The basins constituted an immense natural reservoir that could hold water in reserve for six to eight weeks. In this sense, Egyptís irrigation system was more a means of redistributing and rationing floodwaters (Brewer & Teeter 1999:25). Water was then allowed to flow from one basin to another following the slope of the land, while artificial channels carried water to the farthest area if the flood was low (Silverman 1998:60)... displayed 300 characters
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Water was then allowed to flow from one basin to another following the slope of the land, while artificial channels carried water to the farthest area if the flood was low (Silverman 1998:60). Moreover, Caminos (1997:8) describes how sluices and canals regulated the course and volume of the flow In addition, Quirke & Spencer (1992:16) explain how over the millennia, canals and dykes would have slowly modified local agriculture in two other respects: by increasing the cultivable area and by fostering second or third crops within a year in small select plots... displayed next 300 characters
Foreland basins varies greatly, therefore the exact type of foreland basin that describes the southern Basin the most cannot be decided.
A sedimentary basin can be defined as an area where there is a physiographic low or depression in which there is the potential for accretion of sediments transported from a distant source in largely passive margin environment...
After reaching the surface it can be eroded by the earth's weather patterns and become sedimentary rock. Sedimentary and igneous rock can then become metamorphic when they are pressed into the earth's crust and heated to a melting point ? one sedimentary or igneous rock melts it is magma? then magma can become igneous rock? if any rock melts it will become magma? melting is not required or possible to form metamorphic rock...
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