Image | Description | Source |
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![]() ![]() Age model computed for the trench stratigraphy using OxCal v4.2 (Bronk-Ramsey et al. 2010) and IntCal13 calibration curve (Reimer et al. 2013). Light grey indicates raw calibration and dark grey indicates modelled ages including stratigraphic information. Phases indicate subsets of samples where no stratigraphic order is imposed. Klinger et al (2015) |
Age Model | Klinger et al (2015) |
![]() ![]() Age model computed for the trench stratigraphy using OxCal v4.2 (Bronk-Ramsey et al. 2010) and IntCal13 calibration curve (Reimer et al. 2013). Light grey indicates raw calibration and dark grey indicates modelled ages including stratigraphic information. Phases indicate subsets of samples where no stratigraphic order is imposed. Klinger et al (2015) |
Age Model - big | Klinger et al (2015) |
![]() ![]() Trench log of the southern wall. The full resolution photomosaic of the wall is available in Fig. S1. The different stratigraphic units are indicated by letters A to H located in the synthetic stratigraphic section. Conservative position of event horizons are indicated with a dashed line, including for event Esuppl unambiguously visible in the eastern fault zone only. E8 is indicated for reference, although the dashed line corresponds to E7 event horizon (see discussion in text). Esupp2, between E8 and E9 is not indicated. Meter Marks (MM) are indicated above the trench. Dated 14C samples are indicated by star. To the west, a few samples have been collected up to 2 m outside the gridded wall, where the layers could be traced horizontally. Samples are indicated at the corresponding depth and stratigraphic position. Klinger et al (2015) |
Trench Log | Klinger et al (2015) |
![]() ![]() Some of the earthquakes identified at our trench site have produced major deformation, while others are only responsible for small vertical offsets and cracks. The later are assumed to stop/start in the Yotvata jog and the large one to break through it. The trench suggests that the fault alternates between periods with more numerous smaller events and periods with large less frequent events. Potentially 2 cycles could be observed in this trench. Uv strands for vertical deformation. Chronological indications are located at corresponding stratigraphic level. Klinger et al (2015) |
Simplified Trench Log | Klinger et al (2015) |