Teniky: enigmatic architecture at an archaeological site in southern Madagascar

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ABSTRACT

Teniky is an isolated inland archaeological site in the Isalo massif of southern Madagascar, with enigmatic rock-cut architecture that is unique in all of Madagascar and the wider East African coast. In the first half of the twentieth century visitors described archaeogical structures within a fluvial cirque (i.e. an amphitheatre-shaped valley formed by fluvial erosion), which included man-made terraces, rock-cut niches in the steep cliffs and a rock shelter delimited by walls consisting of carved sandstone blocks. Our investigations at Teniky have led to the discovery of further archaeological structures beyond the cirque. These structures include further terraces, rock-cut niches, stone basins and carved sandstone walls on a hill 2.5 km to the west, as well as sandstone quarries and dry stone walls in the valley in between. AMS radiocarbon dating of charcoal found during excavations at the newly discovered rock-cut niches and carved sandstone walls indicates that they were constructed in the late first millennium/early second millennium c. tenth to twelfth century AD. Pottery sherds at Teniky include Chinese and Southeast Asian ceramics dating to broadly the eleventh to fourteenth centuries, concordant with the radiocarbon ages. The presence of imported ceramics indicates that those living at Teniky participated in Indian Ocean trade networks in medieval times, despite being over 200 km from the nearest coast. The closest stylistic parallels to the enigmatic rock-cut architecture at Teniky are found in present-day Iran, particularly in the Fars region, where rock-cut niches dating to the first millennium AD or earlier have been attributed to Zoroastrian communities. We tentatively interpret the rock-cut architecture at Teniky as part of a former necropolis made by settlers with Zoroastrian origins. More archaeological research is required to test this hypothesis and to address questions such as: where and when did these settlers first arrive on the coast of Madagascar; why and when did they move inland; how did they live and how did they interact with other populations on the island; and why and when was the site deserted?

RÉSUMÉ

Teniky est un site archéologique isolé à l’intérieur des terres dans le massif de l’Isalo au sud de Madagascar, avec des vestiges rupestres énigmatiques qui sont uniques dans tout Madagascar et sur la côte plus vaste de l’Afrique de l’Est. Dans la première moitié du vingtième siècle, les visiteurs ont décrit des vestiges archéologiques dans un cirque fluvial (c'est-à-dire une vallée en forme d’amphithéâtre formée par l’érosion fluviale), comprenant des terrasses artificielles, des niches creusées dans les falaises abruptes et un abri sous roche délimité par des murs constitués de blocs de grès taillés. Nos recherches à Teniky ont permis de découvrir d’autres vestiges archéologiques au-delà du cirque. Ces vestiges comprennent d'autres terrasses, des niches creusées dans la roche, des bassins en pierre et des murs en grès taillés sur une colline située à 2.5 km à l’ouest, ainsi que des carrières de grès et des murs en pierres sèches dans la vallée intermédiaire. La datation au radiocarbone AMS des charbons de bois trouvés lors des fouilles des niches creusées dans la roche et des murs de grès sculptés récemment découverts indique qu’ils ont été construits à la fin du premier millénaire/début du deuxième millénaire (vers les dixième au douzième siècles) après J.-C. Les tessons de poterie de Teniky comprennent des céramiques chinoises et d'Asie du Sud-Est datant du onzième au quatorzième siècles après J.-C., ce qui concorde avec les âges radiocarbones. La présence de céramiques importées indique que les habitants de Teniky ont participé au réseau commercial de l’océan Indien à l’époque médiévale, bien qu’ils aient vécu à plus de 200 km de la côte la plus proche. Les parallèles stylistiques les plus proches de l'architecture énigmatique de Teniky se trouvent en Iran, en particulier dans la région de Fars, où des niches creusées dans la roche datant du premier millénaire après J-.C. ou plus tôt ont été attribuées à des communautés zoroastriennes. Nous interprétons provisoirement l’architecture taillée dans les roches à Teniky comme faisant partie d’une ancienne nécropole construite par des personnes ayant des origines zoroastriennes. Des recherches archéologiques supplémentaires sont nécessaires pour tester cette hypothèse et répondre à des questions telles que: où et quand ces migrants sont-ils arrivés pour la première fois sur la côte de Madagascar; pourquoi et quand se sont-ils déplacés vers l'intérieur des terres; comment ont-ils vécu et comment ont-ils interagi avec d’autres populations sur l’île; et pourquoi et quand le site a-t-il été déserté?

Introduction

Madagascar is situated in the southwestern Indian Ocean and is considered one of the last big islands to have been settled by humans. There is still considerable debate on the origin of the Malagasy population and when the first settlers arrived. Contributions of African, Asian, Indian, Austronesian, Arab and Persian populations have been suggested based on physical and cultural anthropology, oral traditions, linguistics and archaeology (e.g. Heiske et al. Citation2021). Genetic studies have identified African and Asian populations as the main contributors, yet with pronounced regional variability in the relative contribution of these two ancestries (Heiske et al. Citation2021). Bones with tool marks believed to indicate human butchery have been dated between approximately 10,000 and 1000 years BP and have been used to indicate an early human presence on the island (e.g. Gommery et al. Citation2011; Hansford et al. Citation2018, Citation2020). However, several authors have challenged reported evidence of human butchery prior to c. 1200 BP (Anderson et al. Citation2018; Mitchell Citation2019, Citation2020, Citation2022). Archaeology has so far only documented a relatively late settlement of Madagascar during the mid- to late first millennium AD, with possible exceptions provided by excavations at a rock shelter in the Velondriake area along the coast of southwestern Madagascar, where dated avian eggshell suggests a periodic campsite for mobile foragers at least 2000 cal. BP (Douglass et al. 2019), and others at two rock shelters in northern Madagascar, where Dewar et al. (Citation2013) infer the presence of stone tool-using foragers at least as early as 2000 BC. shows the location of archaeological sites dating to the period AD 700–1100 (Battistini and Vérin Citation1966, Citation1971; Wright and Fanony Citation1992; Dewar and Wright Citation1993; Radimilahy Citation1998, Citation2016; Rakotoarisoa Citation1998; Parker Pearson et al. Citation2010; Serneels et al. Citation2018, Citation2019, Citation2020, Citation2021; Anderson Citation2021).

Figure 1. Digital elevation model of Madagascar. Circles indicate early archaeological sites. Except for Velondriake, Lakaton’i Anja and Ambohiposa, they indicate archaeological sites dating to c. AD 700–1100. The model is compiled from Battistini and Vérin (Citation1966, Citation1971), Wright and Fanony (Citation1992), Dewar and Wright (Citation1993), Radimilahy (Citation1998, Citation2016), Rakotoarisoa (Citation1998), Parker Pearson et al. (Citation2010), Serneels et al. (Citation2018, Citation2019, Citation2020, Citation2021), Douglass et al. (2019), Anderson (Citation2021) and Wright et al. (Citation2022). The black solid square indicates the location of Teniky in southern Madagascar, whereas black open squares indicate other sites mentioned in the text.

Figure 1. Digital elevation model of Madagascar. Circles indicate early archaeological sites. Except for Velondriake, Lakaton’i Anja and Ambohiposa, they indicate archaeological sites dating to c. AD 700–1100. The model is compiled from Battistini and Vérin (Citation1966, Citation1971), Wright and Fanony (Citation1992), Dewar and Wright (Citation1993), Radimilahy (Citation1998, Citation2016), Rakotoarisoa (Citation1998), Parker Pearson et al. (Citation2010), Serneels et al. (Citation2018, Citation2019, Citation2020, Citation2021), Douglass et al. (2019), Anderson (Citation2021) and Wright et al. (Citation2022). The black solid square indicates the location of Teniky in southern Madagascar, whereas black open squares indicate other sites mentioned in the text.

Teniky (also known to as ‘Tenika’) is an inland site with enigmatic rock-cut architecture in central-southern Madagascar, some 200 km from the Mozambique Channel to the west and 275 km from the Indian Ocean to the east (). It is located in the heart of the Isalo National Park and can only be reached on foot, requiring a 20 km hike across rugged terrain dissected by steep canyons. Although the presence of archaeological structures at Teniky has been known for well over 100 years, until now they were only known from a fluvial cirque (i.e. an amphitheatre-shaped valley formed by fluvial erosion) that is partially enclosed by approximately 30–40-m-high cliffs and open to the southwest (). Paulian and Dommergues (Citation1950), Ginther and Hébert (Citation1963) and Ramilisonina and Rakotoarisoa (Citation1971) have succinctly described archaeological structures within this cirque, which include man-made terraces, dry stone walls and rock-cut niches of various sizes and shapes.

Figure 2. Teniky: satellite image of the cirque showing man-made terraces covering an area of about 20 hectares. The red star indicates the location of the Grande Grotte (‘Grotte des Portugais’). Yellow lines trace dry stone walls partially delimiting the cirque. Google Earth 7.3.6.9345 (2 February 2010). Madagascar. 22°18’09.47’’S, 45°18’27.20’’ E, Eye alt 1.30 km. Maxar Technologies 2023. www.earth.google.com (20 December 2023).

Figure 2. Teniky: satellite image of the cirque showing man-made terraces covering an area of about 20 hectares. The red star indicates the location of the Grande Grotte (‘Grotte des Portugais’). Yellow lines trace dry stone walls partially delimiting the cirque. Google Earth 7.3.6.9345 (2 February 2010). Madagascar. 22°18’09.47’’S, 45°18’27.20’’ E, Eye alt 1.30 km. Maxar Technologies 2023. www.earth.google.com (20 December 2023).

