|Archaeological Fieldwork in 2006 (2)|
by Sören Stark, Seminar for Oriental Archaeology and Art History Part 2 (return to Part 1)
C. Remains of single farmsteds, field terrasses, enclosures and water installations
In roughly the same altitude sections as the barrows a whole series of single farmsteads, nearby field terraces, enclosures and remains of irrigation channels and the like was traced by surface prospections (figs. 16 and 17).
Figure 16: Single farmsteads, enclosures and water installations
Figure 17: Traces of a single farmstead at the site Baibiche-Kotin-9a
Their overwhelming majority is situated in the southern tributaries of the upper Argly. A clear maximum was recorded in the Kenkul valley and especially in the Baibiche-Kotin valley where they are distributed in a loose order over large parts of the valley. Only two "farmstead" structures were traced in the middle section of the Uguk-sai branch of the valley system (sites Uguk-2 and 3). In most cases traces of field terraces and aryks exist in the close neighbourhood of these sites. In terms of architecture these "farmsteads" resemble each other in layout: Remaining walls are set in rubble respectively small or medium sized stone boulders. Judging from contemporary analogies they represent the foundations of superstructures built from mud bricks and wood. The general outline of these buildings is roughly rectangular or angled (apart from protruding walls of entries and the like), the number of rooms of each structure ranges from two up to a dozen. Often one or two courtyards are attached. There are no traces of substantial cultural layers. The quantity of ceramic material from the surface is very insignificant. Generally this material can be dated from the 7/8th to the beginning of the 13th century. The repertoire of types and forms of vessels as well as their decoration have evident analogies in the material of the neighbouring Aktangi valley system - with two noteworthy exceptions: 1. In contrast to the record of the Aktangi valley (cf. sites Aktangi-2 and Hodja-Mazori-Tug) there are only very few examples of glazed pottery from sites in the upper Argly system. 2. Traces of ancient metallurgy such as slags and furnace fragments are completely lacking from the "farmstead" sites. Thus, despite of resemblances with settlement sites from the neighbouring Aktangi valley there exist some notable differences: Apart from the almost complete lack of glazed pottery and the complete absence of traces of metallurgy, differences pertain to architecture (single farmsteads instead of small settlements) and the location of these mediaeval farmsteads at a surprisingly high elevation up to 2900 m (whereas the Aktangi sites were confined to altitudes up to 2400 m). This points to a character of these sites which is generally different from the one of the Aktangi settlements: In contrast to the Aktangi settlements the farmsteads in the upper Argly system seem to have been essentially seasonal in character. Until today similar seasonal farmsteads can be observed in the same altitude section of the valley system. Yet another aspect is suggested be contemporary analogies: Today, a good part of the inhabitants of seasonal farms in the Upper Argly system originates from the upper Zarafshan valley, that is from beyond the mountain range. There, agricultural resources are scarce, which nowadays forces people from Aini and Matcha to use the upper Argly valley from spring to early autumn for tending their herds (sheep, goats, cows) and cultivating barley, ray and oat. A similar seasonal pattern of land use might be suggested for the pre Mongol farmsteads in question: The general prosperity of Mawarannahr in the pre-Mongol period might have caused population pressure in the region which might have been a stimulus for the seasonal use of these marginal areas. Like today, seasonal inhabitants might have originated at least partly from Matcha or Fan.
D. Shelters and caves
In contrast to the neighbouring Aktangi valley rock shelters and caves are a rare feature in the archaeological record of the Argly system (fig. 18).
Figure 18: Shelters and caves
None of these sites yielded substantial traces of non-recent human occupation.
E. Isolated stray finds
Figure 19: Isolated stray finds
Stray finds without any related archaeological features at the spot (fig. 19) are mostly confined to pottery sherds. Most of them seem to be "mediaeval" in date (as far as they could be determined). In sharp contrast to the prospection results from the Aktangi system there are almost no stray finds of iron slags and furnace fragments. The only exception is the site Kabutag-2 where a large quantity of slags and furnace fragments were recorded. But this site is located at the feet of the Argly pass thus in immediate neighbourhood of the Aktangi system to which it, therefore, seems economically related. The most remarkable stray find from the upper Argly valley is a chopping tool (14,6 x 10,3 x 7,1 cm) of one of the eastern hill terraces of the Tukchi valley (site Tuktchi-4).
