Fig. 1.28| Transliterated Name | Language | Name |
|---|---|---|
| Tall Zira'a | Arabic | تالل زيرا'ا |
Tall Zirā‘a, located in the middle of the Wādī al-‘Arab and ~4.5 km. SW of Ancient Gadara, was continuously occupied for at least 5,000 years (Vieweger and Haser, 2017).
Figure 0.3
Figure 1.32
Figure 2.111
Figure 1.32
Figure 2.111
Figure 4.4
Figure 4.4
Figure 4.5
Figure 4.5
Figure 4.6
Figure 4.6
Tab. 4.1
19 Rothe and others 2017, 268–70; Häser 2024, 351–52.
20 Häser 2024, 73–83 and 136–38.
21 Soennecken and Leiverkus 2021, 11, 112, site 211/225-16.
Figure 1.32
Fig. 1.68
| Effect | Location | Image(s) | Comments |
|---|---|---|---|
| Landslide | western area of the settlement
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
a landslide destroyed the western area of the settlement- Vieweger and Häser (2017:11) |
|
| Cave collapse | beneath the settlement layers
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
Calcareous sinter caves beneath the settlement layers collapsed- Vieweger and Häser (2017:11) |
| Effect | Location | Image(s) | Comments |
|---|---|---|---|
| Collapsed Walls ? | Monastery consisting of a church and living quarters in Areas I and II
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
Although the walls do not show any clear indication of an earthquake, it is highly probable that the destruction of the monastery was caused by the quake in 749. Afterwards, the site was abandoned almost entirely as only few sherds of Abbasid date and the absence of buildings, which can be attributed to this period, indicate- Haser (2025:127) |
Earthquake Archeological Effects (EAE)| Effect | Location | Image(s) | Comments | Intensity |
|---|---|---|---|---|
| Landslide | western area of the settlement
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
a landslide destroyed the western area of the settlement- Vieweger and Häser (2017:11) |
IV+ | |
| Cave collapse | beneath the settlement layers
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
Calcareous sinter caves beneath the settlement layers collapsed- Vieweger and Häser (2017:11) |
III+ |
Earthquake Archeological Effects (EAE)| Effect | Location | Image(s) | Comments | Intensity |
|---|---|---|---|---|
| Collapsed Walls ? | Monastery consisting of a church and living quarters in Areas I and II
Figure 1.32General Plan of the excavation area on Tall Zira'a (Source: BAI/GPIA) Vieweger and Häser (2017) |
Although the walls do not show any clear indication of an earthquake, it is highly probable that the destruction of the monastery was caused by the quake in 749. Afterwards, the site was abandoned almost entirely as only few sherds of Abbasid date and the absence of buildings, which can be attributed to this period, indicate- Haser (2025:127) |
VIII+? |
Tall Zira'a The Gadara Region Project (2001-2011) Volume 1, Introduction
Tall Zira'a The Gadara Region Project (2001-2011) Volume 2, Early and Middle Bronze Age
Tall Zira'a The Gadara Region Project (2001-2011) Volume 6, Hellenistic to Umayyad Period (Strata 8-3)
Final publication of the excavations and surveys between 2001 and 2011