|
Site
|
Location
|
Coordinates
|
Water
depth (m) |
Basement recovery (m)
|
Lithologic description
|
Paleoenvironment
|
Age (Ma)*
|
|---|---|---|---|---|---|---|---|
| 1136 | Southern Kerguelen Plateau | 59°39.1´S, 4°50.1´E | 1930.6 | 18.4 | Inflated pahoehoe flows of massive basalt | Subaerial | 119 |
| 1137 | Elan Bank | 56°50.0´S, 68°05.6´E | 1004.5 | 105.5 | Crystal vitric tuff and brecciated basalts | Subaerial | 108 |
| 1138 | Central Kerguelen Plateau | 53°33.1´S, 75°58.5´E | 1141.4 | 69.0 | Volcaniclastic deposits and multiple basalt flows | Subaerial | 100 |
| 1139 | Skiff Bank | 50°11.1´S, 63°56.2´E | 1415.3 | 87.3 | Altered volcaniclastic rocks and multiple basalt flows | Subaerial | 69 |
| 1140 | Northern Kerguelen Plateau | 46°15.6´S, 68°29.5´E | 2394.1 | 49.1 | Submarine pillow and massive basalts | Submarine | 34 |
| 1141 | Broken Ridge | 32°13.6´S, 97°07.7´E | 1196.9 | 39.1 | Altered basalts and mafic lava flows | Subaerial | 95 |
| 1142 | Broken Ridge | 32°13.9´S, 97°07.5´E | 1200.8 | 17.3 | Massive and pillowed basalt and volcanic breccia | Submarine? | 95 |
Note: * = new basement ages reported by Pringle and Duncan (2000) and Figure F1.