The best-known and most prominent structure at the cirque of Teniky is the ‘Grande Grotte’ ( and ), a large rock shelter delimited by neatly constructed sandstone walls (Ginther and Hébert Citation1963). In the early twentieth century, French naturalists Alfred and Guillaume Grandidier suggested that shipwrecked Portuguese sailors constructed the walls in the early sixteenth century AD (Paulian and Dommergues Citation1950) and the rock shelter is also known as the ‘Grotte des Portugais’. In their attempts to reach a port where Portuguese ships might be present they traversed the island, stayed in the Isalo Massif and supposedly built the walls at Teniky (Paulian and Dommergues Citation1950). Ginther and Hébert (Citation1963) doubted this interpretation, particularly because of the considerable effort that must have gone into constructing the numerous terraces within the cirque. They dug a trench at the Grande Grotte without being precise on its exact location and extent and reached a reddish soil at a depth of 40–50 cm. No archaeological objects were recovered from the trench. However, they did find a few pottery sherds on the slopes of the cirque and Vérin (Citation1986) mentions that one of these was considered by John Kirkman (who excavated at Gedi on the East African coast in the 1940s and 1950s; Kirkman Citation1954) to be part of a Chinese jar of the sixteenth century AD.

Figure 3. Teniky: the inner sandstone wall at the Grande Grotte in 1940 or 1941. Copyright Musée d’Ethnographie de Genève (MEG), photographs by Jacques Faublée.

Figure 3. Teniky: the inner sandstone wall at the Grande Grotte in 1940 or 1941. Copyright Musée d’Ethnographie de Genève (MEG), photographs by Jacques Faublée.

An inspection of high-resolution satellite images of Teniky in 2019 revealed that the extent of the archeological site was much larger than previously known. The images showed the presence of a large number of terraces and linear and rectangular structures on a north-south trending hill west of the Sahanafo River (, Zone 2) some 2.5 km from the cirque. These new findings, and the fact that no detailed archaeological excavations had ever been carried out at Teniky, motivated us to carry out an archaeological survey of this intruiging site in an attempt to constrain the timing of its occupation and to better understand the rock-cut architecture in order to make inferences about the origin and culture of those who once lived at the site.

Figure 4. Teniky: overview of the site with the Sahanafo River in the central north-south trending valley. Zones 1–8 contain archaeological structures discussed in the text. Black rectangles within Zone 2 indicate the location of satellite images shown in more detail in . The inset at the top right shows a Sakalava tomb. Google Earth 7.3.6.9345 (2 February 2010). Madagascar. 22°18’08.17’’S, 45°17’40.60’’ E, Ey­­e alt 5.26 km. Maxar Technologies 2022. www.earth.google.com (25 October 2022).

Figure 4. Teniky: overview of the site with the Sahanafo River in the central north-south trending valley. Zones 1–8 contain archaeological structures discussed in the text. Black rectangles within Zone 2 indicate the location of satellite images shown in more detail in Figure 27. The inset at the top right shows a Sakalava tomb. Google Earth 7.3.6.9345 (2 February 2010). Madagascar. 22°18’08.17’’S, 45°17’40.60’’ E, Ey­­e alt 5.26 km. Maxar Technologies 2022. www.earth.google.com (25 October 2022).

Here, we present results of field surveys and excavations carried out at Teniky in 2021 and 2022. During field prospecting in 2021 we discovered a new site with rock-cut niches under a rock overhang on the western flank of the north-south trending hill west of the Sahanafo River hidden from view by dense vegetation (GPS co-ordinates: 22°17’53.9”S, 045°17’10.9”E; ). The niches have been cut into the rock over a length of about 25 m. Remnants of walls consisting of carved sandstone blocks were visible in front of the main niche, with the blocks having a similar composition and dimensions as those making up the sandstone walls at the Grande Grotte. In 2022, we continued surface prospecting and carried out excavations in front of the newly discovered niches.

For descriptive purposes, we distinguish eight zones of archaeological interest at Teniky (). The rock-cut niches discovered in 2021 are located within Zone 1, which forms part of the north-south trending hill with terraces and dry stone walls (Zone 2). Zone 3 is situated just east of the Sahanafo River and includes dry stone walls in a forested area of ∼80 × 80 m, a 120-m-long east-northeast trending dry stone wall in its northern part and a 750-m-long north-northeast trending dry stone wall in its eastern part. Zone 4 and 5 include sandstone quarries respectively discovered on the western and eastern side of the Sahanafo River. Zone 6 contains a nearly closed circular, dry stone wall with a diameter of approximately 150 m visible on satellite images, whereas Zone 7 comprises terraces and dry stone walls on a ridge overlooking the Sahanafo Valley, some 600 m north of the cirque. Finally, Zone 8 covers the cirque with the archaeological structures, including rock-cut architecture, terraces and carved sandstone walls, known since at least the late nineteenth century.

During our field surveys, we observed six stone tombs, mostly on ridges at higher elevations (the purple squares in ). The approximately square stone tombs are about 1 to 1.5 m high and sometimes several stone tombs occur next to each other, with a total surface area up to about 10 m2 (inset in ). All the tombs showed signs of destruction and looting. According to our local guides, these tombs are associated with the Sakalava ethnic group, which inhabited the region before being driven out by another ethnic group, the Bara, probably in the nineteenth century. Mid-twentieth-century maps of the Isalo region show the presence of a village called Sahanafo (or Sahanafa) on the east bank of the Sahanafo River. When the Isalo National Park was established in 1962, the inhabitants of Sahanafo were relocated outside the park’s limits and the village was abandoned. The village’s exact location is unknown, but it was probably within or close to Zone 3. Remains of dry stone walls were observed in the field at or near its presumed location (Zone 3). However, it remains unclear when and by whom these walls were constructed and whether they do indeed form part of the former village of Sahanafo.

We first describe the known archaeological structures at the cirque in Zone 8. This is followed by the results of our excavations at the rock-niches in Zone 1 and the results of surface prospecting in Zones 2 through 7. Subsequently, we provide an interpretation of our observations and their significance in the discussion and conclusions to this paper.

Archaeological structures within the cirque (Zone 8)

Satellite images of the cirque show the presence of man-made terraces constructed on the slopes of the cirque and covering an area of about 20 hectares (; Zone 8 in ). The terraces vary in size and shape, with the largest having a surface area of about 1200 m2. Field prospecting reveals that most of these terraces have one or more dry stone walls on the downward valley side. A major northeast-southwest trending dry stone wall (up to 1 m wide and 2 m high) follows the ridge of the cirque on its northwestern side, with a similar wall running north-northwest/south-southeast on a hill slope further south (). Below, we describe and illustrate the main archaeological structures within the cirque (), most of which have previously been mentioned by Paulian and Dommergues (Citation1950), Ginther and Hébert (Citation1963) and Ramilisinona and Rakotoarisoa (1973).

Figure 5. Teniky: aerial view toward the northeast showing the location of the main archaeological structures at the cirque of Teniky: 1) rock-cut chamber with pillars and benches (the Petit Grotte); 2) a series of six rock-cut niches; 3) circular rock-cut niches with recesses; 4) a large rock shelter with sandstone walls and a rock-cut niche (the Grande Grotte or ‘Grotte des Portugais’); 5) a series of about 35 small circular rock-cut niches; 6) ten rock-cut niches separated by vertical walls; 7) a major terrace with aligned sandstone slabs and carved rock boulders; 8) a series of four circular rock-cut niches; 9) six unfinished rock-cut niches; 10) large rock-cut boulders.

Figure 5. Teniky: aerial view toward the northeast showing the location of the main archaeological structures at the cirque of Teniky: 1) rock-cut chamber with pillars and benches (the Petit Grotte); 2) a series of six rock-cut niches; 3) circular rock-cut niches with recesses; 4) a large rock shelter with sandstone walls and a rock-cut niche (the Grande Grotte or ‘Grotte des Portugais’); 5) a series of about 35 small circular rock-cut niches; 6) ten rock-cut niches separated by vertical walls; 7) a major terrace with aligned sandstone slabs and carved rock boulders; 8) a series of four circular rock-cut niches; 9) six unfinished rock-cut niches; 10) large rock-cut boulders.

Rock-cut chamber with pillars and benches (‘Petit Grotte’)

A rock-cut chamber is situated in the northern face of the southernmost cliffs of the cirque (; for location, see number 1 in ) and is referred to as the ‘Petite Grotte’ by Ginther and Hébert (Citation1963). The chamber entrance at the foot of the cliff is approximately 140 cm wide and 100 cm high. The present-day chamber floor is covered by a thick layer of quartz grains. The maximum height of the chamber is about 120 cm and its surface area is approximately 15 m2. It contains several pillars and benches carved into the rock (see the drawing in ), that are partially heavily eroded. Three large pillars in the central part of the chamber are aligned parallel to the cliff face. One is now broken, with the upper part still attached to the ceiling and the lower part missing. All three pillars narrow downward, with the two main pillars still standing having a diameter of about 120 cm at the ceiling and 50 cm some 60 cm above the chamber’s floor. From hereon down, the diameter remains approximately the same. Benches on three sides of the chamber have been carved into the rock about 50–60 cm above the floor. These benches are about 40 cm wide and have a series of small pillars on them that are some 60 cm in height, narrowing downward, from ∼60–70 cm at the ceiling to ∼30 cm at the top of the bench.

Figure 6. Teniky: the rock-cut chamber: a) panoramic photograph as viewed from the entrance with a 40-cm-long scale bar; b and c) photographs taken within the chamber showing benches and the central pillar; d) horizontal section through the chamber; e) vertical section through the large pillar in the centre; f) vertical section through a small pillar on the bench. Images d–f have been redrawn and modified after Paulian and Dommergues (Citation1950). Note that the left-hand large pillar drawn in (d) has since broken and its remains are only visible near the ceiling.

Figure 6. Teniky: the rock-cut chamber: a) panoramic photograph as viewed from the entrance with a 40-cm-long scale bar; b and c) photographs taken within the chamber showing benches and the central pillar; d) horizontal section through the chamber; e) vertical section through the large pillar in the centre; f) vertical section through a small pillar on the bench. Images d–f have been redrawn and modified after Paulian and Dommergues (Citation1950). Note that the left-hand large pillar drawn in (d) has since broken and its remains are only visible near the ceiling.

Rock-cut niches with semi-circular openings

About 150 m east-northeast of the Petit Grotte a series of six niches has been cut in the cliffs about 120 cm above ground level (; for location see number 2 in ). Two of the niches have been partially eroded and are now connected into a single opening. The spacing between the centres of individual niches is about one metre. The niches are near-circular with a nearly flat base parallel to the ground level. As a result, the divisions between adjacent niches display an upward-widening pillar shape when viewed frontally. The niches are about 50–60 cm wide at the base and 40-50 cm high, with a depth of about 50 cm. Several niches are connected inside through a roughly circular hole cut into the dividing wall. About two metres away from these niches, a single, circular rock-cut niche with a diameter of approximately 25 cm and a depth of around 40 cm occurs at a slightly higher level (see the righthand side of a).

