Hemiobol

発行体 Orchomenos of Boeotia
年号 425 BC - 364 BC
種類 Standard circulation coin
額面 Hemiobol (1⁄12)
通貨 Drachm
材質 Silver
重量 0.38 g
直径 7.0 mm
厚さ
形状 Round (irregular)
製造技法 Hammered
向き
彫刻師
流通終了年
参考文献 BCD Boiotia#209b
表面の説明 Half wheat grain, with sprouting end facing upward
表面の文字体系
表面の銘文
裏面の説明 Wheat ear upwards
裏面の文字体系 Greek
裏面の銘文
鋳造所
鋳造数 ND (425 BC - 364 BC) - -
Numisquare ID 5676569430
追加情報

Historical Context: This silver Hemiobol, issued by Orchomenos in Boeotia between 425 BC and 364 BC, reflects a period of significant political flux. Orchomenos, a prominent city-state, navigated the turbulent Peloponnesian War and the subsequent rise of Theban hegemony. Issuance of such small denominations underscores the city's need for a functional internal economy, facilitating daily commerce amidst shifting alliances and conflicts with its powerful Boeotian neighbor, Thebes. This coin testifies to Orchomenos's persistent autonomy during the Classical era.

Artistry: While no specific engraver is attributed, this minute Hemiobol exhibits characteristics of Classical Greek numismatic tradition, filtered through a distinctive Boeotian regional style. Typically, the obverse features a simplified Boeotian shield, rendered with its characteristic central indentation. The reverse often displays a single grain ear, symbolizing the fertile Copais basin. The design, though compact, aims for clarity and immediate recognition, reflecting the practical demands of a fractional currency. Execution maintains a robust, abstract representation of its civic emblems.

Technical/Grading: Weighing a mere 0.38 grams and measuring 7.0 millimeters, this Hemiobol represents a significant minting challenge. The small flan size often results in incomplete strikes, with design portions frequently off-center or weakly impressed. High-points for wear or strike quality typically include the raised boss of the Boeotian shield or the individual kernels of the grain ear. Collectors should anticipate variations in strike sharpness and centering. Silver purity is generally high, but surface preservation, given its diminutive nature and extensive circulation, can vary considerably.

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