Tuesday, March 4, 2014

Transects--Viewing the complexity of ancient cultures at a continental scale

https://rowman.com/ISBN/9781498514279/Impact-of-Tectonic-Activity-on-Ancient-Civilizations-Recurrent-Shakeups-Tenacity-Resilience-and-Change

This posting has been revised and incorporated in a published book as of August 2015 (link above)


Transects: Viewing the comparative complexity of ancient cultures at a continental scale

Eric R. Force (eforce@email.arizona.edu)

Previous postings of this weblog, and related publications (see references) have described the remarkably active tectonic environments of ancient civilizations, and quantified the apparent spatial relationship.  An additional way to verify the significance of this relation between ancient civilizations and active tectonic boundaries is to back away, to view it as if from afar, comparing the complexity of cultures in tectonically quiescent cratonic interiors with those we have described on tectonically active plate margins (1).  This could be done along “transects” ideally crossing plate margins at right angles for particular times in antiquity, as a way of dealing with the huge number of cultures that have come and gone in the entire eastern hemisphere.  Figure 1 quantifies the results in terms of the listed criteria of Childe (1950) for civilization normalized to plate-boundary location.  An extended discussion of the validity of these criteria is below in a note (2).
My introduction in this weblog to the quandary posed by the spatial distribution of civilizations (3) is itself a transect of sorts across the southern margin of the Eurasian plate, from Greece to Etruria to southern Gaul in about 600-300 B.C.  It was noted that cultural accomplishment varied with tectonic activity; both accomplishment and tectonism were great in Greece, both more moderate in Etruria, both very modest in pre-Roman Gaul (4).  As a transect this assemblage is somewhat compromised, as it crosses tectonic boundaries in a composite way and is discontinuous.  It of course was only meant to provoke thought, but we can keep it in mind as better sample transects come along.  It is linked with one of these in figure 1.
Good transect possibilities are actually hard to find.  Many are inherently one-sided due to intervening seaways or nearly-impassible deserts or mountain ranges.  The looped shape of plate boundaries make some of them impractical to cross with straight lines (fig. 2).  So, a few of those I’ll describe start in a quiescent cratonic interior and approach an active margin, but end when we get there, i.e. they are one-sided transects. 

A western Asia transect.—One exception to these difficulties would extend from modern Jordan through northern Mesopotamia into the land between the Black and Caspian seas and on to the Caucasus Mountains.  If we look in on the area in the interval 900-700 B.C. we find the SW end inhabited by Aramean-speaking nomads.  The country is dry, of course, but not so useless that Nabatean farmers and builders could not inhabit it some centuries later.  Far to the west were principalities of Moab and Edom, but another plate boundary lies just beyond them.
At the Euphrates plain we abruptly enter the Assyrian  civilization and empire, which seemingly could have written Childe’s criteria as self-description.   This culture and its capitals Ninevah and Assur are well-described as exceedingly complex (5) .  The convergent boundary between the Arabian and Eurasian plates is only about 120 km to the northeast.  It is somewhat distributed, with different motion types on different faults (6). 
Across this zone was the Urartu kingdom, centered around Lake Van.  These people, successors to Bronze-age Hurrians and ancestors to Armenians, were renowned for their metal (especially bronze) work, complex dams and canals, temples, fortresses, and inscribed stele, and they left behind epigraphy suggesting  a national consciousness.  They had their own religion, and their language, though commonly written in Assyrian, is still poorly understood.
Past Urartu toward the Caucasus Mountains were nomadic Cimmerians, and at times the Scythians, for which there will be more description later.  Portable art, trade, and occasional concerted effort of these cultures seem the only assets that Childe would appreciate (7).  Figure 1 shows this transect in terms of Childe’s criteria for the cultures described.  Note that he greatest cultural complexities plot nearest the plate boundary. 
The result of this transect would have been roughly the same if our path had crossed the Tigris-Euphrates valley anywhere along its length.  What if the time period had been different?  If we adopt the same path and look at the late Bronze-Age cultures along it, in Jordan there would have been nomads; in place of Iron-age Assyrians we would have a so-called Old Assyria, the northern half of the previous Akkadian empire of Mesopotamia (but lacking the famous art and architecture of its descendent); in place of Urartu we would have the Hurrian-Mittani culture, famous for its ceramics, metallurgy, music, religion, and thriving cities; and the nomads to the north were not yet as accomplished as the Scythians would be.  Figure 1 shows (dotted) that we have replicated the same curve as for the later period but at a lower level and with narrower distribution. 

