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Climate history

environmental_impacts

Subject: 
Environmental Science
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Climatology
Physical geography
Climate forcing agents
Climate change
Climate history
Climate forcing
Panspermia
Svante Arrhenius
Greenhouse effect
Global warming
Greenhouse gas
University of Hong Kong

The University of Hong Kong - Faculty of Engineering L4: Environmental Impacts Faculty of Engineering CCST9016 Energy: Its Evolution and Environmental Impacts Dr. Match Wai Lun Ko Department of Mechanical Engineering The University of Hong Kong [email protected] 1 The University of Hong Kong - Faculty of Engineering ? Climate change: The whole world has been threatened under the influence of global warming (CO2 effect). PART A. Global Environment Impact From: http://scienceblogs.com/framing-science/2006/12/melting_metaphors_new_study_on.php 2 The University of Hong Kong - Faculty of Engineering An Early Warning ? The idea that increased levels of carbon dioxide in the air could cause the earth to warm is not new. ? Theory was suggested in 1895 by a Swedish

Geological Time Scale

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Environmental Science
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Historical geology
Phanerozoic
Geologic time scale
Glaciology
Cenozoic
Ice ages
Climate history
Quaternary
Pleistocene
Epoch
Pliocene
Quaternary glaciation
Environment
Tags: 
Geologic time scale
Phanerozoic
Historical geology
Planetary science
Climate history
Extinction events
Geological history of Earth
Cenozoic
Cretaceous
Permian
Pleistocene
Mesozoic
Environment
geology time scale geologic eon epoch

Eon Era Period Epoch Major Events Phanerozoic Cenozoic Quaternary (0-1.6 million yrs BP) Holocene (Present-10,000 yrs) Modern humans develop. Pleistocene Ice Age Interglacial. Pleistocene (10,000 -1,600,000 yrs) Pleistocene Ice Age. Extinction of many species of large mammals and birds. Tertiary Pliocene (1.6-5.3 million yrs) Development of hominid bipedalism. Cascade Mountains began forming. Climate cooling. Miocene (5.3-24 million yrs) Chimpanzee and hominid lines evolve. Extensive glaciation in Southern Hemisphere. Climate cooling. Oligocene (24-37 million yrs) Browsing mammals and many types of modern plants evolve. Creation of the Alps and Himalaya mountain chains. Volcanoes form in Rocky Mountains. Eocene

Chapter 1 Notes

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US History
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Geology
Historical geology
Physical geography
Glaciology
Geology of Minnesota
Supercontinents
Climate history
Ice ages
Canadian Shield
Bering Sea
Americas
Continent
Environment

Chapter 01 - New World Beginnings---33,000 B.C.-A.D. 1769. ?I. The Shaping of North America 1. 225 million yrs. ago supercontinent 2. Mountains-- Appalachians pre separation, all others after making them ?American? mountains. 3. Canadian Shield- NE corner of Americas, maybe first above sea level 4. Ice Age- 2 million yrs. ago--2 mile thick ice, Canada, N. America 5. Glacial action eroded Canadian Shield II. Peopling the Americas 1. The Land Bridge-- Sea level dropped because of glaciers exposing a land bridge. ? ? Bering Sea between Siberia and Alaska 2. Nomadic hunters following migratory game herds 3. Ice Age ended, glaciers melted, land bridge under water--10,000 yrs. ago 4. When Europeans arrived in 1492-- 54 million people lived in the Americas.
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