'Late paleozoic' diaporamas de présentation

Late Paleozoic Earth History

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Plate Tectonics and Continental Drift

Plate Tectonics and Continental Drift. Tectonics. Tectonic Forces are forces generated from within Earth causing rock to become ___________ . 1. The study of the origin and arrangement of Earth surface including mountain belts, continents, and earthquake belts. deformed. Tectonics.

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Topic #5 Causes of Ice Ages/Glaciation I) Ice Age vs Glaciation -Periods of global glaciation

Topic #5 Causes of Ice Ages/Glaciation I) Ice Age vs Glaciation -Periods of global glaciation -Geographic extent of global glaciation II) Terrestrial Causes of Ice Age/Glaciation Volcanism -particle size of ash plume -height of ash plume -water vapor and high acidity gases

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Chapter 15

Chapter 15. The Late Paleozoic World. Guiding Questions. How did marine life of late Paleozoic time differ from that of middle Paleozoic time? How did terrestrial floras change on a global scale in late Paleozoic time? What changes occurred in terrestrial faunas during late Paleozoic time?

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History of Extinctions

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Prentice Hall EARTH SCIENCE

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Prentice Hall EARTH SCIENCE

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Prentice Hall EARTH SCIENCE

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Prentice Hall EARTH SCIENCE

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HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I.

HISTORICAL GEOLOGY LECTURE 10. LATE PALEOZOIC GEOLOGY I. The Late Paleozoic (Devonian-Mississippian-Pennsylvanian-Permian) is noted for a number of geologically significant events:. - widespread COLONIZATION of the land by large plants, reptiles and amphibians.

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http://vishnu.glg.nau.edu/rcb/globaltext.html

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Late Paleozoic

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