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East-West Orientation of Historical Empires 

Peter Turchin, Jonathan M. Adams, and Thomas D. Hall 

November 2004 

 

Does environment affect the ability of states to project power? If state expansion is more easily 
accomplished by staying within the same ecological zone, then state territories should be oriented 
in the east-west direction, mirroring the orientation of major ecological zones of the world. Our 
analysis of 62 largest empires in history supports this conjecture. 

 
 

In a chapter entitled “Spacious Skies and Tilted Axes” Jared Diamond (1997) argued that 

food production spreads more easily latitudinally (in the East-West direction) rather than 
longitudinally. A latitudinal shift is easier because similar climates and soil types tend to be 
arranged in east-west oriented bands. This geographic pattern is best illustrated by a map of the 
global distribution of biomes (Figure 1). A 

biome

 is a major type of ecological community such 

as the grassland, desert, or temperate seasonal forest (Ricklefs 2001).   
 
 

Although Diamond focused primarily on the spread of crop cultivars and domesticated 

animals, the same principle should influence the military/political, demographic, and cultural 
dynamics of societies. Consider the greatest empire ever (in terms of territorial extent), conquered 
by the Mongols under Chinggis Khan and his immediate successors. The core of the Mongolian 
Empire was the Great Eurasian Steppe that stretches for many thousands of kilometers from the 
Khingan Mountains in the east to the Carpathians in the west (McNeill 1964). The Mongols were 
steppe warriors, and they were able to rapidly extend their influence over this whole region 
(Barfield 1994). The regions inhabited by settled agriculturalists adjacent to the steppe were 
incorporated more slowly and to a lesser degree than the steppe. For example, the Russian 
principalities of the forest zone were not occupied by the steppe-dwellers, being instead subjected 
to tribute. As a result, the Mongolian Empire, with its core based on the steppe, was much wider 
in the latitudinal rather than longitudinal direction. The ease of conquest was not the only factor 
promoting the latitudinal spread of the great empires. Societies inhabiting similar ecological 
zones tend to be more similar to each other than societies located in very different zones. 
Techniques developed for integrating and controlling a certain type of society should, therefore, 
be easier to extend latitudinally. Note that this “ecologic factor” should be detectable only at large 
geographic scales—a small state, as long as it stays within the same biome, will find it equally 
easy (or equally hard) to expand in any direction, longitudinal or latitudinal. 
 
 

Territorial expansion by states is a complex macrosociological process, influenced by 

many factors other than the environment. Does the ecological factor have a detectable effect on 
the projection of military/political power, or is its influence lost in the “noise” of complex 
interactions? To answer this question, we compiled a list of all large historical empires with peak 
territories exceeding 1 Mm

2

 (= 1,000,000 km

2

), and measured the distances from their eastern to 

western extremes, as well as from the northern to southern extreme (Endnote 1). Our measure of 
the tendency to expand in the latitudinal direction is the log-transformed ratio of the east-west 
distance to north-south distance (Endnote 2) the “latitudinal index.”  
 
 

The frequency distribution of the latitudinal index in our sample of 62 historic empires is 

strongly skewed to the right (Figure 2), and the mean index is significantly greater than zero (

t

 = 

4.83, 

P

 < 0.001). The great majority of empires, nearly 80%, have a positive latitidinal index—

that is, they are wider in the east-west compared to the north-south direction. There are only three 
empires that have a strong north-south orientation, and these are the proverbial exceptions that 
prove the rule. The New Kingdom of Egypt had at its core the valley of a major river running 
south-north, the Nile. The Inca empire was located on the west coast of South America, where 

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ecological zones run longitudinally (see Figure 1) due to a major mountain chain, the Andes. 
Finally, the Khmer empire was located entirely within the wet tropical forest biome. Thus, even 
though these three cases do not conform to the rule of latitudinal spread, they obey the more 
general rule of “expansion within an ecological zone.”  
 
