structural integrity) | ||
14 | Description | Description | Bromley, Gordon RM |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
154 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Unit (drift unit) | 6 Lithology (CsD: clast-supported diamicto...) | 7 Depth rel [m] (weathering depth) | 8 Thickness [m] (deflation pavement) | 9 Comment | 10 Obs (cavernous weathering of surfa...) | 11 Obs (planed boulders) | 12 Obs (patterned ground) | 13 Obs (ghosts (highly rotten clasts ...) | 14 Description |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy III | (us) CsD | 0.0 | 0.00 | No | No | Frost cracks | No | Boulders largely confined to surface. Sand fines with depth. | |
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy A | Boulder | 0.0 | 0.00 | No | No | No | No | No fine sediments. Boulders angular and lightly stained. | |
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy B | CsD | 0.6 | 0.20 | Minor | No | No | No | Unit thickness ranges from one clast to 1 m, includes pockets of sorted sand. | |
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy C | (us) CSD | weathering depth and deflation pavem. thickness unknown | Moderate | No | No | No | Drift dominated by boulders. | ||
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy D | (ms) CsD | 0.8 | 0.10 | Extreme | Yes | No | Yes | Deeply stained sand fines with depth. 4 cm salt lens at 10 cm depth, salt flecks common to 15 cm depth. | |
Quartz_Hills | -85.9200 | -132.5000 | 1400 | Reedy E | (sr) MsD | >0.5 | 0.20 | Extreme | Yes | No | Yes | Sand & gravel confined to upper 5 cm and probably products of weathering of surface boulders. | |
Caloplaca_Hills | -86.0667 | -131.0000 | 800 | Reedy III | 0.0 | no deflation pavement thickness | No | No | No | Unit consists of occasional fresh boulders and cobbles. | |||
Caloplaca_Hills | -86.0667 | -131.0000 | 800 | Reedy B | no deflation pavement thickness | Minor | No | No | Surface of frost-shattered boulders, sand and weathering detritus. | ||||
Caloplaca_Hills | -86.0667 | -131.0000 | 800 | Reedy D | Extensive | No | Yes | Surface formed of deeply stained, angular boulders, weathering detritus and coarse gravel. Boulders exfoliating. | |||||
Caloplaca_Hills | -86.0667 | -131.0000 | 800 | Reedy E | Extreme | Yes | No | Deflated surface dominated by coarse weathering detritus. Silty sand below surface. | |||||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Reedy III | No | No | No | No | Unit consists of occasional fresh boulders and cobbles. | ||||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Reedy B | CsD | No | No | No | No | Clast types exotic to lower Polygon Spur. Unit very loose. Salt flecks common to 60 cm. | |||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Reedy C | (us) MsD | 0.3 | 0.20 | Moderate | No | No | No | Highly compacted silty-sand matrix to 70 cm. Salt throughout. | |
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Reedy D | (gr) CsD | >1.0 | Moderate- Extensive | No | No | No | Matrix tightly packed. Fractured clasts throughout unit. Salt beneath surface boulders. | ||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Reedy E | (sr) MsD | >1.0 | Extreme | No | No | Many granite boulders rest on pedestals of underlying sedimentary bedrock protected from wind erosion. | |||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Red | (sr/sd) MsD | >1.0 | 0.05 | No | No | Relict frost cracks | No | Matrix varies from silt to silt-rich gravel. Exotic clasts on surface and throughout depth. | |
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Horlick Unit 5 | (cr) MsD | no deflation pavement thickness | No | No | No | Surface dominated by weathered clay and exotic clasts. Clay highly compacted. Granite and large boulders absent. | |||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Cirque I | CsD | No | No | Frost cracks | No | Unit overlies buried glacier ice. | |||
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Cirque II | (sd) MsD | >0.5 | 0.10 | No | No | Polygons (>2 m) | No | Unit overlies buried glacier ice. Surface of small, moderately stained and exfoliating boulders. | |
Polygon_Spur | -85.9900 | -126.0500 | 2160 | Cirque III | (sd) MsD | >0.5 | 0.10 | No | No | Polygons (>2 m) | No | Unit overlies buried glacier ice. Greater abundance of surface boulders. Fresher clasts in frost cracks. |