Höfle, Hans-Christian; Buggisch, Werner (2011): Tab. 7: Results of an inventory of erratics in the Mount Provender area and at Lake Lundström on Mount Gass [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.767442, In supplement to: Höfle, H-C; Buggisch, W (1995): Glacial geology and petrography of erratics in the Shackleton Range, Antarctica. Polarforschung, 63(2/3), 183-201, hdl:10013/epic.29721.d001
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Coverage:
Latitude: -80.500000 * Longitude: -22.000000
Minimum Elevation: 0.0 m * Maximum Elevation: 0.0 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Site | Site | Höfle, Hans-Christian | |||
2 | Sample code/label | Sample label | Höfle, Hans-Christian | |||
3 | Erratics | Erratics | # | Höfle, Hans-Christian | Counting >2000 µm fraction | |
4 | Quartzite | Qzite | % | Höfle, Hans-Christian | ||
5 | Conglomerate | Congl | % | Höfle, Hans-Christian | Limestone conglomerate and breccia | |
6 | Limestone | Lmst | % | Höfle, Hans-Christian | reddish-brown | |
7 | Marble | Mar | % | Höfle, Hans-Christian | ||
8 | Sandstone | Sdst | % | Höfle, Hans-Christian | ||
9 | Conglomerate | Congl | % | Höfle, Hans-Christian | and breccia | |
10 | Schist | Schist | % | Höfle, Hans-Christian | dark grey | |
11 | Schist | Schist | % | Höfle, Hans-Christian | reddish-brown | |
12 | Sedimentary rock | Sedim rock | % | Höfle, Hans-Christian | total | |
13 | Granite | Gran | % | Höfle, Hans-Christian | ||
14 | Garnet gneiss | Grt geneis | % | Höfle, Hans-Christian | ||
15 | Garnet-mica schist | Grt-mica sch | % | Höfle, Hans-Christian | ||
16 | Mica schist | Mica schist | % | Höfle, Hans-Christian | ||
17 | Gneiss | Gnei | % | Höfle, Hans-Christian | ||
18 | Amphibolite schist | Amph schist | % | Höfle, Hans-Christian | ||
19 | Dolerite | Dolerite | % | Höfle, Hans-Christian | ||
20 | Rock fragments | Rock fragm | % | Höfle, Hans-Christian | total non-sedimentary rocks |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
300 data points
Data
1 Site | 2 Sample label | 3 Erratics [#] | 4 Qzite [%] | 5 Congl [%] (Limestone conglomerate and br...) | 6 Lmst [%] (reddish-brown) | 7 Mar [%] | 8 Sdst [%] | 9 Congl [%] (and breccia) | 10 Schist [%] (dark grey) | 11 Schist [%] (reddish-brown) | 12 Sedim rock [%] (total) | 13 Gran [%] | 14 Grt geneis [%] | 15 Grt-mica sch [%] | 16 Mica schist [%] | 17 Gnei [%] | 18 Amph schist [%] | 19 Dolerite [%] | 20 Rock fragm [%] (total non-sedimentary rocks) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Mount Provender | P1 | 137 | 12 | 7 | 3 | 6 | 23 | 1 | 4 | 0 | 56 | 6 | 14 | 4 | 8 | 11 | 9 | 1 | 44 |
Mount Provender | P3 | 126 | 10 | 7 | 12 | 8 | 25 | 0 | 11 | 6 | 79 | 1 | 7 | 0 | 2 | 12 | 0 | 0 | 21 |
Mount Provender | P5 | 74 | 8 | 1 | 0 | 0 | 35 | 0 | 4 | 4 | 53 | 0 | 9 | 5 | 8 | 16 | 7 | 1 | 47 |
Mount Provender | P6 | 104 | 5 | 0 | 2 | 1 | 53 | 0 | 14 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 |
Mount Provender | P7 | 89 | 0 | 2 | 0 | 0 | 40 | 0 | 44 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
Mount Provender | P8 | 67 | 0 | 0 | 0 | 1 | 46 | 0 | 39 | 4 | 91 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 9 |
Mount Provender | P9 | 101 | 0 | 1 | 3 | 0 | 38 | 0 | 30 | 4 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 |
Mount Provender | P10 | 114 | 0 | 0 | 4 | 0 | 23 | 0 | 7 | 5 | 39 | 0 | 26 | 0 | 0 | 0 | 0 | 0 | 61 |
Mount Provender | P11 | 102 | 0 | 0 | 0 | 0 | 55 | 0 | 5 | 5 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 |
Mount Provender | P12 | 99 | 0 | 0 | 1 | 0 | 22 | 0 | 57 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 |
Mount Provender | P13 | 75 | 0 | 0 | 0 | 0 | 15 | 0 | 73 | 1 | 89 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 11 |
Mount Provender | P15 | 156 | 0 | 1 | 4 | 0 | 49 | 1 | 12 | 1 | 60 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 32 |
Mount Provender | P17 | 127 | 0 | 2 | 0 | 0 | 56 | 2 | 23 | 2 | 83 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 17 |
Mount Provender | P18 | 132 | 0 | 0 | 0 | 0 | 19 | 0 | 3 | 0 | 22 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 110 |
Lake Lundstroem, Mount Gass | GASS | 74 | 30 | 0 | 14 | 0 | 0 | 3 | 24 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 27 |