Fill (archaeology)
In archaeology fills are contexts representing material that has accumalated or been deposited into a cut feature such as ditch or pit of some kind. Fills a important part of the archaeological record as there formation and composition can throw light on many aspects of archaeological study.
Primary fills
Primary fill like so many other other terms in archaeology can have several different but allied meanings. Used singularly it denotes the context that first appears in the sequence after the context representing the cut. In many cases this will be a silt or naturally accumulating material that forms in the bas of some hole or trench before its function is realized. For example a medieval rubbish pit which may be open for some time before rubbish is placed in it allowing natural processes to silt up the base. but the interpretation may mark the end of a cut feature's use. For example a ditch that silts up by neglect, could represent the start of the end of the features function in the record. secondary and subsequent fills all form above the primary fill. Primary Fills used in the plural tends to denote all the fills with in a feature that are sealed by layer(s) possibly representing a change in phase or function.
Slumping
Slumping is a process that can occur to any context in the record and not just fills and represents how a context's deposition morphology may deform from its original position by natural settling action. This relates to fills which have a tendency to settle radically over time. and in turn have a bearing on the excavation of cut features. As fills slump the overlying layers which seal the feature will slump in sympathy creating false impressions of fills below the lip of the cut and introduce the possibility of contaminated dating evidence into the features excavation. (See archaeological section in fig 1). also the degree of slumping of the primary fills compared to the slumping of overlying sealing layers is a possible measure of time differences
Tip lines
Tip lines are an intrinsic characteristic of fills but it is a term that can apply to many other types of context such as dumps. Tip lines are the angles which the contexts form as indicator of action in the past. As fills of a feature form stratigraphiaclly the direction off the horizontal by which they form may give us information. For example a ditch that has fills all angled so one side of each fill is higher on a specific side of the ditch could represent that the ditch was backfilled from the side where the fills were highest. (See archaeological section in fig 2). This can be circumstantial evidence for features or detail not preserved in the archaeological record. This reading of a fills deposition morphology is an example of why deposits and contexts are important discoveries in themselves independent of whether they represent structures or contain artifacts.
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