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A synthetic, concluding discussion addressing the relationship between Ur-Aeolic and Special Mycenean and providing a historical framework for, especially, the introduction of Aeolic language and culture (pre-Thessalian/Boeotian) into European Greece following the Bronze-Age collapses and for the spread of pre-Aeolians (Iron-Age Ahhiyawans) eastward into Cilicia.
The Macedonia Alexander left in spring 334 BCE was principally the making of his father Philip II, though Philip’s ‘Macedonia proper’ had been largely a recovery of the Argead realm of Alexander I more than a century earlier. Early expansion from Pieria into the central plain of Bottiaea established a core of Argead control in Lower Macedonia. Following the retreat of Xerxes’ army after 479, Alexander I took full advantage of a power void to expand into the eastern region, conquering eastern Mygdonia, annexing Crestonia and Bisaltia eastwards to the Strymon valley and gaining control of rich supplies of mineral deposits and timber. Most of the eastern territory was lost after 450 BCE, but Philip II, in addition to recovering the old kingdom and consolidating Upper with Lower Macedonia, through conquest and diplomacy more than doubled the politically controlled territory of Macedonia. His transformation of Macedonia included the subjugation of Paeonians, Illyrians, Thracians and Triballians, the opening up of trade and securing of mining, control of Epirus, domination of Thessaly and the uniting of the southern Greek poleis under his hegemony. Alexander inherited a stable kingdom, a tested army of Macedonians, subordinate allies and a secure supply line to Asia.
This chapter studies the consequences of the conquest of Epirus and the supposed destruction and enslavement of 70 cities and 150,000 persons by the Romans, as well as the region’s revitalization under Augustus.
Illyris, Macedonia and Epirus have much more in common with one another than with the Greek peninsula. Their climate on the whole is continental, whereas that of the Greek peninsula is Mediterranean, and their livelihood has depended until very recently on pastoralism and stock-raising rather than on arboriculture, agriculture and maritime trade. Yet their coastal areas approximate to the Mediterranean climate. The olive, for instance, flourishes at Valona and Preveza and in Chalcidice, but it is not found inland of Elbasan, Paramythia and parts of the coastal plain of Macedonia. In peninsular Greece the first two centuries of the Iron Age were impoverished in contrast with the preceding period. The Phrygian period in west Macedonia lasted for some three and a half centuries, and the entry into Thrace and later into Asia Minor was made from a basis of strength.
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