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Lecture 7. Marine Sediments
Lecture 7. Marine Sediments

...  Directed the Challenger Expedition (1872-1876)  First major scientific expedition  Globe-encircling voyage  Chemical, physical, and biological measurements and collections  Disproved Edward Forbes “azoic theory” by collecting sea life from waters as deep as 9000 m ...
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... experiences two high tides and two low tides of nearly equal level each lunar day. This type is more likely to occur when the moon is over the equator. Mixed semidiurnal tides = the coastline experiences successive high tides or low tides that are significantly different heights through the cycle. T ...
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... sometimes called "oxygen narios, there's one that gets minimum zones" where relatively little attention, plants, fish and other or­ but definitely has enormous ganisms would struggle to survive. potential consequences. It goes like this: The Now, in the new study, oceans are getting warm­ Long and h ...
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... continental rise into deep ocean basins. Among Earth’s flattest and smoothest regions an the least explored. Formed by particles of sediment slowly drifting onto the deep ocean floor. Most abyssal plains occur in the Atlantic and Indian oceans. Cover about 40% of the ocean floor Depths from 2,200 to ...
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... deposits fill in valleys and create flat seafloor areas called ______________________________ ...
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The Floors of the Oceans

... Bruce Heezen and Marie Tharp of LamontDoherty. Using thousands of sonar tracks, they produced physiographic charts of the ocean basins. These were later published in enhanced versions by the National Geographic Society, and are still widely used. ...
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Physical oceanography



Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.
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