Propagated ridge structure and faulting as a control on sediment accumulation

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Propagated ridge structure and faulting as a control on sediment accumulation

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dc.contributor.author Hearn, Casey K.
dc.date.accessioned 2012-08-24T23:26:24Z
dc.date.available 2012-08-24T23:26:24Z
dc.date.issued 2012-06
dc.identifier.uri http://hdl.handle.net/1773/20484
dc.description Senior thesis written for Oceanography 444 en_US
dc.description.abstract [Author's Abstract] In the Eastern Tropical North Pacific within the Sea of Cortez lies a unique geologic feature. Three tectonic plates spread and twist apart over millions of years as brand new sea floor is created, leaving a wide range of unique topographies. Three thousand meters above, in the surface ocean, a rain of biological waste products sinks slowly down to blanket the sea floor in a thickening layer of organic ooze. In March of 2012, I embarked on a research cruise aboard the Thomas G. Thompson to study the effect of seafloor topography on the distribution of sediment in this area by using sonar imaging. The high resolution multibeam sonar on the Thompson enabled me to construct datasets containing topography and sediment significance across the area. By comparing these data through a series of measurements describing different aspects of the topography, I was able to establish relationships between geologic features and the pattern of sediment. en_US
dc.language.iso en_US en_US
dc.relation.ispartofseries Proceedings from the University of Washington School of Oceanography Senior Thesis, Academic Year 2011-2012;
dc.subject Marine sediments--Sea of Cortez--Observations en_US
dc.subject Submarine topography en_US
dc.title Propagated ridge structure and faulting as a control on sediment accumulation en_US
dc.type Article en_US


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