Transliterated Name | Source | Name |
---|---|---|
Tulul Abu al-'Alayiq | Arabic | |
Tel Abu Alak | Arabic |
Netzer (1975:89) reports that the earliest remains of the Hellensitic-Roman periods
at Tel Abu Alaik are pre-Herodian
and
probably Hasmonean
.
Netzer (1975:92) also reports that, as of 1975, no evidence had been found to establish
a building date for the winter palace at the site but finds of pottery and coins indicate that it was used at least by the
last Hasmonean
Kings, as well as by Herod in the early years of his reign.
The town of Jericho is situated on the wide plain of the Jordan Valley, about 10 km ( 6 mi.) north of the Dead Sea and close to the steep cliffs that fringe the valley to the west(map reference 193.142). At a depth of 250 m below sea level, it is the lowest town on the surface of the earth. This location, shut in by mountain walls to the east and west, has a climate that is tropical in summer and usually mild in winter. The amount of rainfall is small, about 140 mm a year, most of which falls in a few violent downpours - in some years there is virtually none. The flourishing agriculture of which the area is capable is dependent on the spring known as Elisha's Well, or 'Ein es-Sultan. With irrigation based on the spring, the valley's alluvial soil can produce crops of almost every kind, tropical and temperate in habitat - dates, green vegetables, or wheat. In times of expansion, the waters of 'Ein es-Sultan can be supplemented by those of'Ein ed-Duk (Na'aran), some 3 km (2 mi.) to the northwest, which, as in the Early Arab period and today, can be brought to Jericho by aqueduct. With irrigation, an extensive oasis can be created; but when it is neglected, the area reverts to the parched scrub of the adjacent valley, as is seen in nineteenth-century photographs taken in the immediate neighborhood of 'Ein es-Sultan. Destruction of the irrigation system by enemies, or the interruption of the water supply as a result of the earth movements to which the Jordan Valley is liable, may account for the periodic abandonments of the ancient site that excavation has revealed.
Historians of the Hellenistic-Roman period (Strabo, Pliny, and Josephus) stress Jericho's economic and military importance. In the tropical climate prevailing in the vale, the groves of Jericho produced high-quality dates and various medicinal plants and spices, particularly balsam, which thrives on intensive irrigation. Because of these products, famed throughout antiquity, Josephus considered the valley a veritable paradise (War IV, 469).
In 1838, the site was first discovered by E. Robinson, at the debouchment of Wadi Qelt from the hills. In 1868, C. Warren conducted excavations at the two mounds of'Alayiq (map reference 191.139) as part of his examination of nine mounds in the Jericho area. He cut large trenches (3m deep) in an east-west direction and ascribed his finds to the Roman period. On mound 1, south of Wadi Qelt, many glass fragments and a Roman amphora with a seal impression on its handle were found; and on mound 2, north of the wadi, walls of sun-dried brick, some of them decorated with painted plaster, were exposed.
Excavations were carried out from 1973 by a Hebrew University expedition headed by E. Netzer, with the assistance of the Israel Exploration Society and the staff officer for archaeology in Judea and Samaria. The excavations were conducted annually from 1973 to 1983 and in 1986-1987. Mounds 1 and 2 were reexamined and large areas to the west and east of mound 2 and to the north of mound 1 were cleared; these were the most extensive excavations ever conducted at the site. In addition, the extensive system of aqueducts west and north of the site (originally surveyed by the British Palestine Exploration Fund) was resurveyed and investigated; numerous agricultural installations were discovered in the vicinity of this water-supply system
Several short excavation seasons were conducted in 1998–2000 at the Second Temple period winter palaces in the area of Tulul Abu el-‘Alayiq in Jericho. The excavations were conducted by an expedition of the Hebrew University of Jerusalem under the direction of E. Netzer, with the assistance of Y. Kalman and R. Laureys-Chachy. The work concentrated upon the area east of the twin palaces, the area northeast of Herod’s second palace, and the workshop area.
King Herod received a Hasmonean Winter Palace at Jericho which may have been destroyed by the
31 BCE Josephus Quake.
Herod subsequently rebuilt a palace at a different but nearby location on top of a damaged synagogue.
Roller (1998) notes that the original Hasmonean palace remained in use until the
30's BCE "as the drowning of Aristobulus in 36 BCE demonstrates"
(see Antiquities of the Jews Book XV Chapter 3 Paragraph 3). This would indicate that
Ambraseys (2009) was mistaken in his assertion that it is more probable
that the structure was destroyed by war when Herod conquered Jericho in 39 BCE taking it from
Antigonus II Mattathias -
the last Hasmonean King of Judea.
Karcz et al (1977) reports that a strong earthquake in 31 BCE destroyed the palace
.
Effect | Location | Image(s) | Description |
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