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As we can see from this quotation from this page about Classics Research at Cornell University
"It is a common mistake to think that classics is just about the ancient languages -- it is not," said Manning, whose position includes an affiliation with the Department of Earth and Atmospheric Sciences (EAS). "I use interdisciplinary approaches that bring environmental, climatic, material culture, geo-archaeological and anthropological evidence together to study past climate, environmental changes, landscapes, societies and people."
| A History of Climate A brief introduction to the history of climate |
| NOAA If you have paleoclimatology questions to be answered |
| What is theHolocene? a useful explanation from Berkeley |
The Holocene is the name given to the last ~10,000 years of the Earth's history -- the time since the end of the last major glacial epoch, or "ice age." Since then, there have been small-scale climate shifts -- notably the "Little Ice Age" between about 1200 and 1700 A.D. -- but in general, the Holocene has been a relatively warm period in between ice ages.
| 'Climate Research University of East Anglia' |
| High-Resolution Climate Variability of the Holocene |
| Colorado Geophysics provides many scientific enquiry methods |
| Quaternary climate change,here |
Also try this site for many of these subjects Kevin Greene Online Companion 'Dating the past'
TopIn 535AD, nature literally came to standstill. Winter gripped the earth for two years Startling new evidence shows that trees all over the world - from Ireland to Siberia, California to Finland - stopped growing during the mid-sixth century. Eyewitness accounts describe what we might now call a 'nuclear winter.' According to the Syrian Bishop, John of Ephesus"The sun became dark ...Each day it shone for about four hours, and still this light was only a feeble shadow"from Wikipedia 'Climate Changes of 535-536'
Prof.Mike Baillie is Professor of Palaeoecology at Queens University,Belfast
'Irish crannogs (wooden forts built over water) are archaeological evidence to support Keys’ and Baillie’s theory of a severely cold period in the sixth century. In fact, much of the wood that Baillie dated came from crannogs in which people sought refuge during times of trouble and clan warfare. The mid-sixth century marks the beginning of the construction of crannogs. Baillie sees a strong connection between the need for such forts and the deteriorating climate.' an excellent page with mapshttp://www.ees1.lanl.gov/Wohletz/Krakatau.htm Was it caused by a Volcano eg KrakatoaSuburban Emergency Management Project in the U.S.A
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