1. References

The geology of Palestine includes deep Arabian Shield metamorphic rocks, overlain by sandstone, dolostone, limestone, gypsum and clays from the Paleozoic, Mesozoic and Cenozoic.

Research published in 2012 confirmed the existence of Pleistocene loess in the Wadi Gaza, which has a large watershed covering the Northern Negev Desert, the Hebron Mountains and the Gaza Strip—where it discharges into the Mediterranean Sea. The study identified three Kurkar ridges in the Gaza Strip running northeast-southwest: Skeikh Ejilin Ridge, Al Montar Ridge and Bait Hanon Ridge. During the winter, the wadi feeds up to 20 million cubic meters of rainwater into the area.^[1]

References

• Max-Planck-Institute for Molecular Biomedicine
• Max Planck Institute for Molecular Biomedicine
• Max Planck Institute for molecular cell biology and genetics
• Max Planck Institute for Molecular Genetics
• Max Planck Institute for Neurobiology
• Max Planck Institute for Nuclear Physics
• Max Planck Institute for Plant Breeding Research
• Max Planck Institute for Polymer Research
• Max planck institute for psycholinguistics
• Max Planck Institute for Psycholinguistics
• Max Planck Institute for Radio Astronomy
• Max Planck Institute for Research into Economic Systems
• Max Planck Institute for Research on Collective Goods
• Max Planck Institute for Social Anthropology
• Max Planck Institute for Software Systems
• Max Planck Institute for Solar System Research
• Max Planck Institute for Solid State Research
• Max Planck Institute for Terrestrial Microbiology
• Max Planck Institute for the Science of Human History
• Max Planck Institute for the Science of Light
• Max Planck Institute for the Study of Religious and Ethnic Diversity
• Max Planck Institute of Biophysics
• Max Planck Institute of Colloids and Interfaces
• Max Planck Institute of Experimental Endocrinology
• Max Planck Institute of Immunobiology and Epigenetics