PPT-Illustrated Ocean Zonation

Author : pasty-toler | Published Date : 2016-08-14

Poster Zones Include Epipelagic sunlight Mesopelagic twilight Bathypelagic Midnight Abyssalpelagic the Abyss Hadalpelagic trenches Continental Shelf Continental

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Illustrated Ocean Zonation: Transcript


Poster Zones Include Epipelagic sunlight Mesopelagic twilight Bathypelagic Midnight Abyssalpelagic the Abyss Hadalpelagic trenches Continental Shelf Continental Rise Continental Slope. Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP While written to incorporate computer technology the lesson can be easily adapted to paper and pen Lesson Objective Students will compose a series of slides based on the exhibits at OC The teacher may select one type of exhibit such as those that co Vocabulary. Ocean Current. Coriolis Effect. Rip Current. Upwelling. Major Ocean Currents. An . Ocean Current. is a large volume of water flowing in a certain direction.. Wind-driven currents are called surface currents.. Unit C:. Inserting Objects into a Presentation. Objectives. Insert text from Microsoft Word. Insert clip art. Insert and style a picture. Insert a text box. Microsoft Office 2010-Illustrated. Objectives. By: Ray Bradbury . Author Highlights. Ray Bradbury was born in Waukegan, Illinois on August 22, 1920. Bradbury's reputation as a leading science fiction writer occurred in 1950 with . The Martian Chronicles. C-BIG - Conservation . Biology Informatics Group. Dept. of Biosciences, University of Helsinki. http://cbig.it.helsinki.fi. Zonation in practice: tutorial and GUI. Simplified . Zonation. workflow. 1. How do different currents form. What is upwelling. What do ocean currents transfer. Predict. T F. Ocean currents are always cold. C. ontinents affect the direction of currents. Currents only flow near the surface of the ocean. Warm Up & Spiral . November 4. How are surface currents created?. How are deep ocean currents created? . What are 2 factors that affect the density of water?. What is upwelling? . Objectioves. : 8.E.1.1/1.2. From 100-200 m (600 ft) to the deepest part. Mesopelagic (to depth of 3300 ft -1000 m). Twilight. THE DEEP - Bathypelagic, Abyssopelagic & Hadopelagic. No sunlight at all. THE MESOPELAGIC. From 100-200 m to depth of 3300 ft (1000 m). 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: . Ocean Decade Research . Programme. on the Maritime Acoustic Environment (UN-MAE). Modeling and Prediction of Ocean Ambient Sound. . A Satellite activity of UN Ocean Decade Laboratories: A Prediction Ocean . The illustrated guide to a Ph.D.. Professor . Matt Might. , CS, University of Utah. has a good way of explaining what it means. to do a Ph.D.. It is also applicable to doing MS research. and probably your life after graduation. For much of human history, knowledge of the ocean and its currents was not recorded for many reasons - most sailors could not write and information was passed orally.. European nations began systematic ocean explorations but kept information secret between the 15. The Vast World . Ocean. Area of Continents and Oceans. Seventy one percent (71%) of the globe is covered with oceans or seas.. Continents and islands compose the remaining twenty nine percent (29 %)..

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