| Transliterated Name | Source | Name |
|---|---|---|
| Tyre | Arabic | صور |
| Tyrus | Latin | |
| Tyros | Greek | Τύρος |
| Sur | Phoenician | |
| Ṣurru | Akkadian | |
| Tzór | Hebrew | צוֹר |
Fig. 2
Fig. 14
Fig. 17
Fig. 2
Fig. 14
Fig. 1
Fig. 6
Fig. 1
Fig. 6
Fig. 3
Fig. 4
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 16
Marriner et al (2005) undertook a litho and biostratigraphical study of four core sequences from the landward edge of the current harbor. AMS radiocarbon dating was performed on dateable material found in the cores. The cores appeared to capture harbor sediments and showed a clear break in sedimentaion at the end of the Byzantine era noting the following :
4.6. Unit A - Exposed beach environment (post-Byzantine)Core profiles were presented and tsunamites were not found in the parts of the cores dated to the 6th - 10th centuries CE but a loss of harbor maintenance (e.g. continuous dredging operations) was evident.
The transition to unit A is dated to between the 6th to 10th centuries AD. The unit comprises a grey, shelly sand unit with textures of between: 3% to 31% for the gravels, 58% to 83% for the sands and 9% to 18% for the silts and clays.
Cerithium vulgatum and Pirenella conica dominatethe macrofauna suite, with numerous secondary species from diverse biocenoses (Ringicula auriculata, Nassarius pygmaeus, Gibberula miliaria ), consequence of an environmental opening. The increase in coastal ostracod taxa such as Urocythereis sp. and Aurila woodwardii, is to the detriment of the formerly abundant lagoonal taxa of unit B. This translates a re-exposure of the environment to the influence of the marine swell and currents. For the foraminifera, the dominant taxa are Ammonia convexa, Peneroplis planatus and Cellanthus craticulatum. The tests of many of these individuals have been broken by waveaction, confirming a rise in energy dynamics, due to the collapse of harbour maintenance. This is linked to the demise of Tyre as a Mediterranean commercial centre.
In Tyre, port opening may have been amplified by approx. 3 m collapse of the island after the 6th century AD (Marriner et al. 2005). Its northern Persian (?) mole is currently 2.5 m below present sea level (Descamps, pers. commun.), translating a subsidence of approx. 3-3.5 m. On the southern shore, drowned quarries at -2.5 m below MSL have also been discovered, and similar subsidence is translated in the city's coastal chronostratigraphy.
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Somewhere between Acre and Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description |
|---|---|---|---|
|
Tyre |
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Somewhere between Acre and Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
| Effect | Location | Image(s) | Description | Intensity |
|---|---|---|---|---|
|
Tyre |
|
|
Fleming, W. B. (1915). The History of Tyre, New York: AMS Press.
– open access at archive.org
Gatier, P. L., et al. (2011). Mission archéologique de Tyr:
Rapport préliminaire 2008–2009, BAAL 14: 103–129.
Katzenstein, H. J. (1973). The History of Tyre: From the
Beginning of the Second Millennium BCE until the Fall of
the Neo-Babylonian Empire in 538 BCE, Jerusalem.
Marriner, N., et al. (2005). Geoarchaeology of Tyre’s
Ancient Northern Harbour, Phoenicia, Journal of
Archaeological Science 32: 1302–1327.
Bikai, P. M. (1978). The Pottery of Tyre, Warminster.
Archaeological report on the principal excavation
examining the pre-Hellenistic city.
Chehab, M. (1983–1986). Fouilles de Tyr: Ija
Nécropole, Bulletin du Musée de Beyrouth
33–36, Paris. Final excavation reports on the
Roman and Byzantine cemeteries.
Jidejian, N. (1969). Tyre Through the Ages,
Beirut. Especially valuable for the Persian
and Hellenistic periods, with extensive
photographic documentation.
Joukowsky, M. S., ed. (1992). The Heritage
of Tyre: Essays on the History,
Archaeology, and Preservation of Tyre,
Dubuque, Iowa.
Katzenstein, H. J. (1973). The History of
Tyre: From the Beginning of the Second
Millennium BCE until the Fall of the
Neo-Babylonian Empire in 538 BCE,
Jerusalem.
Katzenstein, H. J., and Edwards, D. (1992).
Tyre. In The Anchor Bible Dictionary,
vol. 6, pp. 686–692, New York.
Sader, H. (1991). Phoenician Stelae from
Tyre, Berytus Archaeological Studies
39: 101–126.
Sader, H. (1992). Phoenician Stelae from
Tyre (continued), Studi Epigrafici e
Linguistici 9: 53–79.
Seeden, H. (1991). A tophet in Tyre?,
Berytus Archaeological Studies
39: 39–82.