 

All of the largest empires (with territory over 10 Mm

2

) were oriented in the east-west 

direction. We have already discussed the case of the Mongol empire. The Islamic Caliphate is a 
variation on the same pattern, except that the “native biome” of the Arabs was the subtropical 
desert, rather than the temperate grassland/desert of the Mongols. The next largest state in history 
after the Mongols, the Russian empire (peak area of 22.8 Mm

2

 in 1895), originated in the 

transitional zone between the steppe and the forest (ecologists call such transitional zones 

ecotones

). Once the Muscovite state began expanding in the sixteenth century, it spread fastest 

precisely within the same ecotone—eastward along the boundary between the Eurasian steppe 
and northern taiga. Eastward expansion was extremely rapid, so that the Pacific was reached by 
the mid-seventeenth century. In contrast, the southern advance into the steppes and deserts of 
Central Asia took a much longer time, and they were conquered only by the late nineteenth 
century.  
 
 

Another example of the same dynamic is the early expansion of Rome. The territory of 

the Roman Empire in the first century B.C.E. coincides almost precisely with the 
woodland/shrubland biome (also known as the Mediterranean zone). Subsequent expansion took 
the Romans into the forests of northern Europe. However, severe reverses, such as the battle of 
Teutoburg Forest in 9 C.E., in which 20,000 legionnaires were obliterated by the tribal Germans 
(Wells 2003), persuaded the Romans to abandon plans of further conquest. The general rule, thus, 
seems to be that expansion is easiest and most lasting when occuring within the same ecological 
zone. Expansion into other biomes is possible, but more difficult, slow, and requires greater state 
resources. The case of China is probably the best illustration of this principle. The native biome 
of the Chinese is the temperate seasonal forest (Endnote 3), and this was precisely the area that 
was first unified by each of a long succession of Chinese empires. The strength of the Chinese 
state, however, allowed it to expand into alien biomes, and at their peaks the great Chinese 
empires intruded into the steppe (Inner Mongolia, Chinese Turkestan), the alpine biome (Tibet), 
and the tropical rain forest (Vietnam).  
 
 

Is the influence of ecology detectable in the shapes of modern states? At first glance, no. 

The average latitude index for the 29 modern states whose territory exceeds 1 Mm

2

 is positive, 

but not significantly different from 0. However, if we exclude South American countries, where 
biomes extend in the longitudinal direction, the statistical test indicates that the pattern is 
detectable even today (

t

 = 2.66, 

P

 = 0.014). The tendency to east-west orientation in modern 

countries, nevertheless, is much weaker than for historical empires. Partly this could be due to the 
effect of modern technology, but we suspect that it is also an artefact of the propensity of modern 
states to claim territory even if it is not used by their populations. A striking example of this 
tendency is Canada, whose population is squeezed into a narrow band running east-west along its 
southern border with the US, but which nevertheless claims extensive territories in the Arctic. 
Because of the addition of these lands, which are almost totally devoid of human occupation, the 
latitudinal index of Canada is slightly negative. Algeria and Lybia provide other examples of the 
same tendency—their populations are largely confined to the east-west band along the 
Mediterranean littoral, but their latitudinal indices are essentially zero, because they claim huge 
territories to the south, in the Saharan desert.  
 
 

In conclusion, our results indicate that the physical and biological environment has a 

detectable effect on the shapes of historic and modern states. It appears that projection of 

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military/political power is easier within the same ecological zone (biome). Our results should not 
be interpreted as a kind of “ecological determinism”—although ecology is important, its 
influence on state expansion patterns is transmitted by entirely social mechanisms. On the other 
hand, certain techniques and ideas from ecological sciences have proved to be fruitful in 
suggesting novel approaches to the study of social systems (Turchin and Hall 2003). Diamond’s 
original insight, which motivated our study, is one example; another is the recent demonstration 
that cultural variability exhibits a latitudinal gradient (Pagel and Mace 2004). Our results also 
have interesting implications for the study of historical dynamics (Turchin 2003). Researchers 
working within the world-system paradigm have noted that the rise and fall of populations, cities, 
and empires is characterized by a broad-scale synchronicity (Chase-Dunn and Hall 1997, Chase-
Dunn et al. 2000). For example, there is a substantial correlation between the dynamics of 
Western Europe and China. On the other hand, South Asian dynamics are completely 
uncorrelated with the rest of Eurasia. Our finding that the propagation of “signals” within 
military-political networks is facilitated in the latitudinal, but not longitudinal directions suggest 
one possible explanation for this macrohistoric pattern. 
 