Figure 7. Teniky: rock-cut niches: a) panoramic view of rock-cut niches and a single cylindrical rock-cut niche slightly higher to the right; b and c) detailed views. The scale bar is 40 cm long.

Figure 7. Teniky: rock-cut niches: a) panoramic view of rock-cut niches and a single cylindrical rock-cut niche slightly higher to the right; b and c) detailed views. The scale bar is 40 cm long.

A series of five circular rock-cut niches with recesses

Just south of the Grande Grotte (see below) a series of circular openings is cut in the cliff wall about one metre above the ground surface (; for location, see number 3 in ). Their diameter is ∼35 cm and their depth about 50 cm (a). Some of the niches are heavily eroded and two adjacent openings have merged into a single opening (b). A recess or circular notch is still preserved around the openings, suggesting that they could be closed off with a stone or wooden slab.

Figure 8. Teniky: circular niches with a recess around the opening. Note that erosion has resulted in merging of two adjacent niches in the photograph on the left. The scale bar is 40 cm long.

Figure 8. Teniky: circular niches with a recess around the opening. Note that erosion has resulted in merging of two adjacent niches in the photograph on the left. The scale bar is 40 cm long.

Rock shelter delimited by sandstone walls (Grande Grotte)

A large rock shelter, situated at 22°18’05.4’’S, 045°18’35.9’’E, is referred to by Ginther and Hébert (Citation1963) as the Grande Grotte (for location, see number 4 in ). The rock shelter is delimited by two parallel stone walls consisting of sandstone blocks, which have been carefully squared and stacked without the use of mortar (). The photographs taken by Jacques Faublée, an ethnologist working in southern Madagascar in the early 1940s, show a better-preserved state of the wall ().

Figure 9. Teniky: remains of the inner wall at the rock shelter with an opening in the centre of the photograph. The left part of the wall has partially collapsed.

Figure 9. Teniky: remains of the inner wall at the rock shelter with an opening in the centre of the photograph. The left part of the wall has partially collapsed.

The inner wall contains an opening, probably representing an entrance to the rock shelter (). Bevelled blocks are visible on either side of the opening at the base (a and b) and on one side about 150 cm above ground level, suggesting that the entrance might once have held some kind of closure. The initial dimensions of the inner wall closing off the rock shelter are approximately 15 m long, up to 3 m high and 70 cm wide. The carved sandstone blocks vary between 40 and 75 cm in length and are around 20 cm wide and 10 cm high. Almost every sandstone block bears traces of graffiti, mostly names and dates scratched into the sandstone blocks, with dates going back to the late nineteenth century.

Figure 10. Teniky: the rock shelter: a and b) details of the inner wall showing bevelled sandstone blocks at the base of the entrance. The scale bar in (a) is 40 cm long. Note the deterioration of the sandstone blocks when comparing these photographs with those taken by the French ethnologist Faublée (see ). Graffiti in (b) bear the year 1900; c) remains of the weathered outer wall at the rock shelter with a 30-cm-long scale bar; d) niche in rock shelter with a bench about 40 cm above the ground. The scale bar here is 40 cm long.

Figure 10. Teniky: the rock shelter: a and b) details of the inner wall showing bevelled sandstone blocks at the base of the entrance. The scale bar in (a) is 40 cm long. Note the deterioration of the sandstone blocks when comparing these photographs with those taken by the French ethnologist Faublée (see Figure 3). Graffiti in (b) bear the year 1900; c) remains of the weathered outer wall at the rock shelter with a 30-cm-long scale bar; d) niche in rock shelter with a bench about 40 cm above the ground. The scale bar here is 40 cm long.

Parallel to the inner wall are the remnants of a similarly constructed sandstone wall around eight metres away. This outer wall has a width of about 80 cm, while its maximum height above ground level is about 120 cm (c). As the outer wall is exposed to rain and wind, the weathered surface is much darker than the inner wall, which is protected from the elements by the rock overhang. Scratching the weathered surface of the blocks of the outer wall reveals the same light colour as the blocks from the inner wall. The construction style of the inner and outer walls at the Grande Grotte is unique within Madagascar and is also unknown on the East African coast. The sandstone blocks of the walls were most likely sourced from the quarries discovered in Zones 4 and 5, east and west of the Sahanafo River (), that we discuss further below.

The ground level of the rock shelter, limited by the inner wall, covers a surface area of about 15 × 15 m and the shelter has a maximum height of approximately six metres. A niche has been cut in the northern part of the rock shelter (d). It is about 1.2 m wide at the entrance, 1.5 m deep and 1 m high. The niche has a bench set about 30 cm above ground level with a maximum width of about 30 cm. Recesses are carved into the rock at the niche's entrance, with the shape and position of the recesses suggesting that the niche could be closed off.

Small circular rock-cut niches

Other man-made structures at Teniky include a series of approximately 35 circular niches cut in the sandstone cliffs over a horizontal distance of about 40 metres (; for location see number 5 in ). The niches are circular with a diameter of ∼20–25 cm and they are around 40 cm deep. The spacing between the niches is irregular and some have been almost completely eroded, with just a small depression left in the cliff wall. Some niches are up to 3–4 metres above present-day ground level. Inspection of the niches revealed that they do not contain any artefacts. The bases of the niches are covered by a layer of quartz grains eroded from the hole’s ceiling that is several centimetres thick. Birds of prey have made their nests in a few of the niches.

Figure 11. Teniky: a series of 35 circular rock-cut niches.

Figure 11. Teniky: a series of 35 circular rock-cut niches.

Rectangular rock-cut niches with carved, vertical separations

About 200 m northwest of the major rock shelter, ten rock-cut niches are carved in the cliff face (; for location, see number 6 in ) adjacent to a major terrace. The base of the niches is approximately 50 cm above ground level. They have a rectangular opening that is about 120 cm high and 80 cm wide and are about 80 cm deep (a and b). Vertical walls with pillar-like shapes in frontal view separate the niches. Several vertical walls between adjacent niches have circular depressions or openings carved into them, while other vertical walls are heavily eroded with frontal parts partially missing (b). Some layers have preserved evidence of tool marks (c and d).

Figure 12. Teniky: images of the niches: a–b) quadrangular rock-cut niches; c–d) the presence of tool marks in the niches. These are absent in the underlying brown-reddish layer in (d), which is friable and erodes more easily.

Figure 12. Teniky: images of the niches: a–b) quadrangular rock-cut niches; c–d) the presence of tool marks in the niches. These are absent in the underlying brown-reddish layer in (d), which is friable and erodes more easily.

Series of four circular rock-cut niches

About 10 metres north of the rectangular rock niches just described, four circular rock-cut niches are present, about one metre above ground level (; for location, see number 7 in ). They are about 25 cm in diameter and 50 cm deep. A circular depression in the cliff wall at the same level, but 70 cm away from the southernmost niche, suggests the former presence of a fifth niche that has been heavily eroded. There are vague indications of former recesses around the holes, but it is difficult to make a definite statement in view of the heavily eroded rims of the holes.

Figure 13. Teniky: a series of four circular rock-cut niches, with a possible fifth, heavily eroded niche on the far right partially visible.

Figure 13. Teniky: a series of four circular rock-cut niches, with a possible fifth, heavily eroded niche on the far right partially visible.

Aligned stone slabs on a terrace with carved conglomerate blocks

A terrace in the northern part of the cirque (for location, see number 8 in ), covering an area of about 65 × 12 metres, contains aligned carved sandstone blocks placed in the ground, with the upper side of the blocks at ground level having a width of some 15 cm with the individual length of blocks varying between 30 and 65 cm. The longest dimension of the structure is oriented parallel to the cliff wall and extends for 8 m. Perpendicular to each end, aligned sandstone blocks extend over a total distance of about 2.5 m towards the cliff wall. On the inner side of the aligned blocks, a carved conglomerate block was found with dimensions of approximately 65 × 65 cm and a height of about 35 cm (). The block has rectangular recesses carved into three vertical sides and a slight roughly square depression at the top and possibly represents a basin used to hold water or fire.

Figure 14. Teniky: carved block on the terrace. The block has a square top surface containing a roughly square depression.

Figure 14. Teniky: carved block on the terrace. The block has a square top surface containing a roughly square depression.

A series of six rectangular rock-cut niches

At the base of the cliff further to the north, a series of five rectangular niches approximately 100 cm wide, 50–60 cm high and 30 cm deep have been cut in the rock face (; for location see number 9 in ). The back wall of the niches is irregular, suggesting that they were left unfinished.

Figure 15. Teniky: Rock-cut niches at the foot of the cliff.

Figure 15. Teniky: Rock-cut niches at the foot of the cliff.

Rock-cut conglomerate boulders

Further examples of rock-cut architecture are found on the slopes below the cliffs at Teniky (; for location, see number 10 in ), where two large conglomerate boulders have been worked. Both are heavily eroded. The first has a rectangular base (∼90 × 140 cm) and is about 1 m high, with a stepped base on one side and a slightly gabled roof (a and b). Each of the four sides has two square openings with recesses, suggesting that the openings could be closed off. The interior of the boulder has been hollowed out with a flat base. At one corner, erosion has resulted in the merging of two openings. The second boulder has roughly the same shape and dimensions as the first one and has also been hollowed out (c and d). In contrast to the first boulder, it has a pillar-shaped support in the interior (d), which resembles the pillars in the rock-cut chamber (i.e. the Petit Grotte). At first sight, it might be tempting to consider the carved boulders as architectural models used to plan the construction of the rock-cut chamber at the Petit Grotte (Ginther and Hébert Citation1963), but in view of the considerable amount of effort that must have gone into carving the boulders and the presence of recesses around the openings we consider this unlikely and suggest instead that it served a ritual function.