Figure 20: Chopping tool
Its 6 cm long semi-oval and bifacial cutting edge has an angle of 110º. It is flaked in one of the narrow ends of the regularly oval pebble core (porphyrit). A distinct pebble stone industry with similar chopping tools is known from several Middle Paleolithic (Mousterian) sites in the piedmont region of the Turkestan range (sometimes labelled as "Shakhristan-sai paleolithic"). Another untypical stray find from the upper Argly valley is a grindstone (site Kenkul-17) which is most probably related to one of the nearby mediaeval farmsteads (Kenkul-1 to 6).
2.2 The Lower part of the Argly system
The archaeological record from the lower part of the Argly system (around the present-day kishlaks of Ovchi and Uguk) is constituted by the following groups of material:
A. Qal'a-i-Mugh (site Qal'a-i-Mugh-1)
The early-mediaeval fortress of Qal'a-i-Mugh (lit.: "Castle of the Magus") is situated a the north-western margins of the present-day kishlak Ovchi (see map in fig. 26). It was first mentioned and described by A. I. Bilalov in the course of his investigations of the Basmanda-sai irrigation in 1974. The site is situated at the north-eastern end of a plateau which runs about 4 km from south-west to north-east between the mountains in the north and the plain of the Argly in the south and is intersected by several small wadis.
Figure 21: Qal'a-i-Mugh
Whereas the northern and the south-eastern edges of the qal'a are naturally defended by steep slopes (up to 40 m high), the south-western and western flanks are defended by artifical moats. In addition, substantial remains of fortification walls of mud bricks on stone fundaments can be observed in the south-western edge of the fortress. The inner area of the fortress measuring ca. 135 m from east to west and 37-145 m from north to south is relatively flat, except for a nearly quadratic elevation (ca. 16 x 18 m) at the eastern edge of the fortress which seems to represent the remains of a small donjon or a keshk. Surface findings of pottery sherds date from the 6th and the 7-8th centuries (fig. 27/2, 4, 5). This corresponds to the dating suggested by Bilalov. The location of the qal'a is wisely chosen: It not only provides control over the irrigation oasis of the lower Argly valley but also controls the entry into the Obburdon valley and thus, via the Obburdon pass, the most convenient access to Matcha in the upper Zarafshan valley and to other areas further southwards in Northern Bactria/Tokharistan.
Our prospections identified three further sites which belong to the former fortification system of the lower Argly valley (Qal'a-i-Mugh-2, Qal'a-i-Mugh-4 and Argly-7). Both Qal'a-i-Mugh-2 and Qal'a-i-Mugh-4 are situated some 40 m above the plain, on the steep slope of the plateau, about 1 respectively 2,5 km to the south-west of the qal'a (Qal'a-i-Mugh-1) (see map in fig. 26). Today both sites form small clay elevations of about 10 m in diameter and 1-2 m height. Whereas in the case of Qal'a-i-Mugh-2 no ceramic material could be collected from the surface, some early-mediaeval sherds were recorded in the plain at the foot of Qal'a-i-Mugh-4. Possibly, both sites are of early-mediaeval date and constitute a communication line between the qal'a and the edge of the irrigation oasis (where Qal'a-i-Mugh-4 is situated) towards the upper parts of the Argly valley. A third site of this category (Argly-7) is situated on hill-slope at the north-eastern margin of the present-day kishlak. Obviously, this watchtower holds an important strategic position as it is situatated immediately opposite the branch-off into the Obburdon valley. What is still traceable are remains of pakhsa foundations. Ceramic material, however, was absent from the site's surface. Nevertheless, it seems reasonable to suggest that the site Argly-7 dates also to the Mediaeval period when such kind of watchtowers were common in Mawarannahr. A last monument which formerly complemented the fortification system of the Argly valley system was reported to us by the local population in the Uguk branch of the lower Argly system. Today it has completely disappeared because of recent building activities. According to our informants it represented a fortified farmstead in the very centre of Uguk, on a steep slope, ca. 20 m above the Uguk-sai. Its former location is still called "Qal'a" by the local population. Possibly, this fortification should be interpreted as a late-mediaeval refuge.
