Abstract
The geological environment of the site is composed of mobile sand, kurkar, hamra and grumosols (swelling and cracking clay soils) sediments of the Quaternary Hefer formation.
Keywords
geology
Recommended Citation
Barzilay, Eldad
(2006)
"The Kurkar and Hamra Genesis of the Northern Hill of Tel Mikhal (Tel Michal) (pp. 127–130),"
'Atiqot: Vol. 52, Article 47.
DOI: https://doi.org/10.70967/2948-040X.2140
Available at:
https://publications.iaa.org.il/atiqot/vol52/iss1/47
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