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The soils of Galilee change from calcareous rock in the coastal plain, to Cenomanian and Turonian limestone (deposited from about 99 to 89 million years ago) in Upper Galilee, and to Eocene formations (those dating from about 55 to 35 million years ago) in the lower part of the region.Rock salt and gypsum are abundant in the Great Rift Valley.A sandy shoreline with many beaches borders the Mediterranean coast.Inland to the east, fertile farmland is giving way to growing agricultural settlements and the cities of Tel Aviv and Haifa and their suburbs. These mountains terminate to the east in an escarpment overlooking the Great Rift Valley.The coastal plain is covered mainly by alluvial soils.Parts of the arid northern Negev, where soil development would not be expected, have windblown loess soils because of proximity to the coastal plain.

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