Figure 16. Teniky: two heavily eroded worked rock boulders: a–b) the first rock-cut boulder with a slightly gabled roof and square openings with recesses; c–d) the second rock-cut boulder with a gabled roof and a pillar-shaped structure in the interior. Both scale bars are 40 cm long.

Figure 16. Teniky: two heavily eroded worked rock boulders: a–b) the first rock-cut boulder with a slightly gabled roof and square openings with recesses; c–d) the second rock-cut boulder with a gabled roof and a pillar-shaped structure in the interior. Both scale bars are 40 cm long.

Excavations at the rock shelter in Zone 1

In late 2022 we carried out excavations at the rock shelter in Zone 1 discovered the year before (). The shelter is curved in plan view and eight quadrangular niches (N1–8) have been cut in the cliff wall (b). A ninth niche (N9), with a near-circular opening, is located a few metres away, towards the west (inset in b). In addition to the niches, we found further archaeological structures at the foot of the rock shelter, including (i) two sandstone walls (W1 and W2) in the northeast part; (ii) an area of approximately 4 × 3 m in front of the sandstone walls, partly outlined by rock slabs placed vertically in the ground (ST14; c); and (iii) a stone basin (ST18) about 3 m away from the cliff, close to the rock-cut niches N2-N8 in the southwestern part of the rock overhang.

Figure 17. Teniky: aerial views taken during excavations at the rock shelter in Zone 1: a) location of the rock shelter on the western flank of the north-south trending hill with dense vegetation masking the site having been removed; b) view of the excavations with eight niches visible (N1N8). The inset in (b) shows the ninth, nearly circular niche (N9) some 6 m away from N8; c) view of the northeastern part of the rock shelter showing niche N1, sandstone walls W1 and W2 and structure ST14, which is partially outlined by vertical rock slabs. Numbers preceded by SD indicate the location of trenches.

Figure 17. Teniky: aerial views taken during excavations at the rock shelter in Zone 1: a) location of the rock shelter on the western flank of the north-south trending hill with dense vegetation masking the site having been removed; b) view of the excavations with eight niches visible (N1–N8). The inset in (b) shows the ninth, nearly circular niche (N9) some 6 m away from N8; c) view of the northeastern part of the rock shelter showing niche N1, sandstone walls W1 and W2 and structure ST14, which is partially outlined by vertical rock slabs. Numbers preceded by SD indicate the location of trenches.

After clearing the site of dense vegetation, excavations were undertaken close to the niches. We started with trenches in front of niche N1, where most structures seemed to be concentrated: SD001 (surface area: ∼3 × 2 m), SD002 (6 × 1.5 m), SD003 (1 × 1 m) and SD004 (3.5 × 2.5 m). In the areas covered by SD001 and SD002, we dug two deeper trenches, SD009 and SD008, to investigate the stratigraphy at a larger depth. In front of niches N2-N8, we dug two small trenches: SD005 (2 × 1.5 m) and SD007 (1 × 1.5 m).

Rock-cut niche with bench (N1) in the northeastern part of the rock shelter

The main niche N1 at the rock shelter is slightly curved with a length of about 5.5 m and a height of 1–1.2 m (). The niche is strongly eroded and has three pillars against the back wall. The outlines of at least three further pillars in the frontal part of the niche are still visible on the ceiling. Due to erosion, no tool marks are visible. The first two pillars (P1 and P2) are almost identical in size (approximately 0.75 m high and 0.30 m wide). Each of the pillars has a quadrangular shape flaring in its upper section. The third pillar (P3) differs from the other two. One of its faces seems to have not been cut but instead left straight, giving it a more massive, rougher appearance than the other two. The pillar has a width of 0.67 m at the base and widens upwards to 0.8 m. The morphology of P3 and the adjacent space E4, which stand out from the remaining structures at the niche, suggest that there may have been two construction phases. During the first phase, possibly only a quadrangular niche, occupying space E4, was cut. During the second phase, the adjacent part of the rock-cut structure, including the pillars, was shaped. The E4 niche was redesigned to fit into the space, with pillar P3 being roughly cut into the wall of the old niche ().

Figure 18. Teniky: rock-cut niche N1 with bench: a) the frontal view of the niche shows the bench and the three pillars (P1, P2 and P3) set at the back wit ha 50 cm scale bar; b) plan view of the niche with the location of structures ST4 and ST16 indicated. E4 is the space between P3 and the southern limit of the niche.

Figure 18. Teniky: rock-cut niche N1 with bench: a) the frontal view of the niche shows the bench and the three pillars (P1, P2 and P3) set at the back wit ha 50 cm scale bar; b) plan view of the niche with the location of structures ST4 and ST16 indicated. E4 is the space between P3 and the southern limit of the niche.

The bench of niche N1 was covered with a thick layer of sandstone grains and angular blocks. Two structures, ST16 and ST4, were identified on the bench. ST16 is an elongated, 1.5-m-long structure between pillars P1 and P2, characterised by flat stones (). At its southern end, the structure nearly joins pillar P2, whereas at its northern end there is an approximately 0.5-m-long gap between it and pillar P1. The structure consists of a large squared sandstone block (0.80 × 0.20 × 0.10 m) with smaller sandstone blocks on either side. The dimensions of the largest block, which is heavily eroded, suggest that it comes from either wall W1 or W2 (see below) and was moved to this location. Structure ST4 consists of a pile of stones in no particular arrangement located in the northern corner of the bench (b). Most stones are flat and rectangular (0.25 × 0.35 × 0.10 m). They could be stones that belonged to structure ST16 and were moved for an undetermined reason.

Sandstone walls in front of niche N1

Two sandstone walls (W1 and W2) are present in front of niche N1 (). Both walls are made up of squared sandstone blocks (∼0.9 × 0.25 × 0.10 m), with segments of each wall already visible before the onset of excavations. No foundation trenches were found for either of the two walls. They appear erected on sight, with the foundations resting directly on the ground. The presence of a large number of sandstone blocks on the slope bears witness to the demolishment of the walls (a and b).

Figure 19. Teniky: structures in the northeastern part of the rock shelter at the end of the excavations: ab) aerial views showing walls W1 and W2, as well as structures ST23 and ST27; c) plan view drawing of walls W1 and W2, as well as structures ST23 and ST27, before the digging of trenches SD008 and SD009. The locations of trenches SD001, SD002 and SD003 are indicated. The sandstone blocks on the slope in front of the stone walls (visible in the photographs) result from their demolition and are not drawn in (c).

Figure 19. Teniky: structures in the northeastern part of the rock shelter at the end of the excavations: a–b) aerial views showing walls W1 and W2, as well as structures ST23 and ST27; c) plan view drawing of walls W1 and W2, as well as structures ST23 and ST27, before the digging of trenches SD008 and SD009. The locations of trenches SD001, SD002 and SD003 are indicated. The sandstone blocks on the slope in front of the stone walls (visible in the photographs) result from their demolition and are not drawn in (c).

Wall W1 roughly follows the curved rock overhang with a total length of about 13.5 metres. It has a short (∼4.5 m) north-northwest/south-southeast section and a long (∼9.0 m) northeast/southwest one. Wall W2 is 2.5 m long, trends perpendicular to the long section of wall W1 () and is positioned close to the change in orientation of wall W1. The long section of wall W1 has a maximum width of approximately 1.10 m near its southwestern end. The number of layers of sandstone blocks making up wall W1 varies depending on the underlying topography. Three to four layers of sandstone blocks are visible in places, giving the wall a maximum height of about 0.5 to 0.6 m. Some of the visible blocks are more eroded than others. Most of the blocks in the long northeast-southwest section of wall W1 are laid out perpendicular to the slope of the terrain. The blocks have slid slightly downslope near the limit with wall W2, resulting in a gap between the two walls. The short north-northwest/south-southeast section of W1 is partially built on a large boulder and consists of blocks mostly laid parallel to the slope of the terrain. The top layer of this section is very smooth, suggesting that it probably represents the initial upper limit of the wall, which must have been around 0.55 m high. Excavation SD003 did not reveal a continuation of wall W1 (c), which ends at the location indicated in c. Structure ST23 near the southwestern end of wall W1 (b and c) has a length of 2.70 m and a width of 1.10 m and comprises large, fairly well-preserved sandstone blocks of the same size and material as those in the walls. They are arranged in two levels, giving the impression of a stairway or entrance (b, b).

Excavation SD002 comprises a rectangular area measuring approximately 1.40 × 6.00 m. It was positioned along wall W1 to document its facing and stratigraphic insertion. The stratigraphy along the south-eastern edge of the excavation is — from top to bottom — first characterised by a succession of very fine, light-coloured sandy layers (UT17 and UT51; ). This is an accumulation of humus, quartz grains and debris eroded from the roof and walls of the rock shelter. Interspersed is a thin layer composed mainly of ash and charcoal flakes (UT49) and another layer showing traces of fire, probably a natural fire because of the presence of burnt roots. Beneath these layers, two layers of silty sand, one beige-grey (UT21) and the other ochre-red (UT24), probably correspond to a walking level. They correspond to the upper level of the sandstone blocks, making up structure ST23 and could therefore be anthropogenic. Two undated ceramic sherds were found in layer UT24. Beneath layers UT21 and UT24, a very compact, grey-white, sandy-silt layer (UT38) appeared, similar to layer UT30 (see ). Layer UT38 probably formed due to partial demolition and erosion of wall W1. Beneath this layer, a succession of rather loose, orangey-beige, sandy layers (UT37, UT52 and UT53) were identified in trench SD008. These appear to be natural soil layers on which wall W1 was built.

Figure 20. Teniky: stratigraphic sections of selected excavations at the rock overhang in Zone 1 with the location of two dated charcoal samples, PLV2–2 and PLV8, indicated in (d).

Figure 20. Teniky: stratigraphic sections of selected excavations at the rock overhang in Zone 1 with the location of two dated charcoal samples, PLV2–2 and PLV8, indicated in (d).

