Page 35 - Life & Land Use on the Bahrain Islands (Curtis E Larsen)
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        of artesian springs are located. A measured area for this favorable land as derived
        from 1956 aerial photography is 85 km^, less than 14% the total available land.
        When viewed in terms of population density as calculated from the 1971 census, the
        average density is 408 people/km^, but this becomes 2941 people/km when only
        the arable land is considered. The Manama-Muharraq urban center alone shows
        27,060 people/km^ by comparison. Thus, even though land area is physically

        limited, it is used in a still more restricted manner by the present population.
                Traditional farming has relied upon the natural availability of artesian
        water from the Eocene age aquifers to supply various gravity flow irrigation
        systems. However, natural springs occur only in the northern portion of the island.
        Modern well-drilling has provided farmers with methods for locating wells near
        arable land, and gasoline-powered pumps have aided in the extraction of water, but
        the best water is also restricted to the northern quarter of Bahrain.
                Usable soils are important factors. For agricultural use in an arid region,
        soils should not only provide necessary nutrients, but should also be able to offer
        adequate drainage. Inadequate drainage properties can lead to an increase in soil
        salinity, a potential check on plant viability. Bahrain’s best potential soils are
        found along the coastal plain surrounding the flanks of the geologic dome. These
        are derived from coastal deposits left by past incursions of higher sea level during
        the Pleistocene, as well as from the weathering products of the local limestones
        and dolomites transported by intermittent flow in the various wadis,   Unlike
        freshwater sources, the soils extend around the periphery of the main island. In the
        central depression, physical and chemical weathering of surrounding rocks, as well
        as redeposition by wadi flows have combined to provide still other potentially
        arable soils. Yet, though this area of arable soils is great, it is unusable without
        irrigation. Therefore, even the use of the existing soils is confined to the areas of
        the greatest water.

                Bahrain, like the Arabian Peninsula, is located within the Saharo-Arabian
        arid zone that occupies North Africa, and parts of Iran, Pakistan, and India
        (Rumney 1968). Temperatures in Bahrain average 26.4°C during the year with the
        highest average monthly temperatures (32.3°, 33.9°, 34.1°C) during June, July, and
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