UNDERSEA FEATURE NAME PROPOSAL (Sea NOTE overleaf) Matoba Seamount

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2-1 INTERNATIONAL HYDROGRAPHIC ORGANIZATION INTERGOVERNMENTAL OCEANOGRAPHIC COMMISSION (of UNESCO) Note: The boxes will expand as you fill the form. UNDERSEA FEATURE NAME PROPOSAL (Sea NOTE overleaf) Name Proposed: Hattori Seamount Ocean or Sea: Northwest Pacific Ocean Geometry that best defines the feature (Yes/No) : Point Line Polygon Multiple points Multiple lines* Multiple polygons* Yes * Geometry should be clearly distinguished when providing the coordinates below. Coordinates: Lat. (e.g. 63 32.6 N) 27 41.35'N 27 44.94'N 27 49.19'N 27 49.40'N 27 47.01'N 27 34.59'N 27 29.02'N 27 24.24'N 27 27.05'N 27 38.48'N 27 41.35'N Combination of geometries* Long. (e.g. 046 21.3 W) 152 40.62'E 152 46.22'E 152 57.28'E 153 01.71'E 153 05.31'E 153 08.42'E 153 06.70'E 152 49.91'E 152 45.12'E 152 43.27'E 152 40.62'E Feature Description: Maximum Depth : 6,000 m Steepness : Minimum Depth : 1,938 m Shape : Distorted conical Total Relief : 4,062 m Dimension/Size : 50 km 45 km Associated Features: Matoba Seamount Chart/Map References: Shown Named on Map/Chart: 6727 Shown Unnamed on Map/Chart: Within Area of Map/Chart: W48 Reason for Choice of Name (if a person, state how associated with the feature to be named): Named after a geologist/technician the late Dr. Mutsuo Hattori. Discovery Facts: Discovery Date: Feb. 1999 Discoverer (Individual, Ship): The Japanese survey vessel Shoyo Supporting Survey Data, including Track Controls: Date of Survey: Feb. Mar. 1999 Survey Ship: The Japanese survey vessel Shoyo Sounding Equipement: Multibeam echo sounder Seabeam 2112 Type of Navigation: GPS with Selective Availability Estimated Horizontal Accuracy (nm): 0.054 nm (100 m) Survey Track Spacing: Less than 10 nm Supporting material can be submitted as Annex in analog or digital form.

2-2 Proposer(s): Name(s): JCUFN Date: Aug. 17, 2016 E-mail: ico@jodc.go.jp Organization and Address: Concurrer (name, e-mail, organization and address): Hydrographic and Oceanographic Department, Japan Coast Guard Kasumigaseki 3-1-1,Chiyoda-ku, Tokyo 100-8932, Japan Remarks: The position of the summit is located in (27 36.16 N, 152 52.43 E). NOTE : This form should be forwarded, when completed : a) If the undersea feature is located inside the external limit of the territorial sea :- to your "National Authority for Approval of Undersea Feature Names" (see page 2-9) or, if this does not exist or is not known, either to the IHB or to the IOC (see addresses below); b) If at least 50 % of the undersea feature is located outside the external limits of the territorial sea :- to the IHB or to the IOC, at the following addresses : International Hydrographic Bureau (IHB) 4, Quai Antoine 1er B.P. 445 MC 98011 MONACO CEDEX Principality of MONACO Fax: +377 93 10 81 40 E-mail: info@ihb.mc Intergovernmental Oceanographic Commission (IOC) UNESCO Place de Fontenoy 75700 PARIS France Fax: +33 1 45 68 58 12 E-mail: info@unesco.org

2-3 Personal history of the late Dr. Mutsuo Hattori Given name: Mutsuo Family name: Hatorri 1939 Born March 2014 Diseased Education 1962 B.S., Tohoku University 1967 PhD, Tohoku University Professional carrier: 1972 Resercher, Japan Marine Science and Technology Center (JAMSTEC) 1998 Retired from JAMSTEC 1998-2002 Techincal advisor, JAMSTEC Remarks: He was a geologist/technician working for JAMSTEC. In his early career, he studied the Sugami Bay using the submersible Shinkai 2000, describing the geology and chemosynthetic biological communities. The Sagami Bay is closely located to Tokyo, which is one of the deepest bay in the world, due to the presence of the Sagami Trough, a subduction boundary between the Philippine Sea and North American Plates. He also contributed to the development of the first Japan-made 3000 m- class ROV, Dolphin 3K in late 1980 s. Futhermore, he also contributed to develop a technique to measure seafloor radioactivity. List of selected publications: Hattori, M., Y. Kanie, T. Oba, and K. Akimoto, Environmental conditions of carbonates and chemosynthetic animal communities associated with cold seepage zones along the subduction zone in Sagami Bay, central Japan, Fossils, 60, 13-22, 1996. Hatorri, M., M. Okano, and O. Togawa, Sea bottom gamma ray measurement by NaI (Tl) Scintillation spectrometers installed on manned submersibles, ROV and sea bottom long term observatory, In Underwater Technology, 2000, UT 00, Proceedings of the 2000 International Symposium on IEEE, 212-217, 2000. Nomoto, M. and M. Hattori, A dep ROV Dolphin 3K : design and performance analysis, IEEE Journal of Oceanci Engineering, 11, 373-391, 1986.

2-4 Fig. 1. Bathymetric map of the Hattori Seamount. Contours are in 100 m.

Fig. 2. Bathymetric map of the Hattori Seamount, shown with track lines. Contours are in 100 m. 2-5

Fig. 3. Bathymetric profile across the Hattori Seamount. 2-6