South and central Asia.—Another nearly-symmetrical transect begins in peninsular India, crosses the Ganges plain, then the Himalayas onto the Tibetan plateau and into central Asia.  Let’s look at this for about A.D. 400-600 when complex cultures are most evident and numerous for this region (8).
The south end begins in ancient Kalinga, roughly the Bihar of today, then under the thumb of the rulers of the Ganges plain to the north.  It contained rich cities along the coast carrying on a flourishing trade with Burma (and already boasting some notable temples) but very few sizeable settlements to the south and west.  The culture was based on tribal feudalism, though Kalingans had previously united sufficiently to battle invaders from the Ganges.  Kalingans had their own Dravidian script.  The religion was mostly Jain, already ancient, though the area has a rich history of religious transitions involving Hinduism and Buddhism.
Northward into the Ganges plain we enter at this period the Guptan empire and its culture.  It was one of the world’s greatest, already showing all the essential characteristics we associate with Indian culture as still revered by countless devotees the world over (9).  North of the Ganges plain only 150 km we pass across the plate boundary into the Himalayas, and we’ll have to excuse areas at very high elevations for a lack of great civilizations, but remarkably soon we pass into a part of the Tibetan plateau where an empire was emerging.   Many palace-fortresses that subsequently became monastic cities included barley-granaries, military armories, and factories for trade goods (10).  Chinese records show the militaristic nature of this culture, later minimized as Buddhism took over its records. 
Moving north again onto the northern Tibetan plateau we would encounter only Altaic-speaking nomadic cultures that seem embodiments of a contrast with Childe’s criteria.  Still farther north come the Hsiung-Nu nomads against whom China built its great wall.  Figure 1 thus shows a definite relation between cultural complexity and distance from tectonic plate boundaries. 

Southeastern Europe.—A one-sided transect could go from Greece northward into eastern Europe.  Ancient Greek civilization (11) must be what Childe had in mind when he proposed his criteria, and as we’ve seen, several of its originating sites are practically on major tectonic boundaries.  Several time periods including the Mycenaean era would be suitable for our transect, but if we choose that for 600-300 B.C., classical Greek civilization is at its height.  Its northern margin is with a tribal mostly-agricultural culture called the Thracians by Herodotus, a major source of information about them.  In the later part of our time interval it was united into a so-called Odrysian kingdom that was in the process of becoming Hellenized, speaking Greek in court, etc. and styling its capital village of Seuthopolis a city.    Then at about the Danube River the dominant culture becomes that of the Scythians, a semi-nomadic tribal culture about which Herodotus was particularly intrigued.  Their portable arts, especially in gold and mostly preserved in their burial mounds, are widely admired. Their language and religion are vaguely Iranic, and reportedly their economy benefitted from trade in slaves they captured in raids.  The Scythians were the end point of our south and central Asia transect also; as a loose confederation they occupied an enormous area of central Asia. 
This transect, along with the composite transect of my introduction (12),  pivots at ancient Greece as a common point and using the same time interval.  As with the other two transects (of figure 1), cultural complexity falls off markedly away from tectonic plate boundaries.  And clearly, the same transect taken in the late Bronze Age would have the same general character, with lower Childe-scores and with narrower geographic spread (13).

Two African half-transects.—Transects of ancient cultures do not have to run through great civilizations; they just have to present contrasts in both cultural complexity and tectonic environments.  In Africa, two possible transects are limited by seaways and deserts to being one-sided, but are nevertheless illustrative. 
First, if we start anywhere on the Punic coast of present-day Tunisia and venture southward, it is over 400 kilometers before we reach country too dry for settlement, partly because of the coastal embayment of the Gulf of Gabes.  The boundary between the African and Eurasian plates swings gently in the other direction, however, giving a range of distance from plate boundaries from about 100 km for ancient Carthage, Utica, etc. to 500 km at the south end of the Gulf where Phoenicians never settled but nomads roamed until late in Carthage’s history (14).  Thus any such transect taken from at least 1000 B.C. to about 200 B.C. would show cultural complexity approaching the Childe maximum at the end nearest the plate boundary to the Childe minimum at the other end.
Transects that cross the Nile where it traverses desert landscapes would show complex cultures only along the river.  But farther south, the ancient kingdom of Axum (Aksum) was adjacent to the Afar triangle, where the African-Arabian plate boundary is in the adjacent narrows of the Red Sea and where the East African Rift begins. The highlands at this latitude are vegetated across Ethiopia to the Sudan.  By A.D. 200 and for about 500 years thereafter, Axum might be considered a great ancient civilization (15) if we knew enough about it .  But to the west were like Neolithic tribes, except for Egyptian refugees that formed a kingdom of Meroe on the river—which Axum eventually conquered.  Again, an exceedingly complex culture about 200 km from a plate boundary contrasts with a comparatively simple one at about 900 km. 
These two half-transects each consist of only two points, and are hardly worth plotting as their geometries seem obvious.  Added to figure 1, they would support the array showing maxima of cultural complexity along active tectonic boundaries. 

