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  • Friday, February 26, 2021
  • 3:30 PM–4:30 PM

Summary: Mid-oceanic ridge system are mountain chains that characterize crustal boundaries between diverging tectonic plates. Using global imagery sets, the morphology of these ridge systems and their relationship to the change in earth’s gravity latitudinally are examined to propose an additional component of magma generation below diverging systems. 

Join us on Zoom:  https://zoom.us/j/97264495518?pwd=YWVJMi9EdG1DTmFJeGsxQUtSOHpvQT09

February 2021
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