Wall W2 is perpendicular to the northeast-southwest section of W1. It has a maximum height of 0.6 m and a width of ∼0.8–1.0 m and extends from the rock overhang until wall W1. In the middle of wall W2, a nearly square flat surface (∼0.9 × 1.0 m; structure ST27) comprises rectangular sandstone blocks (0.9 × 0.2 × 0.1 m), which have their long dimension parallel to the trend of wall W2. The blocks’ flat appearance and alignment suggest that ST27 represents a threshold that provided access to a space in front of niche N1, delimited by walls W1 and W2. Eroded and angular sandstone blocks (∼0.6 × 0.2 m) in random, tilted positions were found at depth on either side of wall W2 and are considered to result from its destruction. Excavation SD001 measures approximately 1.40 × 1.80 m and was positioned on either side of wall W2 to document its facing and stratigraphic insertion. The stratigraphy southwest of wall W2 is similar to that observed in SD002, but is quite different on the northeastern side. Northeast of wall W2, a succession of very fine sandy layers (UT46, UT45 and UT44) was first excavated. This is an accumulation of humus, dust and quartz grains eroded from the ceiling and walls of the shelter. These layers were followed by a much more compact, orange, sandy layer (UT20). This could be a floor or walking level at the same height as the interpreted threshold (ST 27). Below this, a very compact, white, sandy layer (UT30) was uncovered, which is interpreted as a man-made layer consisting of demolished sandstone blocks mixed with sand to stabilise and level the ground. Beneath this white sandy layer (UT30) lies a compact, brown, sandy loam (UT31) with charcoal flakes and unidentified animal bones. No traces of man-made cuts were observed on the bones. It is not clear whether the charcoal flakes originate from a man-made or natural fire. The brown, sandy layer could have become compacted during the construction of the niches and sandstone walls. Beneath this layer, a succession of rather loose, orangey-beige, sandy layers (UT43, UT42, UT41 and UT40) was identified. These appear to be natural soil layers on top of which the man-made features were constructed. Toppled blocks resulting from the partial demolition of wall W2 have fallen onto the walking level on either side (UT28 and UT29; ). On the southestern side of wall W2, the walking level onto which the blocks fell is lower than on the northeastern side. The difference in height of the walking level and the difference in stratigraphy on either side of wall W2 suggest there may have been an interior part (northeast of wall W2) and an exterior part (southwest of wall W2) or at least two spaces used differently. Structure ST27 is possibly the threshold of the entrance to the slightly raised area (delimited by walls W1 and W2), positioned directly in front of niche N1.

Figure 21. Teniky: structure ST27 a) showing the central part of wall W2. Note that the walking level is at different heights on either side of wall W2, being lower on the right (southwestern part). In the upper left of the photograph, part of niche N1 is visible; b) Structure ST23 is a possible stairway or entrance near the southwestern limit of wall W1. The scale bar is 50 cm.

Figure 21. Teniky: structure ST27 a) showing the central part of wall W2. Note that the walking level is at different heights on either side of wall W2, being lower on the right (southwestern part). In the upper left of the photograph, part of niche N1 is visible; b) Structure ST23 is a possible stairway or entrance near the southwestern limit of wall W1. The scale bar is 50 cm.

Structures ST14 and ST18

ST14 is a nearly rectangular structure, around 2.80 m wide and 3.60 m long (). Its southwestern and southeastern sides are partially bounded by a dozen flat stones placed vertically in the ground. Most likely, some of the stones have disappeared due to erosion, notably along the structure’s northwestern and northeastern sides. In between this structure and wall W1, two fragments of a stone basin were found. During excavation SD004, the humus at ST14 was removed and the natural, sterile ground came directly into view. The stones therefore appear to have been planted directly into the latter.

Figure 22. Teniky: structure ST 14 and excavation SD 004: a) photograph of structure ST14 at the onset of the excavations looking northwest. The scale bar is 50 cm; b) map of excavation SD004 with the position of the flat stones placed vertically into the ground.

Figure 22. Teniky: structure ST 14 and excavation SD 004: a) photograph of structure ST14 at the onset of the excavations looking northwest. The scale bar is 50 cm; b) map of excavation SD004 with the position of the flat stones placed vertically into the ground.

Structure ST18 is a single, carved conglomerate block (0.48 × 0.56 m and 0.3 m high) with a central, rectangular depression (0.26 × 0.34 m; ). The block shows a break in the middle and two of the feet are damaged. Its shape suggests that it is some kind of basin placed directly on the ground. Its prominent position close to the rock-cut niches N2 to N8 suggests that it might have held water or fire for use in ritual ceremonies.

Figure 23. Teniky: basin ST18 in front of the niches N2N8. Note the circular niche N9 in the far background. The scale bar is 30 cm.

Figure 23. Teniky: basin ST18 in front of the niches N2–N8. Note the circular niche N9 in the far background. The scale bar is 30 cm.

Rock-cut niches N2 to N9 in the southwestern part of the rock shelter

Seven rectangular niches (N2–N8) and a circular niche (N9) are visible in the southwestern part of the rock shelter (b and ). The rectangular niches all have a bench with a base that is approximately 0.5–1.0 m above the ground. Niches N2 and N3 are badly eroded, and their original size seems smaller than niches N4 to N8. The latter niches have dimensions of 0.9 × 0.7 × 1.4 m. Their ceilings and bottoms are fairly flat, their walls nearly vertical and their angles almost right (i.e. 90°). No traces of tools have been observed, most probably due to the effects of subsequent erosion. All the niches were excavated but they contained only an accumulation of several centimetres of sediment resulting from the erosion of the walls and ceiling.

Figure 24. Teniky: photograph of rock-cut niches N2–N8 at the rock shelter in Zone 1 with a stone basin (ST18) in the foreground.

Figure 24. Teniky: photograph of rock-cut niches N2–N8 at the rock shelter in Zone 1 with a stone basin (ST18) in the foreground.

Niche N9 is a roughly circular niche (0.5 × 0.7 × 1.0 m) cut into the rock face a few metres away from niches N2–N8 (inset in b). Its inner walls are quite eroded with no visible tool marks while its bottom is rather flat. The niche was filled with quartz grains and conglomerate debris eroded from the ceiling. No artefacts were encountered during its excavation. Grooves are visible along the margins of the inner rim of the niche, suggesting that the opening could be closed off.

Dating of structures

We attempted to date niche N1 using optically stimulated luminescence (OSL). In the dark, we removed the thick sandy layer covering the bench and scratched quartz grains from the bench itself. Unfortunately, the OSL signal from the quartz grains proved too weak. Radiocarbon dating using accelerator mass spectrometry (AMS) turned out to be more revealing. Four small pieces of charcoal found during our excavations at the rock shelter were dated at the Laboratory for the Analysis of Radiocarbon with AMS (LARA) of the University of Bern (Szidat et al. Citation2014), giving uncalibrated ages of between 986 ± 22 (BE-19991.1.1) and 1161 ± 22 BP (BE-19989.1.1; ). The ages were calibrated with OxCal 4.4 (Bronk Ramsey, Citation2009) using the southern hemisphere calibration curve SHCal20 (Hogg et al. Citation2020). Although the composition of the charcoal has not been determined and the small charcoal pieces are potentially relatively mobile, there is a certain homogeneity in the results of the radiocarbon dates. Calibrated ages fall in the range cal. AD 891–1155, i.e. between the end of the ninth century and the middle of the twelfth century AD ().

Figure 25. Teniky: calibrated radiocarbon ages (cal. AD) using OxCal 4.4 and southern hemisphere calibration curve SHCal20 (Bronk Ramsey Citation2009; Hogg et al. Citation2020).

Figure 25. Teniky: calibrated radiocarbon ages (cal. AD) using OxCal 4.4 and southern hemisphere calibration curve SHCal20 (Bronk Ramsey Citation2009; Hogg et al. Citation2020).

Table 1. Teniky: radiocarbon determinations.

Three charcoal samples, PLV2-2, PLV3 and PLV8, were taken in different stratigraphic positions during excavation at walls W1 and W2 (SD001, and ). Sample PLV8 comes from the stratigraphically lowest position; it was taken from a homogeneously compacted layer (UT31) interpreted as a walking level used during the construction of wall W2 (). Its radiocarbon age lies in the range cal. AD 1021–1150. Layer UT31 is stratigraphically overlain by Layer UT30, which is interpreted as a fill on top of which a compacted layer (UT20) is observed. Layer UT20 abuts wall W2 and is at the same height as the top of the uncovered sandstone blocks (ST27), with the latter probably representing the threshold of an entrance. Layer UT20 is thus inferred to have been a walking level, which formed after the construction of wall W2 and during the use of the space confined by walls W1 and W2. Sample PLV2-2 comes from this layer and its radiocarbon age falls in the range cal. AD 991–1138. Sample PLV3 occupies the highest stratigraphic position as it was found directly on top of one of the sandstone blocks making up structure ST27, which was completely uncovered during the excavation. Its radiocarbon age lies in the range cal. AD 891–990.

Figure 26. Teniky: plan view of SD001 before the excavation of trench SD009 showing wall W2 with structure ST27, part of wall W1 and the position of charcoal samples PLV2–2, PLV3 and PLV8 with calibrated ages given.

Figure 26. Teniky: plan view of SD001 before the excavation of trench SD009 showing wall W2 with structure ST27, part of wall W1 and the position of charcoal samples PLV2–2, PLV3 and PLV8 with calibrated ages given.

Although all three radiocarbon ages fall within a relatively narrow time span between cal. AD 891 and cal. AD 1150, there is a slight age inversion, with the oldest age coming from the charcoal sample in the highest stratigraphic position. This is not surprising, as the problem with dating charcoal is that it is difficult to know exactly what is being dated. Depending on the tree species and the position of the charcoal on the tree trunk (the ‘old wood effect’), radiocarbon ages can vary considerably. In addition, small charcoal fragments are highly mobile and it is difficult to determine whether the dated charcoal comes from a layer that was disturbed during human activity (e.g. construction of the wall or levelling of the terrain) and brought into a different stratigraphic position or whether it was displaced by the wind. A fourth charcoal sample, PLV9 was taken during excavation SD007, located approximately three metres from niche N2. The excavation revealed a linear structure (ST55) at a depth of about 40 cm. This structure is approximately 80 cm long and has four aligned angular rock slabs. The nature of this man-made structure is difficult to interpret due to the limited extent of the excavation. The charcoal sample was taken at the level of the aligned rock slabs and its radiocarbon age lies in the range cal. AD 1030–1155.