Burials have been reported by locals from different spots in the lower part of the Argly valley. These informations could be complemented by our own field observations at the site Qal'a-i-Mugh-3 which is situated at the north-western foot of the early-mediaeval qal'a towards a wadi called "Tangiston" (fig. 22; cf. map in fig. 26). Here, recent building activities revealed an unknown number of burials. The remains of four of them were still visible in situ.
Figure 22: Remains of Burials at Qal'a-i-Mugh-3
They were cut open by a recent dredger trench in a hill slope thus displaying a profile roughly oriented towards north-west. Judging from our field observations the grave chambers were constructed either as stone cists (1 case) or as burial vaults made of small and medium sized stone boulders (3 cases). At the time of our inspection on-site, human remains were already removed. But at least the remains of the cist suggest single-burials. As far as observable on-site (i.e. without excavation) all four burials were oriented NW-SE. Both construction and orientation have analogies in early Muslim burials from other cemeteries in highland Ustrushana (Aktangi-7, Kalai-Sar), lowland Ustrushana (Kul'-tyube) and the upper Zarafshan valley (Zosun), thus suggesting a date roughly between the 9th and the 12th century. However, burials at this site don't seem to be restricted to this period alone. Locals report of chance finds of at least four more burials in this area. Unfortunately, all remains of their construction had already disappeared by the time of our prospection. But we were shown two completely preserved ceramic vessels (a jar and a small flacon) which, supposedly, stem from these unrecorded burials (figs. 23 and 27/3). Both vessels can be securely dated to the 5th-6th centuries.
Figure 23: Jar from Qal'a-i-Mugh-3 (chance find)
Further finds of human burials were reported from a spot in the south-western margin of the present-day kishlak. Until now this location is called "Qal'a-i-Zindon" or "Qal'a-i-Sugud" (see below). Finally, a number of small rubble stone mounds have been traced around the site of Uguk-3 which might represent burials. According to our informants this place is considered by locals as the "original" cemetery of Uguk.
D. Non-recent irrigation structures
Today the lower parts of the Argly valley around Ovchi and Uguk are predominantly characterized by irrigated agriculture. This certainly holds true also for earlier periods as remains of two karezes at both sides of the Basmanda-sai gorge between the lower Argly valley and the kishlak Basmanda confirm (fig. 23).
Figure 24: Remains of a Karez at the right bank of the Basmanda-sai
Both karezes probably date from the pre-Mongol period as present-day Basmanda is most probably to be intendified with mediaeval Marsmanda which boomed in the 10-12th centuries as a supra-regional market place for iron tools and weapons. Similar underground channels of probably the same date are known from other areas in mediaeval Ustrushana (e.g. south of Shahriston).
E. Isolated stray finds
As usual, the main category of stray finds in the lower sections of the Argly system are ceramic sherds. A rather unusual stray find was shown to us by an informant in the remote Shagan-valley, about 5 km to the south of present-day Uguk, namely several fragments of an iron mail (fig. 25).
Figure 25: Fragments of a mail from Uguk-1
They supposedly stem from the vicinity of some unclear stone settings (site Uguk-1). Without any archaeological context it is difficult to suggest a definite dating for this find as similar mails were in use in Mawarannahr over quite a long period - up into the 19th-early 20th century. However, the comparatively good state of preservation of the fragments might suggest a rather recent dating (late-mediaeval to 19th-20th century?). As for ceramic stray finds, two spots received special attention in the course of our field work.They were pointed out to us by the local population (cf. map in fig. 26).
