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calcareous soil

   Also found in: Wikipedia 0.02 sec.
calcareous soil (kălkâr`ēəs), soil formed largely by the weathering of calcareous rocks and fossil shell beds. Different varieties usually contain chalk, marl, and limestone and frequently a large amount of phosphates. They are often very fertile, as in the case of the buckshot soils of the S United States. Sometimes calcareous soils are flinty, thin, and dry. They often form a large part of the soil of deserts, which may prove very fertile when sufficient moisture for crops is applied.


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But, there isn’t much you can do to change a calcareous soil, Ferrie says.
Looking at the limestone and rocky, semi-barren hillsides of the canyons, you can understand why most of our full-sun natives and many drought-tolerant plants do well in the quick draining and calcareous soil prevalent in this area.
 
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