Archaeological sites form through processes that are both natural and human-related. In most cases, they form when cultural remnants have been buried by sediments deposited by either alluvial (water-related) or eolian[?] (wind-related) natural processes, although colluviation[?] - the burial of a site by sediments moved by gravity - and human activities (both deliberate and incidental) also often bury sites. The sediment in which a site is buried is termed the matrix.
Generally, evidence of human activity is not considered an archaeological site unless it exceeds fifty years in age and yields more than a small number of artifacts or features.
Famous archaeological sites:
Search Encyclopedia
|
Featured Article
|