Tholi
Ionian tholi (hills) are named after mythological figures associated with fire or with the nymph Io.
| Tholus | Named after | Coordinates |
|---|---|---|
| Apis Tholus | Apis (Greek) | 10°54′S 347°53′W / 10.9°S 347.88°W / -10.9; -347.88 (Apis Tholus) |
| Inachus Tholus | Inachus (Greek) | 16°11′S 347°46′W / 16.18°S 347.76°W / -16.18; -347.76 (Inachus Tholus) |
| Tsui Goab Tholus | Tsui (Khoikhoi) | 0°06′S 163°00′W / 0.1°S 163.0°W / -0.1; -163.0 (Tsui Goab Tholus) |
Read more about this topic: List Of Geological Features On Io
Other articles related to "tholi":
List Of Geological Features On Venus - Tholi
... Azimua Tholi 34.05S 249.35E 40.0 2006 Sumerian underworld goddess ... Gerd Tholi 54.5S 291.5E 50.0 1997 Scandinavian sky maiden ... Grechukha Tholi 8.6S 255.8E 200.0 2000 Ukrainian field deity ...
... Azimua Tholi 34.05S 249.35E 40.0 2006 Sumerian underworld goddess ... Gerd Tholi 54.5S 291.5E 50.0 1997 Scandinavian sky maiden ... Grechukha Tholi 8.6S 255.8E 200.0 2000 Ukrainian field deity ...
List Of Mountains On Mars
... Tholi, plural of tholus a group of (usually not contiguous) small mountains. 271°29′E / 39.47°N 271.48°E / 39.47 271.48 (Pindus Mons) 16.5 Scandia Tholi 74°05′N 201°17′E / 74.09°N 201.28°E / 74.09 201.28 (Scandia ...
... Tholi, plural of tholus a group of (usually not contiguous) small mountains. 271°29′E / 39.47°N 271.48°E / 39.47 271.48 (Pindus Mons) 16.5 Scandia Tholi 74°05′N 201°17′E / 74.09°N 201.28°E / 74.09 201.28 (Scandia ...
Volcanism On Mars - Tharsis Volcanic Province - Tholi and Paterae
... large shield volcanoes, Tharsis contains a number of smaller volcanoes called tholi and paterae ... The tholi are dome-shaped edifices with flanks that are much steeper than the larger Tharsis shields ... The density of impact craters on many of the tholi indicate they are older than the large shields, having formed between late Noachian and early Hesperian times ...
... large shield volcanoes, Tharsis contains a number of smaller volcanoes called tholi and paterae ... The tholi are dome-shaped edifices with flanks that are much steeper than the larger Tharsis shields ... The density of impact craters on many of the tholi indicate they are older than the large shields, having formed between late Noachian and early Hesperian times ...
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