Kay 1994, hlm. 59"Actually, Loihi has been known and charted on topographical maps for many years, one of eight of eight or 10 undersea rises in the waters southeast of Hawaii. All were assumed to be very old and geologically dead. But in 1952, spidery tracings on the seismometers at the Hawaii Volcano Observatory [PS, Nov '78] indicated an earthquake swarm there, and Loihi was given its name, (...)" Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Kay 1994, hlm. 86"Taken together, these theories suggest that the apparently youngest volcano in the Hawaiian chain, the underwater Loihi, lies directly above a hot spot, and that the older volcanoes in the group have been progressively carried away to the northwest by plate movement." Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Kay 1994, hlm. 86b"His results quantitatively confirmed by the observation by James D. Dana, a nineteenth-century naturalist, that the islands did indeed increase in age to the northwest and showed the rate of plate movement was about four inches a year." Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
"Global Volcanism Program | Loihi". Smithsonian Institution | Global Volcanism Program (dalam bahasa Inggris). Diarsipkan dari versi asli tanggal 2023-03-26. Diakses tanggal 2020-01-09.
"Global Volcanism Program | Loihi". Smithsonian Institution | Global Volcanism Program (dalam bahasa Inggris). Diarsipkan dari versi asli tanggal 2023-03-26. Diakses tanggal 2020-01-09.
Stauffer 1987, hlm. 133"Loihi Seamount is a young (probably less than 0,5 Ma), active, submarine volcano on the southern extension of the Hawaiian hot spot (...)" Stauffer, Peter H.; Decker, Robert W.; Wright, Thomas Llewellyn (1987). Volcanism in Hawaii (dalam bahasa Inggris). U.S. G.P.O. OCLC600652275.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Kay 1994, hlm. 59"Actually, Loihi has been known and charted on topographical maps for many years, one of eight of eight or 10 undersea rises in the waters southeast of Hawaii. All were assumed to be very old and geologically dead. But in 1952, spidery tracings on the seismometers at the Hawaii Volcano Observatory [PS, Nov '78] indicated an earthquake swarm there, and Loihi was given its name, (...)" Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Stauffer 1987, hlm. 133b"The name Loihi, meaning long in Hawaiian, was first introduced by Emery (1955) to explain the elongate shape of the seamount." Stauffer, Peter H.; Decker, Robert W.; Wright, Thomas Llewellyn (1987). Volcanism in Hawaii (dalam bahasa Inggris). U.S. G.P.O. OCLC600652275.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Kay 1994, hlm. 86"Taken together, these theories suggest that the apparently youngest volcano in the Hawaiian chain, the underwater Loihi, lies directly above a hot spot, and that the older volcanoes in the group have been progressively carried away to the northwest by plate movement." Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
Kay 1994, hlm. 86b"His results quantitatively confirmed by the observation by James D. Dana, a nineteenth-century naturalist, that the islands did indeed increase in age to the northwest and showed the rate of plate movement was about four inches a year." Kay, E. Alison (1994). A Natural history of the Hawaiian Islands : selected readings II (dalam bahasa Inggris). Honolulu: University of Hawaii Press. ISBN0-8248-1659-5. OCLC29913031.Parameter |url-status= yang tidak diketahui akan diabaikan (bantuan)
