Publication Date

12-12-2014

Degree Level

B.A.

Program

History

First Advisor

Root, Bradley

Second Advisor

Cardenas, Richard

Document Type

Thesis

Medium

manuscript

LCSH subject

Rome—History—Empire, 30 B.C.-476 A.D; Rome—Environmental conditions; Climatic changes—History; Agriculture and state—Rome

Abstract

Although historians have debated the various causes of the fall of the Roman Empire for centuries, scholars did not consider the impact of environmental change until the early twentieth century. Initially, environmental historians believed that agricultural decline resultant from soil erosion and deforestation played a dominant role; however, scientific and historical evidence can now be utilized to demonstrate that these two factors were much less prevalent during the third through fifth centuries than they had been during the prosperous Pax Romana. In contrast, recent climatological studies, most notably dendrochronological sequences, have established that a combination of cooling and desertification plagued Eurasia during the late Roman Empire. Moreover, the examination of a wide variety of literary sources, historical writings, and archaeological findings related to flooding of the Tiber and Nile Rivers substantiates the climate change theory. Thus, a steady decrease in temperature and precipitation during the third and fourth centuries triggered a severe drought that devastated Roman agriculture and contributed significantly to the collapse of the Roman Empire by inciting demographic decline, economic retrogression, and political upheaval, as well as by prompting the westward migrations of the Germanic and Hunnic peoples into Roman territory.

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