Chalcolithic

The Chalcolithic period, also known as the Copper Age, is the transition phase between the Stone Age (Neolithic) and the Bronze Age, lasting roughly from 5000 to 3000 BC depending on the region. [1]

Meaning and Etymology

The word comes from the Greek words chalkos ("copper") and lithos ("stone").
It signifies the time when humans first began using pure, unalloyed copper alongside traditional stone tools. [1, 2, 3]

Key Characteristics

Metalworking: Humans learned to cold-work and later smelt copper to make simple axes, chisels, and ornaments, though stone tools remained common. [1]
Economy: Communities relied on advanced farming, livestock rearing, and a wide variety of cultivated crops. [1, 2]
Trade: Long-distance trade networks expanded to exchange raw copper, flint, pottery, and precious items. [1, 2]
Culture and Pottery: Distinctive painted pottery traditions emerged, such as fine black-and-red ware. [1, 2]
Social Change: Villages grew larger, some featured early fortifications, and burial practices with grave goods hint at early social differentiation. [1]

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Early Mesopotamia

The Uruk period (c. 4000 to 3100 BC) existed from the protohistoric Chalcolithic to the early Bronze Age period in the history of Mesopotamia, following the Ubaid period.^[3] Named after the Sumerian city of Uruk, this period saw the emergence of urban life in Mesopotamia. It was followed by the Sumerian civilization in southern Mesopotamia.^[4] The late Uruk period (3400 to 3200 BC) saw the gradual emergence of cuneiform script and corresponds to the early Bronze Age

Levantine Chalcolithic

Periodisation

The Chalcolithic period is divided into three primary stages, called the Early Chalcolithic, Middle Chalcolithic and Late Chalcolithic, each identified with a different material culture. The chronology of the period was refined by the Israeli prehistorian Yosef Garfinkel.^[7]

Early Chalcolithic (5,800–5,300 BC)

The identification of the Early Chalcolithic emerged alongside the first excavations at Jericho (1935–1936), where John Garstang initially classified Layer VIII for a time as Chalcolithic.^[8] Subsequent definitions were refined based on ceramic assemblages, especially those from Wadi Rabah and Munhata Layer 2b, excavated by J. Kaplan and J. Perrot.^[9] At Munhata, a large exposure (47,320 sherds) revealed a standardized repertoire of 21 pottery types, dominated by carinated bowls, holemouth jars with square rims, pithoi with thumb-ledge handles, and bow-rim jars. Decoration was mainly by red or black slip, often burnished (86.4%), with a smaller component of surface manipulation (13.5%); handles were rare and applied rope decoration absent.^[10] Comparable assemblages were identified at Jericho (Layer VIII and PNB), Wadi Rabah, Teluliyot Batash III, ‘Ein el-Jarba, and Nahal Bezet, while most forms show clear parallels in Halafian sites such as Tel Halaf, Shams ed-Din, and Tell Turlu.^[11]

Lithic industries also shift dramatically: the small Neolithic arrowheads disappear from Mediterranean-climatic zones, persisting only in desert areas, while new sickle blades and adzes become common. At Nahal Zehora I, only the transversal arrowhead remains, bifacial axes decline to about 3%, and adzes increase significantly.^[12] Obsidian artifacts appear widely and indicate a peak in long-distance exchange networks.^[13][14] In contrast, figurative art declines sharply compared to Yarmukian culture; the few anthropomorphic figurines are schematic and emphasize female sexual features. New elements, such as elongated slingstones, also emerge and have parallels in Halafian assemblages.^[15] Evidence from sites like Hagoshrim further points to strong northern connections, including abundant obsidian and stamped seals.^[16][17]

The Early Chalcolithic represents a rapid and far-reaching transformation in the material culture of the south- and central- Levant. The ceramic repertoire is largely new and closely tied to Halafian traditions of northern Syria, suggesting processes of cultural transmission rather than local development. This phase is also marked by a high degree of regional homogeneity, observable across former Yarmukian and Jericho IX zones as well as in the broader Levant, including the Beq'a,^[18] Byblos (“néolithique moyen”),^[19][20] and the ‘Amuq Phase C.