A precise bathymetric map of the world’s deepest seafloor, Challenger Deep in the Mariana Trench

Data from three bathymetric surveys by R/V Kairei using a 12-kHz multibeam echosounder and differential GPS were used to create an improved topographic model of the Challenger Deep in the southwestern part of the Mariana Trench, which is known as the deepest seafloor in the world. The strike of most of the elongated structures related to plate bending accompanied by subduction of the Pacific plate is N70°E and is not parallel to the trench axis. The bending-related structures were formed by reactivation of seafloor spreading fabric. Challenger Deep consists of three en echelon depressions along the trench axis, each of which is 6–10 km long, about 2 km wide, and deeper than 10,850 m. The eastern depression is the deepest, with a depth of 10,920 ± 5 m.

[1]  P. Bird An updated digital model of plate boundaries , 2003 .

[2]  M. Nakanishi Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean , 2011 .

[3]  Robert L. Fisher Meanwhile, Back on the Surface: Further Notes on the Sounding of Trenches , 2009 .

[4]  V. A. D. Grosso New equation for the speed of sound in natural waters (with comparisons to other equations) , 1974 .

[5]  K. Okino,et al.  Morphology and origin of the Challenger Deep in the Southern Mariana Trench , 2002 .

[6]  John Murray,et al.  Report on the scientific results of the voyage of H.M.S. Challenger during the years 1873-76, under the command of Captain George S. Nares and the late Captain Frank Tourle Thomson : a summary of the scientific results, , 2010 .

[7]  Robert S. Dietz,et al.  Seven miles down : the story of the bathyscaph Trieste , 1961 .

[8]  Louis L. Whitcomb,et al.  Journey to the Challenger Deep: 50 Years Later With the Nereus Hybrid Remotely Operated Vehicle , 2009 .

[9]  Meghan S. Miller,et al.  Three‐dimensional visualization of a near‐vertical slab tear beneath the southern Mariana arc , 2006 .

[10]  Dale N. Chayes,et al.  Improved processing of Hydrosweep DS multibeam data on the R/V Maurice Ewing , 1996 .

[11]  Y. Ogawa,et al.  Outer slope faulting associated with the western Kuril and Japan trenches , 1998 .

[12]  K. Taira,et al.  Deep CTD Casts in the Challenger Deep, Mariana Trench , 2005 .

[13]  Kazuo Kobayashi,et al.  Magnetic anomaly lineations from Late Jurassic to Early Cretaceous in the west-central Pacific Ocean , 1992 .

[14]  D. Masson Fault patterns at outer trench walls , 1991 .

[15]  Fernando Martinez,et al.  Why is the Challenger Deep so deep , 2003 .

[16]  W. Weinrebe,et al.  Relationship between bend‐faulting at trenches and intermediate‐depth seismicity , 2005 .

[17]  Walter H. F. Smith,et al.  New, improved version of generic mapping tools released , 1998 .

[18]  Dana R. Yoerger,et al.  Navigation and control of the Nereus hybrid underwater vehicle for global ocean science to 10,903 m depth: Preliminary results , 2010, 2010 IEEE International Conference on Robotics and Automation.

[19]  Dana R. Yoerger,et al.  Field trials of the Nereus hybrid underwater robotic vehicle in the challenger deep of the Mariana Trench , 2009, OCEANS 2009.

[20]  Kazuo Kobayashi,et al.  A new Mesozoic isochron chart of the northwestern Pacific Ocean: Paleomagnetic and tectonic implications , 1992 .

[21]  Taro Aoki,et al.  The sea trial of "KAIKO", the full ocean depth research ROV , 1995, 'Challenges of Our Changing Global Environment'. Conference Proceedings. OCEANS '95 MTS/IEEE.

[22]  Walter H. F. Smith,et al.  Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings , 1997 .

[23]  Zohar Gvirtzman,et al.  Bathymetry of Mariana trench‐arc system and formation of the Challenger Deep as a consequence of weak plate coupling , 2004 .

[24]  James P. Barry,et al.  Revisiting the Challenger Deep Using the ROV Kaiko , 2009 .