Read e-book online The GALE Encyclopedia of Science PDF

By K. Lee Lerner, Brenda Wilmoth Lerner

ISBN-10: 0787675547

ISBN-13: 9780787675547

ISBN-10: 0787675555

ISBN-13: 9780787675554

ISBN-10: 0787675563

ISBN-13: 9780787675561

ISBN-10: 0787675571

ISBN-13: 9780787675578

ISBN-10: 0787675598

ISBN-13: 9780787675592

ISBN-10: 0787675601

ISBN-13: 9780787675608

Comprises greater than 2,000 entries starting from brief definitions to significant overviews of techniques in all parts of technology.

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Conceptual Physics. Englewood Cliffs, NJ: Prentice Hall, 2001. G. Kraige. Engineering Mechanics, Dynamics. 5th ed. New York: John Wiley & Sons, 2002. Methods of Motion: An Introduction to Mechanics. Washington, DC: National Science Teachers Association, 1992. Serway, Raymond, Jerry S. Faughn, and Clement J. Moses. College Physics. 6th ed. Pacific Grove, CA: Brooks/Cole, 2002. Kenneth L. Frazier Accelerators The term accelerators most commonly refers to particle accelerators, devices for increasing the velocity of subatomic particles such as protons, electrons, and positrons.

Stahl Professor Emeritus Department of Physics California State University, Los Angeles Los Angeles, California Robert L. Stearns Department of Physics Vassar College Poughkeepsie, New York Ilana Steinhorn Science Writer Boalsburg, Pennsylvania David Stone Conservation Advisory Services Gai Soleil Chemin Des Clyettes Le Muids, Switzerland Eric R. Swanson Associate Professor Department of Earth and Physical Sciences University of Texas San Antonio, Texas Cheryl Taylor Science Educator Kailua, Hawaii Nicholas C.

Science. 5542 (October 19, 2001): 503. Larry Gilman Abyssal plain Abyssal plains are the vast, flat, sediment-covered areas of the deep ocean floor. They are the flattest, most featureless areas on the Earth, and have a slope of less than one foot of elevation difference for each thousand feet of distance. The lack of features is due to a thick blanket of sediment that covers most of the surface. These flat abyssal plains occur at depths of over 6,500 ft (1,980 m) below sea level. They are underlain by the oceanic crust, which is predominantly basalt—a dark, fine-grained volcanic rock.

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The GALE Encyclopedia of Science by K. Lee Lerner, Brenda Wilmoth Lerner


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