Eratosthenes Seamount
| Eratosthenes Seamount | |
|---|---|
|
Bathymetric features south of Cyprus | |
| Summit depth | 690 m (2,264 ft) |
| Height | 2,000 m (6,562 ft) |
| Summit area | 120 km × 80 km (75 mi × 50 mi) |
| Location | |
| Location | Eastern Mediterranean |
| Group | Eratosthenes Abyssal Plain |
| Country | 33°40′N 32°40′E / 33.667°N 32.667°ECoordinates: 33°40′N 32°40′E / 33.667°N 32.667°E |
| Geology | |
| Type | Seamount (continental fragment) |
The Eratosthenes Seamount is a seamount in the Eastern Mediterranean about 100 km south of western Cyprus. It is a large, submerged massif, about 120 km long and 80 km wide. Its peak lies at the depth of 690 m and it rises 2000 m above the surrounding seafloor, which is located at the depth of up to 2,700 m and is a part of the Eratosthenes Abyssal Plain. It is one of the largest features on the Eastern Mediterranean seafloor.
See also
- CenSeam
- Ferdinandea
References
- Mart, Yossi and Robertson, Alastair H. F. (1998). Eratosthenes Seamount: an oceanographic yardstick recording the Late Mesozoic-Tertiary geological history of the Eastern Mediterranean, in Robertson, A.H.F., Emeis, K.-C., Richter, C., and Camerlenghi, A. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 160, Chapter 52, 701–708.
- Kempler, Ditza (1998). Eratosthenes Seamount: the possible spearhead of incipient continental collision in the Eastern Mediterranean, in Robertson, A.H.F., Emeis, K.-C., Richter, C., and Camerlenghi, A. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 160, Chapter 53, 709–721.
- Earthref entry