Endnotes: 

Note 1. Our list of large historical states was based on the compilation by Taagepera (1978, 1978, 
1979, 1997), which has been systematized and posted on the web by Chase-Dunn and coworkers 
(http://www.irows.ucr.edu/). We checked the Taagepera list with all major historical atlases in the 
library of the University of Connecticut and found additional eight empires that fitted our criteria 
(Axum, Hsi-Hsia, Kara-Khitai, Srivijaya, Maurian, Kushan, Gupta, and Maratha). We excluded 
the maritime empires of the European Great Powers, because our measure of the latitudinal 
tendency is not applicable to such noncontiguous, widely distributed collections of territories. 
One difficulty in constructing the list was presented by the repeated rise of empires in the same 
location, such as in China. We adopted the middle road of counting each major dynasty (Han, 
Tang, Ming, etc) as a separate empire, but did not distinguish between cycles within a dynasty 
(e.g., Early versus Late Han). Analysis of a reduced dataset, which included only the largest 
empire for each geographic location, yielded qualitatively the same result. See Table 1 for the list 
of empires.  
 
Note 2. Log-transforming the ratio of distances was necessary to make the distribution of the 
index symmetric. Positive values indicate east-west orientation, and negative values – north-south 
orientation.  
 
Note 3. It may seem strange to call the Chinese home biome a â€œforest,” because in present-day 
China, of course, very few forests are left. Remember, however, that the biome names reflect the 
types of ecological communities that would be present before substantial human impact; the 
names are simply a short-hand reference to particular combinations of the climate and soil types.   
 

References 

 

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in

 S. P. Reyna and R. E. Downs, editors. 

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Chase-Dunn, C., S. Manning, and T. D. Hall. 2000. Rise and fall: east-west synchronicity and Indic 

exceptionalism reexamined. Social Science History 

24

:727-754. 

Chase-Dunn, C. K., and T. D. Hall. 1997. Rise and demise: comparing world-systems. Westview Press, 

Boulder, CO. 

Diamond, J. 1997. Guns, Germs, and Steel: The Fates of Human Societies. W. W. Norton, New York. 
McNeill, W. H. 1964. Europe's Steppe Frontier. University of Chicago Press, Chicago, IL. 
Pagel, M., and R. Mace. 2004. The cultural wealth of nations. Nature 

428

:275-278. 

Ricklefs, R. E. 2001. The Economy of Nature, 5th edition. W. H. Freeman, New York. 

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Taagepera, R. 1978. Size and duration of empires: systematics of size. Social Science Research 

7

:108-127. 

Taagepera, R. 1978. Size and duration of empires; growth-decline curves, 3000 to 600 BC. Social Science 

Research 

7

:180-196. 

Taagepera, R. 1979. Size and duration of empires: growth-decline curves, 600 B.C. to 600 A.D. Social 

Science History 

3

:115-138. 

Taagepera, R. 1997. Expansion and contraction patterns of large politices: context for Russia. International 

Studies Quarterly 

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:475-504. 

Turchin, P. 2003. Historical dynamics: why states rise and fall. Princeton University Press, Princeton, NJ. 
Turchin, P., and T. D. Hall. 2003. Spatial synchrony among and within world-systems: insights from 

theoretical ecology. Journal of World Systems Research 

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Legions in the Teutobutg Forest. W. W. Norton, New York. 

 

 
 
 

Table 1. 

 The large historical states used in the analysis.  

 

Date 

(peak) 

Empire name 

World 

Region 

Area 

(Mm

2

)

Latitude

Index 

-1300  Egypt (New Kingdom)  Africa 

1.00

-1.292

350 Axum 

Africa 

1.25

0.241

969 Fatimid 

Africa 

4.10

0.782

1120 Almoravid 

Africa 

1.00

0.561

1200 Almohad 

Africa 

2.00

0.864

1380 Mali 

Africa 

1.10

0.512

1400 Mameluk 

Africa 

2.10

-0.225

1527 Inca 

America 

2.00

-1.139

-176  Hsiung-Nu (Hunnu) 