Despite the inherent uncertainty of radiocarbon determinations run on charcoal the fact that all four ages are relatively closely grouped together and are linked to human activity at the rock shelter suggests that the construction of the stone walls dates back to the late tenth to mid-twelfth centuries AD. While removing the upper soil during excavation of structure ST14 in Zone 1 (SD004; ), a single ceramic sherd was found (a), identified as being of Southeast Asian origin and dated to the eleventh to thirteenth centuries AD (Bing Zhao, pers. comm.) This age interval corresponds closely to the one obtained by radiocarbon dating. In summary, the available radiocarbon ages and the age of the ceramic sherd suggest that the rock-cut structures and the sandstone walls at the rock shelter in Zone 1 date to the late first/early second millennia AD.

Surface prospecting

In addition to the excavations in Zone 1, we carried out surface prospecting in the Sahanafo Valley and on the hills on either side of it to obtain a first inventory of the wider archaeological landscape. Satellite images were of great help in guiding our surface prospecting.

Zone 2

Zone 2 comprises a north-south trending hill around 1500 m long and about 500 m wide near its southern end ( and ). It is a striking landscape feature with the highest point on the hill crest nearly 200 metres above the valley floor. On its flanks and ridges are numerous terraces with dry stone walls bordering some of them (). These structures are visible on satellite images and were identified on the ground. In the northernmost part of the hill, terraces occupy an area of about 10 ha (a). Taken together with the 20 hectares of terraces at the cirque (Zone 8), this suggests that the site of Teniky was of considerable size and importance. At the hill’s highest point, a rectangular structure consisting of dry stone walls contains a raised inner part, like a platform, measuring 45 × 16 m (d). The width of the stone wall is about 60–70 cm and its maximum present-day height about 0.5–0.6 m. Several eroded blocks of cut sandstone, found near the southernmost limit of the platform, can be reassembled into a structure with feet resembling a small square table or basin that measures about 35 × 35 cm and is about 20 cm high. The position of this hill in the landscape, correlated with the type of structures observed on the summit, suggests that this place was occupied during occasional, ritual activities.

Figure 27. Teniky: archaeological structures in Zone 2 include terraces, stone walls, a major platform, rock-cut niches (Zone 1) and a possible path. The location of the images is given in . The scale bar is approximate. Satellite images: Google Earth 7.3.6.9345 (2 February 2010). Madagascar: a) 22°17’46.24”S, 45°17’17.67’’E; b) 22°17’56.27”S, 45°17’10.81’’E; c) 22°18’07.16”S, 45°17’10.56’’E; d) 22°18’27.91”S, 45°17’11.29’’E, Eye alt 445 m. Maxar Technologies 2023. www.earth.google.com (20 December 2023).

Figure 27. Teniky: archaeological structures in Zone 2 include terraces, stone walls, a major platform, rock-cut niches (Zone 1) and a possible path. The location of the images is given in Figure 4. The scale bar is approximate. Satellite images: Google Earth 7.3.6.9345 (2 February 2010). Madagascar: a) 22°17’46.24”S, 45°17’17.67’’E; b) 22°17’56.27”S, 45°17’10.81’’E; c) 22°18’07.16”S, 45°17’10.56’’E; d) 22°18’27.91”S, 45°17’11.29’’E, Eye alt 445 m. Maxar Technologies 2023. www.earth.google.com (20 December 2023).

Zone 3

Zone 3 is located in the valley east of the Sahanafo River, close to a densely forested area ( and ). An approximately 1-m-thick dry stone wall that is difficult to see through the trees and tall grass delimits an area of approximately 80 × 80 m (inset in ). Segments of dry-stone walling are also observable within the area enclosed by this wall. Two major linear features were observed on satellite images of Zone 3 (). Ground truthing in the field revealed that these are remains of dry, unhewn stone walls, the maximum height of which is about 1 m. One wall extends for about 120 m in the northern part of Zone 3, just south of a tributary to the Sahanafo River and trends west-northwest/east-southeast. Another much longer stone wall with a maximum height of about 1 m can be followed for about 750 m and runs north-northeast/south-southwest in the eastern part of Zone 3. Two circular stone structures were observed in the field in its northern part, a few metres west of the wall. These consist of circular dry stone walls with a diameter of about 1.5 m and a height of about 1.5 m. Ceramic sherds collected from the surface between the area with the square stone wall and the long linear stone wall include imported Chinese celadon and Southeast Asian stoneware dated between the eleventh and fourteenth centuries AD (; Bing Zhao, pers. comm.).

Figure 28. Teniky: stone walls in Zone 3. The stippled square in the inset traces the outline of a stone-walled enclosure in a forested area.

Figure 28. Teniky: stone walls in Zone 3. The stippled square in the inset traces the outline of a stone-walled enclosure in a forested area.

Figure 29. Teniky: Chinese and Southeast Asian ceramics: a) eleventh/thirteenth-century sherd found during excavation of structure ST14 in Zone 1 (SD004, b); b–c) twelfth-century sherds found during surface prospecting in Zone 3; (d–i): thirteenth/fourteenth-century sherds found during surface prospecting in Zone 3­­. The estimated ages of the ceramics are courtesy of Bing Zhao.

Figure 29. Teniky: Chinese and Southeast Asian ceramics: a) eleventh/thirteenth-century sherd found during excavation of structure ST14 in Zone 1 (SD004, Figure 22b); b–c) twelfth-century sherds found during surface prospecting in Zone 3; (d–i): thirteenth/fourteenth-century sherds found during surface prospecting in Zone 3­­. The estimated ages of the ceramics are courtesy of Bing Zhao.

Quarries (Zones 4 and 5)

Two sandstone quarries spaced around 500 m apart were discovered by our local guides in Zones 4 and 5, west and east of the Sahanafo River respectively ( and ). The dimensions of partially extracted blocks at these quarries are approximately 75–95 cm, whereas their width varies between 20 and 35 cm. Mineral composition and dimensions are similar to those of the sandstone blocks used to construct the walls at the rock shelters in Zone 1 () and Zone 8 ( and , Grande Grotte). The two quarries are roughly mid-distance between these two rock shelters. Given the characteristics of the stones and the short distance between quarries and stone walls (∼1.0–1.5 km), it is very likely that the stones extracted from these two quarries were used to build the sandstone walls at the rock shelters.

Figure 30. Teniky: Zone 4: a) aerial view of part of the quarry from which shrub and loose gravel were removed at the right; b) detail of a cleaned part of the quarry. The long dimension of the casts varies between ∼75 and 95 cm.

Figure 30. Teniky: Zone 4: a) aerial view of part of the quarry from which shrub and loose gravel were removed at the right; b) detail of a cleaned part of the quarry. The long dimension of the casts varies between ∼75 and 95 cm.

Circular structure in Zone 6

A nearly closed circular structure with a diameter of around 150 m was observed on satellite images in Zone 6 ( and ). Ground truthing revealed a discontinuous dry stone wall with a maximum height of some 80 cm, consisting of unhewn sandstone and conglomerate blocks approximately 30–50 cm in size. The wall is fully closed in its western part but has openings in the southern, eastern and northern parts that are 70 m, 50 m and 20 m wide, respectively. No clear signs of demolition, which could have explained the discontinuous nature of the wall, were observed on the ground. While the view to the south is clear, the slope of the terrain rises to the north, obscuring the horizon when facing north. The absence of a clear view in all directions, combined with the large diameter of the circular structure, makes it unlikely that it represents the remains of a former observation post. The absence of signs of demolition along the openings in the wall makes its interpreation as an animal enclosure implausible. Pending further research, the function of this imposing structure remains enigmatic.

Figure 31. Teniky: a nearly closed circular structure made up of a discontinuous stone wall: a) satellite image; b) photograph of part of the dry stone wall in the northern part of the structure.

Figure 31. Teniky: a nearly closed circular structure made up of a discontinuous stone wall: a) satellite image; b) photograph of part of the dry stone wall in the northern part of the structure.

Zone 7

Zone 7 is located approximately 600 metres north of the cirque () and includes a few terraces and dry stone walls on a small flat area measuring approximately 80 × 30 m. The site is slightly set back from a small rocky escarpment, the summit of which offers an excellent viewpoint, suggesting that it represents a former observation post.

Discussion

Our archaeological survey documents a rich archaeological landscape at Teniky covering an area much larger than previously known. Archaeological structures are found in the Sahanafo valley and on hills on either side, covering nearly 8 km2. New finds include rock-cut niches and stone walls at a rock shelter (Zone 1), where detailed excavations were carried out. Radiocarbon ages on charcoal indicate that the stone walls (W1 and W2) at the rock shelter were constructed close to the turn of the first and second millennia AD.

The walls at the rock shelter in Zone 1 are carefully constructed with squared sandstone blocks extracted from nearby quarries in the Sahanafo Valley. They delimit a slightly elevated space before a large rock-cut niche (N1) with a raised bench and carved pillar-like columns. Seven further rectangular niches (N2–N8) with a raised bench occur a few metres away. Considering their dimensions and the considerable effort that must have gone into building the walls and carving the niches (N1–N8), it seems unlikely that they served as storage rooms or dwellings but rather that they had a ritual function. A ninth smaller and nearly circular niche is slightly set apart from the rock shelter. Its small size and position, coupled with the presence of grooves around the inner rim of the opening indicating that it could be closed off, suggest that this niche probably had a different ritual function than the others. The morphology and character of a nearly square stone basin, a few metres away from the niches, suggest a symbolic, ritual use rather than a functional one. Although poorly preserved, aligned rock slabs were placed vertically in the ground directly in front of the stone walls, probably initially delimiting a small, roughly 10 m2 rectangular space that has since been partly eroded. Its spatial proximity to the rock shelter’s walls and niches suggests that the function of the space is directly related to the latter. Given the overall limited horizontal space in front of the rock shelter with a steep slope just below and the near complete absence of any material culture or structure indicating a domestic use (only one ceramic sherd was found), it is unlikely to represent a former living site. Instead, we consider it likely that the entire assemblage of structures observed at the rock shelter in Zone 1 was used for ritual activities.