Figure 26: Archaeological sites around present-day Ovchi
Figure 27: Sample of ceramic finds from different spots around Ovchi.
1 - Qal'a-i-Zindon; 2, 4, 5 - Qal'a-i-Mugh-1; 3 - Qal'a-i-Mugh-3; 5, 6 - Qal'a-i-Asmâkat
The first one is sitated 300-500 m to the south of the qal'a (Qal'a-i-Mugh-1) and streches over two terraces above the right bank of the Argly-sai, near its confluence with the Rabut-sai. Until the late 40s when this spot was opened up for cultivation, substantial settlement traces where supposedly situated at the spot. Still today these terraces are called "Qal'a-i-Asmâkat" ("Qal'a-i-Asmokat" in modern Tadjik spelling) by the local population. Though architectural remains have by now completely disappeared, prospections revealed a great number of ceramic sherds at the spot, dating roughly to the early-mediaeval and pre-Mongol periods (7/8th-11/12th centuries) (fig. 27/5,6). The second spot which was closer examined in the course of our fieldwork is now situated in the south-western margins of the present-day settlement, which is called "Zindon" (lit.: "Prison"), "Qal'a-i-Zindon" or "Qal'a-i-Sugud" by the locals. Until its destruction in the middle-eighties a small tepa of ca. 30 m diameter and 1-2 m was situated at this spot (first mentioned by Bilalov). Although today this monument is completely bulldozered and overbuilt by a farmstead, a number of ceramic sherds was collected from its vicinity. One of them seems to date to late Antiquity (4-5th centuries) (Fig. 27/1), others are early-mediaeval in date. Stray finds from Qal'a-i-Mugh-1 and from the Ovchi plain now allow a more detailed reconstruction of the settlement history in the Ovchi area (cf. map in fig. 26): The earliest ceramic record is associated with the find spot of Qal'a-i-Zindon (4-5th century). Hypothetically this earliest traceable site might be interpreted as an fortified farmstead ("usad'ba" in Russian-language publications) or a very small rural castle. However, there is no certainty about the exact chronological relation to Qal'a-i-Mugh. Both sites might at least partly be simultaneous in date. However, for the most part of the Early Middle Ages (6th-8th/9th century) Qal'a-i-Mugh-1 should be identified as the seat of the local dihqân. At the same time, the qal'a might have served as a refuge for the villagers living in the valley. At any rate, the existence of such heavily fortified sites is typical for the pre-Muslim Middle Ages when political structures were extremely fragmented. Internal contentions between several minor principalities as well as the grip of external enemies (e.g. frequent Turkic and Muslim incursions) posed a constant threat to the oasis populations in most parts of pre-Muslim Mawarannahr. This situation only changed after the successive incorporation of Transoxania in the Caliphat respectively its eastern Iranian successors. Consequently, most of the former fortifications lost their importance and were abandoned at that time. The same seems to hold true for Qal'a-i-Mugh-1 which was abandoned at one point after the 8-9th century (however, it has to be kept in mind that Ustrushana became comparatively lately part of the "Dâr al-Islâm"). In the following period the settlement centre seems to have moved to a more convenient place at the bottom of the valley, which is attested by stray finds of pottery from the 10-12th century at the site of Qal'a-i-Asmâkat (this coincides chronologically with the integration of this area into the more centralized Sâmânid and Kharakhanid states which provided more political and economic stability than the earlier minor principalities). At the same time, it seems that the settlement retained its older, pre-Muslim, toponym as the name of the pre-Mongol site, handed down by the local population in the form of Asmâkat (Tajik spelling: "Asmokat"), contains the well-known toponym formans "kat" (from Soghdian "ka(n)th"). It might, therefore, be suggested that the toponym "Asmâkat(h)" represents (although in a possibly distorted form) the early-mediaeval toponym of Qal'a-i-Mugh and its rural hinterland.
