440 likes | 706 Views
Morphological Interpretation of Seamounts in American Samoa: Inferring Genesis Mechanisms through Shape and Distribution Analysis. Jed Roberts Master’s Candidate in Geography Department of Geosciences Oregon State University AAG San Francisco - April 19, 2007. Presentation Overview.
E N D
Morphological Interpretation of Seamounts in American Samoa: Inferring Genesis Mechanisms through Shape and Distribution Analysis Jed Roberts Master’s Candidate in Geography Department of Geosciences Oregon State University AAG San Francisco - April 19, 2007
Study Area Image produced by the U.S. National Park Service
Study Area Eastern Volcanic Province (American Samoa) Western Volcanic Province (Samoa) Image produced by the U.S. National Park Service
Tectonic Setting Image modified from Sandwell and Smith
Controversy Artwork by Jayne Doucette, Woods Hole Oceanographic Institution Artwork by Naoto Hirano, Scripps Institution of Oceanography
Multibeam Data Merged with Sandwell and Smith 1km resolution predicted bathymetry Image created using Fledermaus Data source: The Seamount Catalog www.earthref.org
Multibeam Data With 210m resolution swaths isolated Image created using Fledermaus Data source: The Seamount Catalog www.earthref.org
Methods | Identifying Seamounts Slope Surface Map created in Fledermaus Data source: The Seamount Catalog www.earthref.org
Methods | Identifying Seamounts 51 Seamounts Selected Map created in Fledermaus Data source: The Seamount Catalog www.earthref.org
Methods | Characterizing Seamounts Plan View Cross-sectional View Images created in Fledermaus
Methods | Characterizing Seamounts Azimuth Angle Summit Width Slope Right Slope Left Height Base Width Base Depth Images created in Fledermaus
Methods | Distribution Analysis 100-600 m range
Methods | Distribution Analysis Calculation of Area by -2640 m Cutoff Total area before depth cutoff: 27,181 km2 Total area after depth cutoff: 22,745 km2 Map created in Fledermaus Data source: The Seamount Catalog www.earthref.org
Results | Distribution Analysis ν0 = 2.6 ± 0.2 (per 1000 km2) ß-1 = 138 m
Results | Distribution Analysis ASSC is the American Samoa Seamount Chain, MAR is the Mid-Atlantic Ridge, ESC is the Easter Seamount Chain, EPR is the East Pacific Rise
Results | Interpretation Directional Trends Map created in Fledermaus Data source: The Seamount Catalog www.earthref.org
References Abers, G. A., Parsons, B., and Weissel, J. K. 1988. Seamount abundances and distributions in the southeast Pacific. Earth and Planetary Science Letters. 87: 137-51. Bemis, K. G., and Smith, D. K. 1993. Production of small volcanoes in the Superswell region of the South Pacific. Earth and Planetary Science Letters. 118: 251-62. Hart, S. R., Staudigel, H., Koppers, A. A. P., Blusztajn, J., Baker, E. T., Workman, R., Jackson, M., Hauri, E., Kurz, M., Sims, K., Fornari, D., Saal, A., and Lyons, S. 2000. Vailulu'u undersea volcano: The New Samoa. Geochemistry Geophysics Geosystems. 1(12): 2000GC000108. Hart, S. R., Coetzee, M., Workman, R. K., Blusztajn, J., Johnson, K. T. M., Sinton, J. M., Steinberger, B., and Hawkins, J. W. 2004. Genesis of the Western Samoa seamount province: age, geochemical fingerprint and tectonics. Earth and Planetary Science Letters. 227: 37-56. Hirano, N., Takahashi, E., Yamamoto, J., Abe, N., Ingle, S.P., Kaneoka, I., Hirata, T., Kimura, J., Ishii, T., Ogawa, Y., Machida, S., and Suyehiro, K. 2006. Volcanism in Response to Plate Flexure. Science. 313: 1426-28. Jaroslow, G. E., Smith, D. K., and Tucholke, B. E. 2000. Record of seamount production and off-axis evolution in the western North Atlantic Ocean, 25º25'-27º10'N. Journal of Geophysical Research. 105(B2): 2721-36. Kleinrock, M. C., and Brooks, B. A. 1994. Construction and destruction of volcanic knobs at the Cocos-Nazca spreading system near 95ºW. Geophysical Research Letters. 21(21): 2307-10. Magde, L. S., and Smith, D. K. 1995. Seamount volcanism at the Reykjanes Ridge: Relationship to the Iceland hot spot. Journal of Geophyical Research. 100(B5): 8449-68.
References Natland, J. H. 1980. The progression of volcanism in the Samoan linear volcanic chain. American Journal of Science. 280-A: 709-35. Natland, J. H. 2004. The Samoan Chain: A Shallow Lithospheric Fracture System. www.mantleplumes.org (last accessed March 11, 2006). Rappaport, Y., Naar, D. F., Barton, C. C., Liu, Z. J., and Hey, R. N. 1997. Mophology and distrubution of seamounts surrounding Easter Island. Journal of Geophysical Research. 102(B11): 24,713-28. Scheirer, D. S., and Macdonald, K. C. 1995. Near-axis seamounts on the flanks of the East Pacific Rise, 8ºN to 17ºN. Journal of Geophysical Research. 100(B2): 2239-59. Scheirer, D. S., MacDonald, K. C., Forsyth, D. W., and Shen, Y. 1996. Abundant Seamounts of the Rano Rahi Seamount Field Near the Southern East Pacific Rise , 15º S to 19º S. Marine Geophysical Researches. 18: 13-52. Smith, D. K. 1988. Shape analysis of Pacific seamounts. Earth and Planetary Science Letters. 90: 457-66. Smith, D. K., and Jordan, T. H. 1988. Seamount Statistics in the Pacific Ocean. Journal of Geophysical Research. 93(B4): 2899-918. Smith, D. K., and Cann, J. R. 1990. Hundreds of small volcanoes on the median valley floor of the Mid-Atlantic Ridge at 24º-30º N. Nature. 348: 152-5. Smith, D. K., and Cann, J. R. 1992. The Role of Seamount Volcanism in Crustal Construction at the Mid-Atlantic Ridge (24º-30ºN). Journal of Geophyical Research. 97(B2): 1645-58.
References Walker, G. P. L., and Eyre, P. R. 1995. Dike complexes in American Samoa. Journal of Volcanology and Geothermal Research. 69: 241-54. Workman, R. K., Hart, S. R., Jackson, M., Regelous, M., Farley, K. A., Blusztajn, J., Kurz, M., and Staudigel, H. 2004. Recycles metasomatized lithosphere as the origin of the Enriched Mantle II (EM2) end-member: Evidence from the Samoan Volcanic Chain. Geochemistry Geophysics Geosystems. 5(4): 2003GC000623.