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| Detailed Seamount Information |
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| Wodejebato Guyot |    |
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| Index | SMNT-119N-1649E |
Classification | Large B1 Guyot |
| Location | 11º 55.95' N
164º 51.72' E |
Elongation
Irregularity | 1.48 ± 0.05
1.28 ± 0.10 |
| Plate Age | 170.2 - 172.0 Ma |
Oceanic Province | Abyssal Plain |
| Region | West Pacific Seamount Province |
Alternative Names | Sylvania |
| Plate | Pacific Plate |
Age | 82 Ma |
| Tectonic Setting | Hotspot Trail |
Seamount Top | 1290 m |
| Volume | 12476 km3 |
Ocean Bottom | 4505 m |
Shelf Edge
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Volcanic Activity | Extinct |
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| | Description | | Wodejebato Guyot is located at 11¿ 55.9' N, 164¿ 51.7' E and is part of the West Pacific Seamount Province on the Pacific Plate. It is 3215 m high with the top at -1290 m and ocean bottom at -4505 m. The seamount is large with a volume of 12475 km3. It is relatively round with very little elongation and an azimuth of approximately 134¿. The edges are slightly irregular. |
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Wodejebato Guyot -- Multibeam data merged with predicted satellite bathymetry |
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Wodejebato Guyot -- Multibeam bathymetry |
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Wodejebato Guyot -- Predicted satellite bathymetry |
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Wodejebato Guyot -- Residual bathymetry |
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Wodejebato Guyot -- Multibeam data merged with predicted satellite bathymetry |
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Wodejebato Guyot -- Multibeam bathymetry |
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Wodejebato Guyot -- Predicted satellite bathymetry |
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Wodejebato Guyot -- Residual bathymetry |
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Clouard, V. and Bonneville, A. (2001). Ages of seamounts, islands and plateaus on the Pacific plate. 1-42. |
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Keating, B.H. (1987). Summary of radiometric ages from the Pacific. In: Intergovernmental Oceanographic Comission technical series. UNESCO. 32. |
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Koppers, A.A.P. (1998). 40Ar/39Ar Geochronology and Isotope Geochemistry of the West Pacific Seamount Province Implications for Absolute Pacific Plate Motions and the Motions of Hotspots. Vrije Universiteit, Amsterdam. 263pp. |
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Lincoln, J.M., Schlanger, S.O., Bergerson, D., Coogan, A.H. and Premoli-Silva, I. (1989). Cretaceous foundations and multiple periods of uplift in the northern Marshall Islands, West Central Pacific. Abstracts with Programs, Geological Society of America 21(6): 195. |
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| Depth |
Azimuth |
Area |
Length |
Width |
Elongation |
Contour |
Ellipse |
Irregularity |
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| m |
degrees |
km2 |
km |
km |
ratio |
km |
km |
ratio |
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| 2576 |
134.8 |
2021.0 |
67.1 |
44.5 |
1.507 |
228.4 |
164.4 |
1.389 |
| 2898 |
134.5 |
2392.6 |
71.6 |
47.6 |
1.506 |
229.1 |
178.8 |
1.281 |
| 3219 |
134.0 |
2823.1 |
75.6 |
53.1 |
1.423 |
228.2 |
192.7 |
1.184 |
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| 3 % Multibeam Coverage |
1.48 ± 0.05 |
1.28 ± 0.10 |
| 3215 m High |
| 1 Summit |
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