Other possible transects.—These five transects present a remarkably orderly variation of cultural complexity with tectonic position in antiquity (fig. 1).  The reader is bound to wonder how the outcome was determined by my positioning of transects.  For all of them, the path could be varied significantly without changing the overall result—indeed in most cases the peaks at tectonic boundaries would be sharper, with fewer shoulder-cultures.  And choosing an earlier time interval in antiquity would generally sharpen the peaks also, as there would be fewer outlying complex cultures, whereas predecessors of the most accomplished civilization would already be complex.
Many transect possibilities are ruled out by the distribution of major seaways and deserts.  One additional one in south Asia could be added for the specific period of the Indus-Saraswati civilization, extending from peninsular India across the Indus into the mountains of Baluchistan.   This would be analogous to the south Asian transect already plotted (fig. 1) and would resemble it closely.
Ancient Egypt shows no convincing association of ancient civilizations with tectonism; a transect passing through Egypt would show its mode at least 300 km from a plate boundary.  In SE Asia, civilizations that would score high marks on Childe’s scale had not yet arrived in antiquity as treated here, but by about A.D. 900 they had, and Pagan and Borobodur would plot on the boundary between the Eurasian and Indo-Australian plate, but the Khmer empire would not, making this hypothetical plot bimodal.  No transect has been shown through ancient China because of the semantic ambiguity of plate boundaries nearby (16). But these are the only complex considerations I’m aware of; all the ten-pointers derived from Childe’s list in the eastern hemisphere of antiquity have been considered and plotted in figure 2. 

Conclusions.—The transects show that criteria for cultural complexity as listed by Childe (1950) and repeated in modified form by many subsequent authors tends to show a maximum along active tectonic boundaries in antiquity.  This of course is consistent with figure 2, which shows the originating sites of “great ancient civilizations” arrayed along tectonic plate boundaries almost like beads on a string.  But the transect approach not only verifies this distribution, it also gives us the beginnings of a converse case—a “what’s wrong with other places and other cultures” approach, one that will be extensively explored in another post.  It looks like other cultures that occupied the broad quiescent margins of tectonic boundaries were there all along but did not become as accomplished, at least as scored by Childe’s criteria.
The presence and shape of shoulders adjacent to peaks near tectonic boundaries on figure 1 is intriguing.  They give the curves a continent-scale dimension and also suggest that tectonic boundaries have some primary influence--if their influence were secondary to some “real” controlling factor there would be reversals.  The width of the shoulders is greater than expected seismic impact, suggesting possible spread effects.
The transects also give us some very strong clues to the meaning of the distribution.  For the Childe criteria are all cultural criteria, and figure 1 thus suggests that tectonism has an impact on cultural development per se.  We’ve seen some examples of close culture-tectonism relations in descriptions of individual ancient civilizations (18).  Of course tectonic impacts could be indirect, and we’ll look into several possible indirect linkages (19).  Many important variables such as spring distribution that influence cultures are far more fine-grained than either figures 1 or 2 can show. The possibility of multiple factors is also consistent with our data so far--as long as a cultural factor is included.  Indeed we’ll focus on water supply as one such factor in a future blog-post (20).  But as we’ll see, there are a number of seemingly-possible explanations that are inconsistent with the transect data (21).  In the meantime, we have several indications including this very powerful transect information that cultural development in antiquity was somehow related to active tectonism. 
            Despite my participation in several publications on tectonic environments of ancient complex cultures (see references), these transect data are still unpublished.  I will look for opportunities to remedy that situation. 





