Garrett Ito

Associate Professor

Geology and Geophysics Department
SOEST,1680 East-West Rd.
University of Hawaii, Honolulu, HI 96822
808-956-9717 (Office); 808-956-9717 (Fax)
gito@hawaii.edu


Education

B.A. Physics, Colorado College, 1989

Ph.D. Marine Geophysics, MIT/Woods Hole Joint Program, 1996

Professional History

2004- present: Associate Professor, Geology and Geophysics Department, SOEST, Univ. of Hawaii, Honolulu, HI

2002- 2004: Assistant Professor, Geology and Geophysics Department, SOEST, Univ. of Hawaii, Honolulu, HI

2000-2001: Assistant Professor, Department of Geology, University of California, Davis, CA

1996-1999: SOEST Young Investigator, Department of Geology and Geophysics, Univ. of Hawaii, Honolulu, HI

1990-1996: Research Assistant, MIT/WHOI Joint Program in Oceanography


Publications


Research

My research focuses on the mantle and lithospheric processes controlling the origin and evolution of hotspots and mid-ocean ridges. I use a variety of geophysical and geochemical data to characterize crustal and mantle density structure. These analyses are integrated with computer simulations and laboratory experiments, which examine the asthenospheric and lithospheric processes.

Faulting and magmatism at mid-ocean ridges:  In collaborating with Mark Behn, I am using numerical models to study how magmatism and faulting shapes the morphology of mid-ocean ridges.  Mid-ocean ridges are where the tectonic plates are diverging and generating all of the seafloor.

 

Click here for movie

Oceanic Basalt Geochemistry: J. Mahoney and I have developed theoretical models to explore the consequence of mantle convection and melting of a heterogeneous mantle source.  This work is showing large portion of the rich geochemical diversity found in mid-ocean ridge basalts (MORBs) and ocean island basalts (OIBs) can arise out of the melting process alone, independent of any variation in the composition of the mantle source.

 

Magma Transport: My colleagues and I have used both laboratory experiments and numerical models to study magma transport in the lithospheric portion of the mantle and crust.

Hotspot-Ridge Interaction: I use a combination of geophysical data (bathymetry, gravity, and seismics) with 3-D computer simulations of upper mantle flow and melting to examine the dynamics of plume-ridge interaction.

During our research cruise to the Galapagos plume-ridge system, we collected crustal seismic data and sampled ridge-axis basalts. Together these data will help us understand processes of mantle flow and magma generation at this classic plume-ridge system.  My student and I are using the multi-channel reflection data to reveal the detailed structure of the crust, including how magma is being stored.



 




3-D computer models are used to examine the causes for the V-shaped crustal features that extend hundreds of kilometers south of Iceland along the Mid-Atlantic Ridge. The models incorporate a pulsing mantle plume and a high-viscosity, dehydrated melting zone. These two elements are predicted to be key to the formation of the V-shaped features.







 


Graduate Students

Todd Bianco (Ph. D): Todd is examining mechanisms of hotspot volcanism, alternative to melting of an upwelling mantle plume. One mechanism is mantle decompression beneath the flexural arch surrounding growing shield volcanoes. Todd has developed models of mantle flow and melting beneath the flexural arch, which predict the volume and geochemistry of the magmas produced; see Bianco et al,[2005].  Todd is also using numerical models to study how 3-D upper mantle convection and melting contributes to geochemical variations at hotspots such as Hawaii and Iceland. 

Model geometry & melting rates of 2 components

Surface magma composition

 

 

 

Eric Mittelstaedt (Ph. D.): Eric is studying how the interaction between hotspots and mid-ocean ridges influences off-axis volcanism and shapes the geometry of the mid-ocean ridge plate boundary. He is developing numerical models to examine how mantle plumes stress the lithosphere and how this influences the ability of magma to penetrate to the surface [Mittelstaedt and Ito, 2005]. He is also using finite difference models to study how magmatism can influence the rheology of the plate to promote changes in the axis of seafloor spreading [Mittelstaedt et al., 2008]

 

Ashton Flinders (M.S.) Ashton is using gravity to study the internal volcanic structure of the Island of Kauai and the bathymetric swells surrounding the island. 


Courses Instructed

GG304: Physics of the Earth and Planets Spring 2006

GG681: Continuum Mechanics in Geophysics , Fall 2004

GG410/610 Student Seminar, Spring 2006

GG711 Magma and Mantle Dynamics, Fall 2006