. . . . . . . . . . . . "Allison Guyot"@en . . . . . . . . . "179.3300018310547"^^ . . . . . . . . . . . . . . . "44130"^^ . . "Allison"@en . . . . "58684856"^^ . . . . "Allison Guyot (formerly known as Navoceano Guyot) is a tablemount (guyot) in the underwater Mid-Pacific Mountains of the Pacific Ocean. It is a trapezoidal flat mountain rising 1,500 metres above the seafloor to a depth of less than 1,500 m, with a summit platform 35 by 70 kilometres wide. The Mid-Pacific Mountains lie west of Hawaii and northeast of the Marshall Islands, but at the time of their formation were located in the Southern Hemisphere."@en . . . . . . . . . . . . . . "18.26000022888184"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . "1.5"^^ . . . . . . . . . . . . . "Allison Guyot (formerly known as Navoceano Guyot) is a tablemount (guyot) in the underwater Mid-Pacific Mountains of the Pacific Ocean. It is a trapezoidal flat mountain rising 1,500 metres above the seafloor to a depth of less than 1,500 m, with a summit platform 35 by 70 kilometres wide. The Mid-Pacific Mountains lie west of Hawaii and northeast of the Marshall Islands, but at the time of their formation were located in the Southern Hemisphere. The tablemount was probably formed by a hotspot in the present-day Southern Pacific before plate tectonics moved it to its current location. Several hotspots, including the Easter, Marquesas and Society hotspots, may have been involved in the formation of the Mid-Pacific Mountains. Volcanic activity is dated to have occurred circa 111\u201385 million years ago and formed a volcanic island. Subsequently, carbonate deposition commenced as Allison Guyot subsided and eventually buried the island, forming an atoll-like structure and a carbonate platform. Among other animals, crocodilians lived on Allison Guyot. The platform emerged above sea level during the Albian and Turonian ages. It drowned about 99 \u00B1 2 million years ago for unknown reasons; possibly a phase of renewed emergence damaged the reefs, or it was located in unfavourable waters. Later, pelagic sedimentation commenced on the seamount and led to the deposition of sediments including limestone, ooze and sand, which bear traces of climatic events and ocean currents."@en . . . . . . . . "Allison Guyot"@en . . . . . . . . . . "250"^^ . "Pacific Ocean"@en . . . . . "Allison (en anglais Allison Guyot et anciennement Navoceano Guyot) est un guyot du plateau m\u00E9dio-pacifique, au centre de l'oc\u00E9an Pacifique Nord. C'est un mont sous-marin plat et trap\u00E9zo\u00EFdale s'\u00E9levant \u00E0 1 500 m\u00E8tres au-dessus du fond marin, avec une plate-forme sommitale de 35 sur 70 kilom\u00E8tres de large. Il se situe \u00E0 l'ouest d'Hawa\u00EF et au nord-est des \u00CEles Marshall. Il a probablement \u00E9t\u00E9 form\u00E9 par un point chaud dans l'oc\u00E9an Pacifique Sud actuel avant que la tectonique des plaques ne la d\u00E9place \u00E0 son emplacement actuel. De l'activit\u00E9 volcanique y aurait eu lieu il y a environ 111 \u00E0 85 millions d'ann\u00E9es et aurait form\u00E9 une \u00EEle volcanique. La plate-forme est apparue au-dessus du niveau de la mer au cours des \u00E9tages stratigraphiques Albien et Turonien. Par la suite, le d\u00E9p\u00F4t de carbonate a commenc\u00E9 lorsque Allison s'est affaiss\u00E9 et a finalement enseveli l'\u00EEle sous l'eau, formant ainsi une structure semblable \u00E0 un atoll et une plateforme carbonat\u00E9e."@fr . . . . . . . . . . . "POINT(179.33000183105 18.260000228882)"^^ . . . . . . . . . "Guyot Allison"@fr . . . . . . . . . . . . . . . . . . . . . . . . . . . . "1110617897"^^ . . . . "35"^^ . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . "18.26 179.33" . . . . . . . . . . . . . "Allison (en anglais Allison Guyot et anciennement Navoceano Guyot) est un guyot du plateau m\u00E9dio-pacifique, au centre de l'oc\u00E9an Pacifique Nord. C'est un mont sous-marin plat et trap\u00E9zo\u00EFdale s'\u00E9levant \u00E0 1 500 m\u00E8tres au-dessus du fond marin, avec une plate-forme sommitale de 35 sur 70 kilom\u00E8tres de large. Il se situe \u00E0 l'ouest d'Hawa\u00EF et au nord-est des \u00CEles Marshall."@fr . . . . . . . . . . . . . . . . .