Notes
1. This approach first suggested to me by the late John Dohrenwend.  I have used conventional descriptive surveys (Barraclough 1978, Wood 1985, Starr 1991; Scarre and Fagan 2007, supplemented where necessary for obscure cultures by internet encyclopedias) for my brief descriptions except where noted. 
2. Feb. 14, 2012
3. The criteria for great ancient civilizations listed by Childe (1950) are 1 cities, 2 occupational specialties, 3 concentrated food surpluses, 4 monumental public architecture, 5 capabilities for planning and organization, 6 record-keeping and writing, 7 practical science, 8 arts, 9 trade, and 10 some sort of ideological solidarity.  This list has been much modified and re-interpreted (perhaps most recently by Scarre and Fagan 2007) but basically accepted by authorities that put any stock in the term ancient civilization. Some anthropologists do not, for reasons discussed on August 20.  For example, historian Fernandez-Armesto (2001) says “all such lists are bunk,” and this would be so from his point of view--that cultural complexity should be judged on the transformation of the environment a culture inherits (an extremely valuable point of view but one that I would not associate with the term civilization, which derives from the concept of city).   It appears to me that anthropologic interest in cultures has shifted away from their “greatness” to individual interesting features.
Given the conventional view of “great ancient civilizations” that was already extant in Childe’s day, I think his list is a rather common-sense way to describe the components of the concept.  Certainly Childe’s list is useful for my question, i.e. that the apparent spatial correspondence of active tectonic boundaries with conventionally defined great ancient civilizations needs quantification where possible.  Such criteria have been used quantitatively by bona fide anthropologists (cf. Morris 2010). I think it would be scientifically irresponsible not to try out a relation between Childe’s list and tectonic position.  Don’t you?
It would be possible for someone better versed than me in the ancient cultures involved to assign partial scores for each Childe-item.  I have not attempted to do this, simply adding whole integers for the cultural attributes for which I have found documentation. 
4. See Woolf (2000).  A more generous treatment is given by Tacitus, who may himself have been from the region of southern Gaul. 
5. May 8, 2014
6.  See for example McClusky 2000
7.  Concerted effort was tribe-by-tribe, so I did not give the Scythians #5.
8. This transect too would illustrate the same general conclusion at any period of antiquity after about 1100 B.C., and any plate-boundary intersection in the entire Ganges drainage would serve.
9. May 8, 2014
10. Perhaps best described by Fernandez-Armesto 2001.
11. June 27, 2014
12. Feb. 14, 2012
13. The transect that pivots at Greece would in the Bronze Age still have to pivot somewhere in that peninsula, Crete, or the southern Aegean.
14. Markoe 2000
15. Fernandez-Armesto 2001.
16. May 8, 2014
17. Feb. 1, 2014
18. June 27, 2014, June 16, 2014, and May 8, 2014
19. July 17, 2013
20. June 3, 2013
21. Aug. 29 and May 10, 2013

References

Barraclough, G., 1978, The Times atlas of world history:  Times Books, London

Childe, V. G., 1950, The urban revolution: The town planning review, v. 21, p. 3-17

Fernandez-Armesto, F., 2001, Civilizations—culture, ambition, and the transformation of nature:  Free Press, New York

Force, E. R. 2008, Tectonic environments of ancient civilizations in the eastern hemisphere:  Geoarchaeology v. 23 p. 644-653.

Force, E. R., and McFadgen, B. G., 2010, Tectonic environments of ancient civilizations: opportunities for archaeoseismological and anthropological studies, in Ancient Earthquakes, M. Sintubin, I. S. Stewart, T. M. Niemi, and E. Altunel, eds.:  Geological Society of America Special Paper 471, p. 21-28.

-----, 2012, Influences of active tectonism on human development—a review and Neolithic example, in Climates, Landscapes, and Civilizations, L. Giosan, D. Q. Fuller, K. Nicoll, R. K. Flad, and P. D. Clift, eds:  American Geophysical Union Monograph 198, p. 195-202

Markoe, G. E., 2000, Phoenicians: University of California Press

McClusky, S. and others, 2000, Global positioning system constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus: Journal of Geophysical Research v. 105 B3, 5695-5719.
Morris, I., 2010, Why the west rules—for now:  Ferrar, Strauss, and Giroux, New York.

Scarre, C. and Fagan, B. M., 2007, Ancient civilizations (3rd ed.): Longman, New York.

Starr, C. G., 1991, A history of the ancient world: Oxford University Press

Wood, M., 1985, The world atlas of archaeology: Portland House, New York

Woolf, G., 2000, Becoming Roman—the origins of provincial civilization in Gaul:  Cambridge








Figure 1. Two examples of continental-scale transects across some plate-tectonic boundaries showing cultural complexity in antiquity as quantified in terms listed by Childe (1950).  Superposed transects are normalized to approximate locations of plate boundaries; measurement relative to tectonic boundary is to originating site of each culture where known.  Solid line is for western Asia in the 900-700 B.C. time period; dotted line is the same transect in the late Bronze Age.  Lettered localities for that transect are A Ninevah, B Urartu, and C Cimmerians and Scythians.  The dashed transect is south Asia in the AD 400-600 period, with D Kalinga, E Patna area of Guptan empire, and F the Brahmaputra-Llasa valley of Tibet. 






Figure 2.--Locations of originating sites of 13 prominent ancient civilizations relative to various aspects of the southern boundary of the Eurasian plate (after Force, 2008; Force and McFadgen 2010). Civilizations (and sites) shown are 1—Roman (Rome), 2—Etruscan (Tarquinii-Veii), 3—Greek (Corinth) and Mycenaean (Mycenae), 4—Minoan (Knossos-Phaestos), 5 and 6—West Asian (Tyre and Jerusalem), 7—Assyrian (Ninevah), 8—Mesopotamian (Ur-Uruk), 9—Persian (Susa-Pasargadae), 10—Indus (Mohenjodaro), 11—Aryan India (Hastinapura), 12—Egyptian (Memphis), and 13—Chinese (Zhengzhou).