The presence of a 40 × 15-m-large raised platform bordered by dry stone walls at the highest point of the north-south trending hill west of the Sahanafo Valley, and the find of a small sandstone basin within it, suggest that this site was probably also used for occasional, ritual activities, perhaps linked to those presumed to have taken place at the rock shelter in Zone 1.

Considering the dimensions, location and character of the archaeological structures in the cirque east of the Sahanafo Valley (Zone 8), we infer that most of the rock-cut structures there also had a ritual function. It is unlikely that the small rock-cut chamber (the Petite Grotte) with its beautifully carved pillars and benches represents a former storage room, while its small size and height of only 1.2 m makes it unsuitable to live in. Instead, it is more likely that the chamber had a ritual function. Most rock-cut niches in the cirque are considered to have had a ritual function, including the semi-circular and rectangular niches and the niche with a raised bench inside the rock shelter (the Grande Grotte). Rock-cut niches and rock-cut boulders with recesses around the openings may have had a different function than those without recesses. Furthermore, we note the presence of a terrace with a square stone basin and vertical sandstone slabs placed vertically in the ground. Its location immediately adjacent to the cliff wall with niches suggests that it could also have had a ritual use.

The sandstone blocks of the walls in Zone 1 are similar in size and composition to those used in constructing the sandstone walls delimiting the rock overhang at the Grande Grotte in the cirque (Zone 8). Although we have no absolute ages for the latter walls, it seems reasonable to assume that they are from the same period. Besides the radiocabron ages on charcoal from Zone 1 indicating a human presence approximately 1000 years ago, evidence for the former presence of an ancient population at Teniky is also provided by the finds of imported Chinese and Southeast Asian sherds dated to between the eleventh and fourteenth centuries AD (Bing Zhao, pers. comm.). Man-made terraces at Teniky cover a total area of approximately 30 hectares on the hills and ridges west and east of the Sahanafo River, suggesting that Teniky was a fair-sized settlement. Several terraces are directly at the foot of the cliffs, where rock-cut structures have been carved. The presence of large rock-cut boulders and stone basins on several terraces suggests that the levelling of the terraces was coeval with the carving of the rock-cut structures. Thus, in summary, we find evidence that most of the archaeological structures at Teniky, including the stone walls, quarries, terraces, niches, rock-cut boulders and stone basins, form part of a coherent archaeological assemblage made by a specific group of people who lived there about a 1000 years ago.

Teniky is a unique archaeological site in Madagascar as no similar rock-cut architecture is known from anywhere else on the island or from the adjacent East African coast. Given the limited excavations carried out so far and considering the relatively few pieces of ceramics found, we cannot yet say much about the duration of the human occupation at Teniky. We can, however, rule out the possibility that shipwrecked Portuguese sailors made the structures at Teniky in the sixteenth century as previously proposed because Portuguese ships did not sail the Indian Ocean until 1498. Although we did not find one single piece of evidence for a Portuguese presence, it is nevertheless still possible that Portuguese mariners stayed for some time at Teniky during an attempt to traverse the island.

The question thus arises as to who was responsible for the rock-cut architecture and terrace construction at Teniky, and why these people chose to live in such an isolated and secluded environment over 200 km from the nearest coast? The presence of early second-millennium Chinese and Southeast Asian ceramics indicates their participation in Indian Ocean trade networks, but does not give information on their origin. Does the entire assemblage of archaeological structures at Teniky warrant a first attempt at inferring the ethnicity and/or religious affiliation of those who once lived there?

Apart from the possible — but contested — early presence of foragers (Dewar et al. Citation2013; Douglass et al. 2019; Wright et al. Citation2022), archaeological excavations suggest that humans did not arrive on the island of Madagascar until the mid- to late first millennium AD (Anderson et al. Citation2018; Mitchell Citation2019, Citation2020, Citation2022). At some stage early migrants moved into the island’s interior and settled at Teniky in the tenth/eleventh centuries. Although it cannot be fully excluded that they developed their own unique culture and traditions after arriving on the island, the relatively short time interval between arrival on the coast and inland migration makes it more likely that they introduced their culture and traditions from elsewhere. In the following, we present a preliminary hypothesis on the origin and beliefs of the people who once lived at Teniky, but at the same time should like to clarify that our hypothesis must be validated or rejected based on further field studies.

When comparing the approximately 1000-year-old rock-cut niches at Teniky with similar structures elsewhere in the Indian Ocean, the closest stylistic parallels are found in Iran, where a multitude of archaeological sites show niches cut in steep rock walls dating to the first millennium AD or earlier (e.g. Grenet Citation1984; Boucharlat Citation1991; Cereti and Gondet Citation2015; Farjamirad Citation2015). Notably, in the Fars region in southern Iran hundreds of niches of different sizes and shapes have been cut in steep cliff walls, for example at the city of Siraf (). Siraf was a major and prosperous port on the Persian Gulf during the mid/late first millennium. Whitehouse (1971) considers that the port was already of importance in Sasanian times (i.e. before AD 656), although this has recently been questioned by Priestman (Citation2022). In any case, both authors agree that Siraf was an important port city in early Islamic times in the ninth and tenth centuries, with ships actively participating in the Indian Ocean trade network and sailing as far as India, Southeast Asia and East Africa (Whitehouse 1971; Whitehouse and Williamson Citation1973). Extensive archaeological excavations were carried out at Siraf by the British Institute of Persian Studies between 1966 and 1973 (Whitehouse Citation1968, Citation1969, Citation1970, 1971, Citation1972, Citation1974; Whitehouse et al. Citation2009) and, although these studies mostly focused on a Sasanian fort and Islamic monumental houses and buildings near the shore, cemeteries in the hills behind the city were also investigated (Whitehouse Citation1972, Citation1974; Whitehouse et al. Citation2009). Whitehouse mentions the presence of Islamic tombs on the southward-dipping slopes behind the city of Siraf, but also describes the presence of numerous niches (Whitehouse refers to them as ‘chambers’) cut in vertical cliff walls on the slopes and in steep gorges traversing the hills (). These niches are up to 2 m wide and 1.5 m high, sometimes including a rock-cut bench, and are considered by Whitehouse (1971, Citation1972) too small and inaccessible to have been dwellings. Several rock-cut niches contain a scatter of unburnt human bones and Whitehouse (1971, Citation1972) interprets these as tombs. Although single niches occur, several are usually closely grouped (e.g. a–e). Besides the large niches, Whitehouse (1971, Citation1972) also describes and illustrates smaller, rectangular niches (Whitehouse Citation1972: Plate Ia; f–i), sometimes set in a recessed panel retaining plaster, and interprets them as formerly closed-off ossuaries of a Zoroastrian community, intended to receive the bones of the deceased after exposure of the corpse.

Figure 32. Rock-cut niches in the hills immediately north of Siraf, Iran: a–e) larger rock-cut niches; f–i) smaller rock-cut niches. Note that the rock-cut niche on the right-hand side in (g) shows traces of plaster at its rims, whereas the niche in (i) has a recess. Drone images and photos courtesy of Ali Aghajanzadeh.

Figure 32. Rock-cut niches in the hills immediately north of Siraf, Iran: a–e) larger rock-cut niches; f–i) smaller rock-cut niches. Note that the rock-cut niche on the right-hand side in (g) shows traces of plaster at its rims, whereas the niche in (i) has a recess. Drone images and photos courtesy of Ali Aghajanzadeh.

Zoroastrianism is one of the oldest monotheistic religions in the world, practised without interruption to the present day, and was the dominant state religion of the Persian Sasanian Empire (AD 224–656). Zoroastrian funeral rites do not allow direct burial in the ground (Boyce Citation1979). Instead, corpses are left in places of display above the ground, generally called dakhmas in Pahlavi, often on hilltops or mountains, with excarnation of the corpses usually done by animals, such as dogs and vultures. After excarnation, the bones are dried and placed in ossuaries (bone receptacles, called astōdans in Pahlavi) to avoid polluting the earth. After the conquest of the Sasanian Empire by the Arabs in the mid-seventh century, Islam was imposed, but for a long time Zoroastrianism and other religions coexisted with it (Boyce Citation1979; Choksy 1987; Morony Citation2013). The gradual conversion of the majority of Persians to Islam occurred first in the cities and then in the countryside between the eighth and tenth centuries, with a peak in conversion in the ninth (Choksy 1987). However, Buzurg ibn Shahriyar (Citation1981) mentions that Zoroastrians still lived in the city of Siraf in the tenth century. The conversion of Persian Zoroastrians to Islam was, however, never fully accomplished and a small group of Zoroastrians still lives in Iran today. Historical documents, archaeological excavations and genetic studies indicate that some Zoroastrians left Iran and settled in western India in the late eighth century (Nanji and Dhalla Citation2008; Chaubey et al. Citation2017; Dalal and Mitra-Dalal Citation2021; Kumar et al. Citation2023), where they have become known as Parsis, i.e. the people of ‘Pars’ or ‘Fars’, their region of origin in southern Iran.

Notwithstanding the large variety in shape and size of the rock-cut niches in both Teniky and Siraf, the following similarities can be noted between the two sites: (i) larger niches are often closely aligned next to one another with a relatively narrow division between adjacent niches, giving rise to a pillar shape in frontal view; (ii) the openings of the larger niches are either rectangular or arched with a flat base; (iii) there is always a vertical distance between the base of the niche and the ground, i.e. none of the niches reach the ground; and (iv) some of the smaller rock-cut niches show recesses, suggesting that they could be closed. Apart from the stylistic resemblances of niches at Teniky and Siraf, the fact that at both places the openings in the cliffs never reach the ground is of importance, as this follows Zoroastrian funerary rites, according to which the exposed body must not touch the ground and must be protected from the natural elements to prevent pollution. Besides the abovementioned similarities, there are also differences: as far as we can tell from the literature, no nicely carved stone walls have been reported close to rock-cut niches in southern Iran and neither is there evidence for vertically placed slabs in the ground in front of the niches. However, this might be related to the fact that only limited archaeological research has been done on the niches at Siraf and other sites in southern Iran.

