ABSTRACT: This lecture focuses mainly upon this author's excavations, findings, and analysis of a late Old Kingdom fort at Ras Budran in el-Markha Plain, South Sinai, and the broader context of both its time period and East Mediterranean...
moreABSTRACT: This lecture focuses mainly upon this author's excavations, findings, and analysis of a late Old Kingdom fort at Ras Budran in el-Markha Plain, South Sinai, and the broader context of both its time period and East Mediterranean in general. In essence, the time period (Dynasty 6), need, and placement of the fort seem to suggest a felt need for such added security in South Sinai (where no earlier fort/forts have been found --yet). After covering the findings from the fort, the lecture proceeds with a broader discussion. In the context of 2,300-2,200 BCE, climatic change (namely increasing aridity and a few major droughts) plays a definite role in the "collapse" (decline) of Egypt’s Old Kingdom ca. 2,200 BC, while several other factors also played a significant part (albeit much debated regarding their exact role in relation to climate). Increasing aridity toward end of Old Kingdom translated into droughts, which in-turn created famines and led to internal & external instability. At the time of the late Old Kingdom, Egypt’s neighbouring city-states in Palestine (Early Bronze Age III) shifted into a mostly de-urbanized landscape (Early Bronze Age IV: ca.2300-2000 BCE): i.e., reflecting strife. During the same EB IV period, Syrian city-states become much more impoverished, but fared better than de-urbanized Palestinian to South. Egyptian accounts from Dyn.6 report Bedouin massacres of Egyptian expeditions to the Red Sea and in northern Nubia, alongside accounts of military expeditions into Palestine and allusions to forts (or fort-building) along the eastern frontier. Later (propagandistic) Egyptian accounts hearken back to Asiatic Bedouin incursions into the East Delta, and general unrest in peripheral regions (drought?). Evidence for dramatic rise in Bedouin seasonal campsites in EB IV northern Sinai Peninsula: i.e., potential enemies on Egypt’s E. frontier. Evidence for late OK destruction and mass burials at major East Delta city (Mendes), which may suggest civil strife, incursions, or other things. Evidence for the establishment of late Old Kingdom fort(s) in South Sinai, which may suggest a new circumstance where earlier forts are unknown (as of yet). Other evidence, however, suggests that the E. Desert and Sinai Bedu were always somewhat hostile and a threat, such as Egypt’s felt need to have troop escorts here, build fortified camps, and subdue Bedouin tribes. The situation in Dyn.6 (early EB IV) seems to have been a dramatic intensification of former conditions: i.e., Bedu hostility and conflict over marginal resources (i.e., Egyptian exploitation of local wells, game, etc.). Despite all these factors, which are related to climatic factors, Egypt also displays non-climatic factors that had been building in Old Kingdom and also contributed to its “collapse”: i.e., a “last straw” scenario? The lecture continues with a discussion of various factors leading up to the decline/collapse of the Old Kingdom in Dynasty 6. A series of summary text slides are placed at the end of the lecture to provide a quick reference and narrative to the main points. UPDATED: 3 April, 2023. Adding in selected sources, and some minor edits and formatting.