After two field seasons we can now clearly determine and classify the presence of mobile pastoralists in the sample area by archaeological means. They include barrow grounds, petroglyphs, shelters and caves as well as stone enclosures (herdsmen's stations). Notably the barrow grounds constitute an important new source for the history of pastoral-nomadic groupings in this part of Central Asia which will have to be explored by further field work. At the same time our investigations in 2005 and 2006 revealed considerable differences on a micro-regional level even within one and the same high mountain zone: Whereas the archaeological record in the Aktangi system is dominated by "compact" settlements and scattered herdsmen's stations respectively rock shelters, the Argly system offers a totally different spectrum of types of sites: barrows, petroglyphs, single farmsteads and marginal oasis settlements. Partly, these differences might be explained ecologically as the Aktangi system seems to be more "alpine" in character than the more arid Argly system (at least judging from their present appearance). Other possible explanations might be related to external and basically historical factors. Thus, the Argly system is even more secluded than the Aktangi valley, communicating with the lowlands to the north only via a very narrow and difficult mountain gorge (fig. 28).
Figure 28: Mountain gorge between the Argly valley system and Basmanda
Notably the upper part of the Argly system with its multitude of dead end tributary valleys is extremely peripheral in character. This "remoteness" might at least partly count for the fact that many of these valleys were chosen - most probably by mobile pastoralists - as burial areas. If this assumption turnes out to be true, the upper Argly valley would constitute a major burial area of pastoral groupings in Ustrushana. Similar differences between both valley systems can be observed for the pre-Mongol Middle Ages: The Aktangi system is characterized by a stimulated development of compact settlements notably in the lower sections of the valley system. These settlements seem to have been integrated in the market economy of the urban central place in the nearby Shahriston oasis and beyond - they probably supplied these markets with products of the high mountain zone (iron and products of cattle breeding) and received in return products of urban industries (e.g. glazed pottery). In contrast to that, settlement in the Argly valley was dominated by seasonal single farmsteads in the upper sections of the valley systems whose ceramic record seems distinctively less "urban" in character (almost complete lack of glazed pottery) - an observation which also holds true for the ceramic record from the irrigated lower section of the Argly system. Thus, in neighbouring valley systems different settlement structures seem to evolve on the basis of a different external grip on these highland valleys.
Team 2006 (from left to right) - Abdulhamid Hamidov (driver), Matthias Gütte,
Usman Eshankulov, Alexander Puk, Sören Stark, Nabi Rahimov
 Special thanks go to Matthias Gütte who prepared all maps and plans.
 Bilalov, A. I. 1978: "O rabote gornogo arkheologo-topograficheskogo otryada STAKE v 1974 g.", Arkheologicheskie raboty v Tadjikistane 14 (1974), pp. 356-358
 Bilalov, A.I. 1980: Iz istorii orosheniya Ustrushany, Dushanbe, p. 46 (=Material'naya kul'tura Ustrushany, vyp. 4)
 Voronina, V.L. 1980: "Pamyatkiki Kalinabada i ego okrestnostei", Arkheologicheskie raboty v Tadjikistane 15 (1975), 324-335; Negmatov, N.N. 2003, "Istoriko-kul'turnaya oblast' Ustrushana" (=Material'naya kul'tura Ustrushany, vyp. 5), In: Drevnyaya Ustrushana: Goroda, ikh lokalizaciya i khronologiya, Dushanbe
 Fedchenko, A. P. 1873: "Kariz", Materialy dlya statistiki Turkestanskogo kraya, Sankt-Peterburg 1873, p. 91; Idem 1950: Puteshestvie v Turkestan, Moskva, p. 149; Bilalov, A.I. 1973: "K istorii orosheniya Ustrushany (bassein Basmandasaya), Izvestiya AN TadjSSR, Otdel. obshch. nauk 2/72 (1973), pp. 32-33; Idem 1980: Iz istorii orosheniya, pp. 45-47
 Bilalov, "O rabote", pp. 356-358
 These Karezes were first mentioned by Fedchenko ("Kariz", p. 91) and later investigated by Bilalov ("K istorii orosheniya, pp. 32-33; Iz istorii orosheniya, pp. 45-47).
