يبلغ طولها 300 كيلومتر (190 ميل) وارتفاعها 4.3 كيلومتر (2.7 ميل)، وتمتد في اتجاه الشمال الشرقي والجنوب الغربي ولها سطحان مسطحان؛ يرتفع إلى عمق لا يقل عن 1،443 متر (4،730 قدم).[2]
^ McKenzie, J.; Bernoulli, D.; Schlanger, S.O. (1980). "Shallow-Water Carbonate Sediments from the Emperor Seamounts: Their Diagenesis and Paleogeographic Significance" (PDF). Initial Reports of the Deep Sea Drilling Project, 55. Initial Reports of the Deep Sea Drilling Project. 55. U.S. Government Printing Office. p. 415. doi:10.2973/dsdp.proc.55.115.1980. Retrieved 2018-10-03.
^ Zemmels, I.; Cook, H.E. (1973). "X-Ray Mineralogy of Sediments from the Central Pacific Ocean" (PDF). Initial Reports of the Deep Sea Drilling Project, 17. Initial Reports of the Deep Sea Drilling Project. 17. U.S. Government Printing Office. p. 518. doi:10.2973/dsdp.proc.17.118.1973. Retrieved 2018-10-03.
^ Israelson, C.; Buchardt, B.; Haggerty, J.A.; Pearson, P.N. (1995). "Carbonate and Pore-Water Geochemistry of Pelagic Caps at Limalok and Lo-En Guyots, Western Pacific" (PDF). Proceedings of the Ocean Drilling Program, 144 Scientific Results. Proceedings of the Ocean Drilling Program. 144. Ocean Drilling Program. p. 737. doi:10.2973/odp.proc.sr.144.050.1995. Retrieved 2018-10-03.
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