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  2. André Wink - Wikipedia

    en.wikipedia.org/wiki/André_Wink

    André Wink is an emeritus professor of history at University of Wisconsin, Madison. He is known for his studies on India and the Indian Ocean area, particularly over the medieval and early modern age (700 to 1800 CE). He is the author of a series of books published by Brill Academic, Oxford University Press, and Cambridge University Press on ...

  3. Marine sediment - Wikipedia

    en.wikipedia.org/wiki/Marine_sediment

    Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...

  4. Continental margin - Wikipedia

    en.wikipedia.org/wiki/Continental_margin

    A continental margin is the outer edge of continental crust abutting oceanic crust under coastal waters. It is one of the three major zones of the ocean floor, the other two being deep-ocean basins and mid-ocean ridges. The continental margin consists of three different features: the continental rise, the continental slope, and the continental ...

  5. Effects of climate change on oceans - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    Overview of climatic changes and their effects on the ocean. Regional effects are displayed in italics. [1] This NASA animation conveys Earth's oceanic processes as a driving force among Earth's interrelated systems. There are many effects of climate change on oceans. One of the main ones is an increase in ocean temperatures.

  6. Ocean - Wikipedia

    en.wikipedia.org/wiki/Ocean

    The ocean is a major driver of Earth's water cycle. Ocean water represents the largest body of water within the global water cycle (oceans contain 97% of Earth's water). Evaporation from the ocean moves water into the atmosphere to later rain back down onto land and the ocean. [68]

  7. Western Interior Seaway - Wikipedia

    en.wikipedia.org/wiki/Western_Interior_Seaway

    Western Interior Seaway. The Western Interior Seaway (also called the Cretaceous Seaway, the Niobraran Sea, the North American Inland Sea, and the Western Interior Sea) was a large inland sea that split the continent of North America into two landmasses for 34 million years. The ancient sea, which existed from the early Late Cretaceous (100 Ma ...

  8. Atlantic Ocean - Wikipedia

    en.wikipedia.org/wiki/Atlantic_Ocean

    The Atlantic Ocean is the second-largest of the world's five oceanic divisions, with an area of about 85,133,000 km 2 (32,870,000 sq mi). [ 2 ] It covers approximately 17% of Earth's surface and about 24% of its water surface area. During the Age of Discovery, it was known for separating the New World of the Americas (North America and South ...

  9. Oceanic crust - Wikipedia

    en.wikipedia.org/wiki/Oceanic_crust

    The lines represent tectonic plate boundaries. Oceanic crust is the uppermost layer of the oceanic portion of the tectonic plates. It is composed of the upper oceanic crust, with pillow lavas and a dike complex, and the lower oceanic crust, composed of troctolite, gabbro and ultramafic cumulates. [1][2] The crust overlies the rigid uppermost ...

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