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670 pages, Hardcover
Published October 15, 2019
Two circumstances, one exceedingly remote and the other [the aftermath of Rome’s fall] far less so, were critical for European fragmentation and polycentrism. From the late Cretaceous onward, the collision between the African and Eurasian tectonic plates caused the Alpine orogeny, a process that formed the Carpathians and Alps and raised them ever higher. Without the former, Transylvania would not have appeared and the great Eurasian steppe would extend to Vienna; and without the Alps, it might stretch even farther west…