Central Asia 

9.00

0.818

405 Juan-Juan 

Central 

Asia 

2.80

0.740

557 Turks 

Central 

Asia 

6.00

1.026

800 Uigur 

Central 

Asia 

3.10

0.213

800  Tufan (Tibet) 

Central Asia 

4.60

0.605

850 Khazar 

Central 

Asia 

3.00

0.139

1100 Hsi-Hsia 

Central 

Asia 

1.00

0.655

1210 Khorezm 

Central 

Asia 

2.30

0.054

1210 Kara-Khitai 

Central 

Asia 

1.50

0.362

1270 Mongol 

Central 

Asia 

24.00

0.737

1310  Golden Horde 

Central Asia 

6.00

0.153

1350 Chagatai 

Central 

Asia 

3.50

0.383

1405 Timur’s 

Central 

Asia 

4.40

0.426

-1122 Shang 

East 

Asia 

1.25

0.050

-50 China-Early 

Han 

East 

Asia 

6.00

0.661

579 Liang 

East 

Asia 

1.30

0.137

715 China-Tang 

East 

Asia 

5.40

0.375

947  Liao (Kitan) 

East Asia 

2.60

0.606

980 China-Sung 

East 

Asia 

3.10

-0.164

1126  Jurchen (Chin) 

East Asia 

2.30

-0.147

1450 China-Ming 

East 

Asia 

6.50

-0.138

1790 China-Manchu 

East 

Asia 

14.70

0.246

117 Rome 

Europe 

5.00

0.204

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441 Huns 

(Atilla’s) 

Europe 

4.00

1.003

555 

East 

Roman Europe 2.70

0.516

814 Frankish 

Europe 

1.20

0.092

1000 Kiev 

Europe 

2.10

-0.132

1025 Byzantine 

Europe 

1.35

0.806

1480 Lithuania-Poland 

Europe 

1.10

0.079

1683 Ottoman 

Europe 

5.20

0.320

1895 Russia 

Europe 

22.80

0.303

1200 Srivijaya 

Southeast 

Asia 

1.20

0.272

1290 Khmer 

Southeast 

Asia 

1.00

-0.665

-250 Mauryan 

South 

Asia 

5.00

0.191

200 Kushan 

South 

Asia 

2.00

0.095

400 Gupta 

South 

Asia 

3.50

-0.031

648 Harsha 

(Kanyakubia)  South Asia 

1.00

0.668

1312 Delhi 

South 

Asia 

3.20

-0.082

1690 Mughal 

South 

Asia 

4.00

0.435

1760 Maratha 

South 

Asia 

2.50

-0.280

-670 Assyria 

Southwest 

Asia

1.40

1.845

-585 Media 

Southwest 

Asia

2.80

0.141

-500  Achaemenid Persia 

Southwest Asia

5.50

0.200

-323 Alexander’s 

Southwest 

Asia

5.20

0.478

-301 Seleucid 

Southwest 

Asia

3.90

0.882

0 Parthia 

Southwest 

Asia

2.80

1.374

550  Sassanian Persia 

Southwest Asia

3.50

0.292

750 Caliphate 

Southwest 

Asia

11.10

0.730

928 Samanid 

Southwest 

Asia

2.85

-0.194

980  Buyid (Buwahid) 

Southwest Asia

1.60

0.142

1029 Ghaznavid 

Southwest 

Asia

3.40

0.689

1080 Seljuk 

Southwest 

Asia

3.90

0.409

1190 Ayyubids 

Southwest 

Asia

2.00

-0.300

1310 Il-Khan 

Southwest 

Asia

3.75

0.664

 
 
 

Table 2 

 

Region Mean 

SE 

Africa 0.21 

0.28 

0.72

0.50 

Central 

Asia 

0.48 0.08 13 5.80 <0.001

East Asia 

0.18  0.10  9  1.71

0.12 

Europe 0.35 

0.12 

2.92

0.02 

South & SE Asia 

0.07  0.13  9  0.51

0.62 

Southwest 

Asia 

0.52 0.15 14 3.40

0.005 

America 

–1.14 â€“ 1 –  â€“ 

All 

regions 

0.31 0.06 62 4.83 <0.001

 
 
 
 

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Figure 1. Distribution of world biomes (Ricklefs 2001).  
 

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Latitude Index

Fr

eq

uenc

y

1.5

1.0

0.5

0.0

-0.5

-1.0

18

16

14

12

10

8

6

4

2

0

Egypt
Inca

Khmer

 

 
Figure 2. Frequency distribution of the Latitude Index in the sample of large empires.