PPT-Deep Sea Sediments Photomicographs

courtesy of Paula Worstell Scripps Institution of Oceanography and BOSCORF National Oceanographic Center Southampton UK and Ocean Drilling Program See httpwwwboscorforgrepositorycuratorialreferencepacifictransect. DEEP-SEA SEDIMENTS OF INDIAN OCEAN397Thus in the neighborhood of coral reefs, coral ooze and mud originate.In the open ocean the organic material consists almost exclusively ofthose constituents of th Photomicographs. courtesy of Paula . Worstell. , Scripps Institution of Oceanography and. BOSCORF, National Oceanographic Center, Southampton, UK and. Ocean Drilling Program. See:. http://www.boscorf.org/repository/curatorial-reference/pacific-transect. Features of the Ocean Floor. Continental Shelf. Zone . of shallow water where the ocean covers the end of the continent. . Shallow slope. Where most ocean life is found. Why?. Answer: Photic zone is the first 100 feet of water and allows sunlight to penetrate the water. . By; Byron Thompson. The Deep. Anything below 600ft; . Benthic. parts of the sea. Cold…really cold. Home to bioluminescent creatures . Where can you find this biome?. 71% of the earth is covered in water. The End of the Joan of Arc . Teacher Recruitment Strategy. BEST-NC Innovation Lab. September 28, 2016. Cary, NC. Southern Regional Education Board. Andy Baxter, Vice President for Educator Effectiveness. Original Words by Samuel Trevor Francis (1834-1925). Music, chorus, and alternate words by Bob Kauflin.. © 2008 Integrity’s Praise! Music/Sovereign Grace Praise (BMI). Sovereign Grace Music, a division of Sovereign Grace Ministries.. Presented by: Derek . Lumary. Rudy Marmolejo. . Jazmin. . Quijada. What is a Marine Sediment? Why are they important?. Marine Sediments are particles of organic or inorganic origins that . Sediment . in the . Sea. -Sediment is classified in two ways: . Size. and . Origin. -. Size is based on the . Wentworth. grain-size . scale. -Size classification divides sediment by grain size into gravel, sand, and clay. . Rajdeep. . Dasgupta. CIDER Community Workshop, CA. May 08, 2016. Volcanic degassing. hazards. long-term climate. Bio-essential elements. Origin of life. Mantle melting. Chemical differentiation. Properties of asthenosphere. Chapter 5 Topics. Sediments Vary Greatly in Appearance. Sediments May Be Classified by Particle Size. Sediments May Be Classified by Source. Neritic Sediments Overlie Continental Margins. Pelagic Sediments Vary in Composition and Thickness. Calcareous Ooze. Biogenic . calcareous ooze composed . of precipitated CaCO. 3. (usually calcite, but occasionally aragonite) shells of microscopic plankton . Planktonic foraminifera. Coccolithophore. 1. . Continental . Shelf. – 0-200 meters deep. . Contains 8% of the oceans surface area. Biologically richest part of the ocean. Contain . submarine canyons. – canyons eroded by glaciers which channel sediments to the ocean floor. Atmosph = 760 mmHg. Deep into sea, at every 33 feet pressure rises by 1 atmosphere . Vol. of air compressed & pressure increased along with depth. Deep sea diver – breath high pressure air. PATHOPHYSIOLOGY. the East Sea (Sea of Japan) . Kuh Kim. 1. , Kyung-Il Chang. 1. , Yun-Bae Kim. 2. . Jae-Hak Lee. 3. , Sang-Chul Hwang. 3. . 1. Seoul National University. 2. Pohang University of Science and Technology.