Chronometry

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Chronometry and chronology

I use the term “chronometry” to refer to the stratigraphic dimension, i. e., to the clustering of elements according to their contact association. It is a purely inner-referential process, in the sense that only the elements found in contact in any given excavation unit are taken into consideration.

The term “chronology,” on the other hand, refers to the integrative dimension, whereby elements from other units and especially from the wider context of Syro-Mesopotmian history are brought to bear on the analysis of the data.

time measurement	clustering	analysis
chronometry	strata	stratigraphic
chronology	horizons and phases	integrative

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A conflict

Chronometry and chronology are obviously closely interconnected, but there are two conflicting principles of operation:

1. on the one hand, one wants to retain full adherence to the principle that contact associations are the fundamental point of reference for all stratigraphic considerations – and contact associations can be described only at the level of the most elemental unit of excavation, to be identified as strata; accordingly, strata change frequently in the measure in which the excavation itself proceeds.
2. on the other hand, one wants to relate these to the wider chronological frame that matches the full historical dimension of the site and of the region, i.e., phases and horizons. Phases and even more horizons entail greater permanence.

A resolution of this conflict lies in allowing for multiple sequences to exist at the same time, with an indexing system that maintains the distinction while making it possible to establish overarching connections. Accordingly, I use

• the term sequence for the ordering of strata, and
• the term frame for the ordering of horizons and phases;
• in each case a suffix will provide an indexing factor to distinguish among the intervening steps.

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Sequences

A sequence reflects our understanding of the depositional process at any given moment, and in any given excavation unit, in the process of excavations. The logic of the system requires that strata be sequenced independently in each operation, since properly stratigraphic considerations can only apply to contiguous excavations.

The sequence may change dramatically even between areas that are very proximate to each other, and may change within the same operation from year to year. Thus, it is indispensable to register the differences, and to keep the correlation among them perfectly clear we use an indexing system.

Sequences may belong to either

• a single excavation unit, e. g., s120^J3B (stratum 120 in Unit J3, sequence J3b) or
• a broader area, e. g., s122^AAB (stratum 122 in Area AA, sequence AAB).

A sequence by area becomes possible as individual units come either in physical contact with each other, or are sufficiently close to allow a logical extrapolation.

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Frames

In the 2008 season at Mozan we introduced for the first time a sitewide “sequence” which is however guided by very different principles than the proper sequence as defined above. It serves in fact as a broad frame of reference which is informed by data relating not only to the site as a whole, but even more prominently to data extraneous to the site.The MZ frame reflects the accepted understanding of the broad historical setting of Syro-Mesopotamia, and the strata and phases identified in the various sequences are linked to these particular developmental stages.

In 2011, the Mozan frame was fully formalized by Federico Buccellati and was labeled as MZA.

Within it, actual phases and strata are identified and defined, even though they may differ in terms of the depositional process involved within any given Unit. In other words, while the same numbers are used to allow for a correlation across chronological lines, this should not be taken to imply that the depositional processes embodied in the different sequences are the same.

As a result, while the numbers for phases and especially strata may be the same, the definitions for phases and strata will generally differ from area to area, and even from unit to unit. In practice, this means that we retain distinct unit and area sequences (e.g., A1A, AAC, …), but assign numbers within the range of the MZ frame (currently MZA).

An example: phases 53^MZA through 55^MZA are richly represented in area AA (where they were labeled as 5a^AAG through 5c^AAG); they are, however, missing in area JP. Using the MZA sequence simply means that there will be a gap in the numerical sequence of the JP phases: this will call attention to a depositional phenomenon that requires a particular explanation.

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Indexing

In the UGR system, strata and phases (but not horizons) are indexed, meaning that each is given a distinct sequential number as part of an element label (e.g., s12 for stratum 12, h6 for phase 6). The elements from each applicable sequence are listed in the constituent section of the analytical portion of the Urkesh Global Record, UGR (right-hand side, in black), under “strata” and “phases.”

Suffixes identify sub-strata and sub-phases (s12a, h6a).

Distinct sequences and frames are identified in labeling by a suffix appended to either the stratum or the phase. The suffix may be expressed

• either by a superscript, e. g., s120^J3B, h6a^MZA,
• or by a hyphen followed by the identifier, e. g., s120-J3B, h6a-MZA.

To this end a second suffix (preceded by a hyphen, -) is added to each stratum and phase, indicating the sequence to which it belongs – e.g., s12a-AAC refers to stratum 12, substratum a, in sequence C pertaining to area AA.

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Archival versions

The different phase/strata generations that were in use for different units and different areas prior to any given date are archived for permanent future reference, even though only the latest one is in use in any given version of the Urkesh Global Record (UGR). Thus, for area AA (and various units within it) we reached generation G, and for area JP (and various units within it) we reached generation C. For ease of correlation, all previous sequences are accessible from the MZ sitewide book (under “Stratigraphy”, on the left-hand side).

Some of these sequences have been published in printed reports [add links, ZGy27 mDP].