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Research indicates that the earth’s surface is completely enclosed by the soil which comes from the original bedrock. This might include chalk, sand and granite, different types of rocks or clay (Barker). Since the fundamental nature of the soil is analyzed through its underlying rocks therefore initially the subsoil is studied then soil’s fertility is known which further helps in the determination of farming or vegetation settlements. Archeological sites are broadly defined as the settled residues of different structures which over the period of time convert into earthworks and rubble through the process of stone-rubbing, erosion, decay and invasion by the animals and plants (Barker).
Sometimes it is possible that the researchers locate a residual settlement which is on its way to become an archeological site. This basically facilitates scientists in studying the archeological process. The archeological sites are usually found at lowland areas (Barker). One of the important factors in locating an archeological site is the confirmation of the fact that rocks present at the upper layer of earth were formed later than those beneath them. For instance, lave forms after the development of mountainside rocks. However, surface of the earth never remains in the same pattern and hence after some time the covering of different structural settlements remove and the rock beneath them comes to the surface. The same thing happens with the archeological sites since when the superimposed layers are removed the underlying surface becomes visible which indicates the historical remains and the presence of previous living and nonliving objects (Barker).
Archaeological remains are distinguished into different types. The first archeological type deals with the antiquity of man i.e. the recognition of former civilizations, for instance, those humans who lived in caves centuries ago. There are various written records which
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