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'Ubeidiya Formation site II-23, Northern District (HaZafon District), Israel
Lat/Long (Decimal) | 32.6833,35.5667 |
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Co-ordinates Derivation | based on nearby landmark |
Mindat.org Region (for given coordinates) | Northern District (HaZafon District), Israel |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
---|---|---|---|---|---|
'Ubeidiya Formation site II-23 | Gaudzinski S. (2004) | 'Ubeidiya | Site has been subject to much tectonic movement - archaeological levels are almost vertical in the section. There have been four major depositional cycles, the lowest is of archaeological interest and is termed the Fi (lower Fluviatile). This limnic level is 30m thick. Site dated to between 1.4-1.0Ma, but is thought (on faunal grounds) to be at the older end of this range. | claystone | 2.588 - 0.0117 Ma Pleistocene |
'Ubeidiya Formation, site I-15LF/I16 | Gaudzinski S. (2004) | 'Ubeidiya | Site has been subject to much tectonic movement - archaeological levels are almost vertical in the section. There have been four major depositional cycles, the lowest is of archaeological interest and is termed the Fi (lower Fluviatile). This limnic level is 30m thick. Formation dated to between 1.4-1.0Ma, but is thought (on faunal grounds) to be at the older end of this range. | conglomerate | 2.588 - 0.0117 Ma Pleistocene |
Oubeidiyeh, general area | Faure M. (1986) | Ubeidiya | Site has been subject to much tectonic movement - archaeological levels are almost vertical in the section. There have been four major depositional cycles, the lowest is of archaeological interest and is termed the Fi (lower Fluviatile). This limnic level is 30m thick. Formation dated to between 1.4-1.0Ma, but is thought (on faunal grounds) to be at the older end of this range. | conglomerate | 2.588 - 0.0117 Ma Pleistocene |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!