 This identification is contested by L. Sverchkov. However, Sverchkov's recent proposal to identify mediaeval Marsmanda with one of two sites to the south of Bakhmal in the Upper Sanzar valley ("Zamok Myk i ego okruga", in: Drevnii Zaamin, Tashkent 1994, p. 61) is problematic for several reasons: Sverchkov is basing his arguments mainly on al-Idrîsî's geographical work (Kitâb Nuzhat al-mushtâq fi 'khtirâq al-âfâq) which reads: "And between Marsmanda and Nûjkath (there are) two days (of travel); and between Marsmanda and the fortress Mînk (there is) a long day's journey." (ed. Naples-Rome, p. 506, l. 2-3; translation by E. Wakelnig). At the same time Sverchov wants to locate mediaeval Nûjkath at the present-day kishlak Nushkat in the lower Sanzar valley. However, Sverchkov seems to overlook that a few lines earlier (p. 505, l. 17) the same Idrîsi states: "And close to the aforementioned city Bunjikath there is the city Marsmanda" (translation by E. Wakelnig). The following conclusions might be drawn from this: 1) Idrîsî, probably a native from Ceuta who later lived at the court of the Norman kings in Palermo, never traveled beyond Spain, Sicily and North Africa. With regard to toponyms and distances in Mawarannahr he was obviously dependent on the reports of others and, therefore, easily exposed to errors (not to speak of the errors of later copists). Consequently, the mention of Nûjkath in the passage in question should be used with utmost care as this small and little known town never figures in any other extant itinary. Instead, it seems much more likely that "Nûjkath" (one manuscript has "Nîjkath") is but a mere corruption of the far more important capital of Ustrushana, Bunjikath, whose name can be in Arabic transcription ( , and many other variants) easily corrupted into Nûjkath ( ) or Nîjkath ( ). 2) Idrîsî's statement that Marsmanda is situated "close to" Bunjikath is perfectly true for present-day Basmanda but hardly acceptable for Bakhmal in the Sanzar valley. Even if we assume the location of Bunjikath at the site of Shahriston, the communication between the Sanzar valley and the Shahriston valley is rather difficult: The only convenient route leads via Zaamin whereas any shorter route has to make use of a multitude of difficult mountain pathways over passes up to 3100 m. Contrasting to that, the route from Shahriston to Basmanda via Dalyon-i Bolo is easy and takes about 40-45 km, that is exactly a two days' journey.
 Bilalov, A.I.: Iz istorii irrigacii Ustrushany (Material'naya kul'tura Ustrushany, vyp. 4), Dushanbe 1980, p. 46
 I would like to thank P.B. Lur'e for his comments on this toponym in a personal communication.
 Up to now I was unable to find any undisputable evidence for such an "Asmâkat(h)" in a mediaeval source. At first sight, the "Ashkâl al-'âlam", an abridged Persian translation of Istakhrî's "Masâlik wal-Mamâlik" seems to offer a close parallel by mentioning a town of "Arsmânkath" ( ) (Mukhtorov, A.: Amiron va vaziron somonî, Dushanbe 1997, p. 29). However, this is probably a corruption from "Arsbânîkath" ( ) or "Arsiyânkath" ( ), that is mediaeval Isfana.
|Sonderforschungsbereich 586 - Differenz und Integration.|
Wechselwirkungen zwischen nomadischen und seßhaften Lebensformen in Zivilisationen der Alten Welt.
Eingerichtet an der Martin-Luther-Universität Halle-Wittenberg und der Universität Leipzig.
Gefördert von der Deutschen Forschungsgemeinschaft.
|Teilprojekt D6 - Home|
Selbstsicht und Fremdsicht
Seminar für Orientalische Archäologie und Kunstgeschichte der Martin-Luther-Universität Halle-Wittenberg
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