Despite the fact that no traces of human bones have yet been found in any of the niches at Teniky, we tentatively interpret the assemblage of rock-cut structures, stone walls and stone basins as part of a former necropolis the characteristics of which suggest a link to Zoroastrian funeral ceremonies. The large rectangular rock-cut niches may have been dakhmas where the bodies of the dead were exposed. The smaller, circular niches with recesses might then represent astōdans in which the bones of the dead were placed with the openings being closed off by a wooden or stone slab to protect them from the rain and thus prevent them from polluting the earth. The Petite Grotte and the large niche in the Grande Grotte are tentatively interpreted as chamber tombs, where bones stored in astōdans could have been placed on the raised benches along the sides. The two large worked rock boulders found on the slope of the cirque possibly represent larger sarcophagus-like astōdans used to dry or store bones. The openings on all four sides of the boulders have recesses, suggesting that these openings could have been closed in case of precipitation. Differences in the style, size and shape of the inferred astōdans might reflect differences in the social status of the dead.

It is not only the rock-cut architecture at Teniky that points to Zoroastrian rituals, but also the presence of stone basins and tables with rectangular or arc-shaped recesses and openings. These show stylistic similarities with the stone basins, tables and platforms used in Zoroastrian ritual ceremonies (Darmesteter Citation1892; Boyd and Kotwal Citation1983), for example to hold water or fire, both agents of ritual purity. Darmesteter (Citation1892) and Boyd and Kotwal (1893) describe and illustrate the Urvisgah (or Urwīsgāh), a part of the Zoroastrian fire temple complex, where liturgical ceremonies are performed. Plate IV in Darmesteter (Citation1892) shows the Urvisgah of the Maneckji Seth Fire Temple in Mumbai, which was constructed in the first half of the eighteenth century (). The plate shows low stone tables for holding utensils, square stone platforms for the priests to sit on cross-legged and slightly higher stone tables for holding a fire vase. In addition, the plate portrays a low square table with a circular depression, possibly for holding water used during purification ceremonies.

Figure 33. Place of worship in the temple of Manekji (or Maneckji) Seth in Mumbai, India (reproduced from Darmesteter Citation1892). Note the various square stone tables, platforms and basins.

Figure 33. Place of worship in the temple of Manekji (or Maneckji) Seth in Mumbai, India (reproduced from Darmesteter Citation1892). Note the various square stone tables, platforms and basins.

Only a few primary sources discuss the East African coast at the turn of the first and second millennia AD and even fewer make a reference to what is most probably the island of Madagascar. The latter include Buzurg Ibn Shahriyār, a tenth-century Persian sailor and writer, who collected narratives from sailors based in port towns on the Persian Gulf, including Siraf (Trimingham Citation1975; Buzurg Ibn Shahriyār Citation1981). His narratives suggest that Persian contacts with Madagascar existed in the mid-tenth century or earlier. Although Persian trade goods such as ceramics from southern Iran dating to the ninth to twelfth centuries have been found at archaeological sites in Madagascar, for example at Kingany (Anderson Citation2021), it remains difficult to infer a Persian presence from material culture only. The site of Teniky might represent an exception. If the rock-cut architecture and associated stone basins at Teniky are the work of a Zoroastrian community that settled in the Isalo Massif about a thousand years ago, this would strongly point to a former Persian presence in southern Madagascar.

At the moment we can only speculate as to when and where the group of people who ultimately moved to Teniky first landed on the coast of Madagascar and whether they also settled at other coastal or inland sites. The nearest potential first-millennium coastal site is Sarodrano on the shores of the Mozambique Channel, 200 km away from Teniky (). Here, excavations were undertaken in 1966 by Battistini and Vérin (1975) and a single radiocarbon date on charcoal (GAK-928) yielded an uncalibrated age of 1460 ± 90 BP, corresponding to cal. AD 418–841 using Oxcal 4.4 and SHCal20. Unfortunately, however, the site that yielded the date was destroyed by a tropical cyclone in 1970 (Battistini and Vérin 1975).

The inland sites of Asambalahy and Rezoky () are only 60 and 80 km to the west and west-northwest of Teniky, respectively, and were excavated by Vérin (1971). They yielded imported Persian and Chinese ceramics, as well as iron slag. Vérin (1971) proposed that they were occupied between the fourteenth and seventeenth centuries. However, Dewar and Wright (Citation1993) proposed a revision of the dates for these sites, suggesting that they were at least as old as the thirteenth century. Regional surveys and absolute age dating of Asambalahy and Rezoky are needed to determine whether any links might have existed in the past between them and nearby Teniky.

The former inhabitants of Teniky lived along the Sahanafo River, which joins the Malio, a tributary of the Isahena River, with the latter joining the Mangoky River near the small town of Beroroha, seventy kilometres north-northwest of Teniky. The Mangoky is the largest river in Madagascar and flows from the central highlands in a westerly direction to enter the Mozambique Channel fifty kilometres north of Morombe (). A large part of the Mangoky is navigable by small boats such as pirogues and might have been used in the past for inland reconnaissance and human migrations. From an archaeological point of view the Mangoky’s banks and the areas adjacent to them are underexplored, with regional surveys needed to determine whether any early inland settlements can be located. In this context, it is worth noting that excavations at a cave with rock art in the Makay Massif (), north of the Mangoky River, have yielded a radiocarbon carbon age on charcoal of 860 ± 30 BP (GifA-11109/SacA-24631; Gonthier et al. Citation2020a, Citation2020b), which corresponds to a calibrated age in the range cal. AD 1180–1276 (using OxCal 4.4 and SHCal20). However, it is unclear whether any material culture was directly associated with the excavated site. It would be interesting to compare the cave paintings from the Makay Massif with those documented by Rasolondrainy (Citation2012) at the rock shelter of Ampasimaiky in the southern part of the Isalo Massif, 120 km south of Teniky (). Rasolondrainy (Citation2012) proposed that some of the signs painted on the walls of the rock shelter resemble Libyco-Berber writings or inscriptions and inferred a pre-ninth-century AD human presence.

Dry stone walls are a prominent feature at Teniky, in particular in the Sahanafo Valley, where a stone-walled enclosure is situated close to the Sahanafo River with rectilinear stone walls north and east of it (Zone 3, ). Impressive stone-walled enclosures (called mandas) are also known from coeval sites in southern Madagascar such as Andranasoa and Andaro (). They are dated between the tenth and thirteenth centuries on the basis of radiocarbon dating and the presence of imported sgraffiato and Chinese ceramics (Parker Pearson et al. Citation2010). It is clear that further comparative studies between Teniky and the manda sites are necessary to determine whether they show similar archaeological features and whether their inhabitants shared a common culture.

Further south at the coast, Triangular Incised Ware (TIW) pottery has been found on the west and east bank of the Menarandra rivermouth (at Enijo, ; Parker-Pearson et al. Citation2010). This pottery style is from approximately AD 600–1000 along the southern Swahili coast of East Africa and indicates first-millennium interactions between Madagascar and East Africa (Parker-Pearson et al. Citation2010). So far, Enijo is the only site with TIW pottery in Madagascar and it remains unclear whether its occupants interacted with the manda sites or others such as Teniky further north.

At the moment it is not known whether Teniky had any connections with contemporaneous sites in northern Madagascar, such as Kingany (Anderson Citation2021), Mahilaka (Radimilahy 1981), Vohemar (Wright et al. Citation2022), Nosy Mangabe (Dewar and Wright Citation1993) or those in the Mananara Valley (Wright and Fanony Citation1992). More archaeological research, including detailed comparative analyses of local and imported pottery, is needed to determine the role that Teniky and its inhabitants played within Madagascar and the Indian Ocean.

Conclusions

Our archaeological excavations and field prospecting at Teniky reveal a much larger and more important archaeological landscape than previously known. This includes many newly found archaeological structures, including terraces, stone walls, stone basins and rock-cut structures in various sizes, shapes and forms constructed in the late first/early second millennia AD. No similar assemblage of archaeological structures is known anywhere else in Madagascar or East Africa. Our investigations of the rock-cut architecture in and near the cliff walls at Teniky suggest that most of them had a ritual function and we tentatively interpret them as part of a necropolis. The rock-cut niches at Teniky show similarities to those known from various sites throughout Iran, dated to the first millennium or older and related to Zoroastrian funerary practices. We cannot exclude the possibility that the archaeological structures at Teniky were the work of a group of people whose specific rites and beliefs developed and evolved after their arrival on the island and whose rock-cut structures show, by chance, formal similarities to Zoroastrian ones in Iran. However, we consider it more likely that the people who arrived on the coast of Madagascar and ultimately settled at Teniky introduced their rites and beliefs from outside the island and continued to practise them in a similar way while there. Independent of the origin, religion and funerary rites of Teniky’s former inhabitants, further archaeological studies are required to fully situate it within Madagascar and the western Indian Ocean. Questions that need to be addressed include: Where and when did the settlers first arrive on the coast of Madagascar? Did they come straight from their region of origin, or did they first settle in other parts of the Indian Ocean? Why did they move inland to the isolated inland site of Teniky? How did they live, how long did they stay and why was the site deserted? What was the relation of Teniky with contemporaneous sites on Madagascar and what was its role in the Indian Ocean trade network? We hope that future research may help resolve these questions.

Acknowledgments

We should like to thank the Ministry of Communications and Culture of Madagascar for granting us a research permit (309-2022/MCC/SG) to carry out excavations at Teniky. We express our gratitude to the late Dr Mamy A. Rakotoarijaona (Director General of Madagascar National Parks), Dr Harinaina Léon Razafindralaisa (Director General ad interim of Madagascar National Parks) and Nandrarana Jean-Jacques Rakotoarivelo (Director Isalo National Park) for their support of our research. Prof. Lucien M.A. Rakotozafy, Director of the Institute of Civilizations/Museum of Art and Archaeology (ICMAA) of the University of Antananarivo and Dr Bako Rasoarifetra (ICMAA) provided administrative and logistical help. We thank Prof. Dr Frank Preusser of the Universität Freiburg, Germany, for examining the samples taken for OSL dating, Dr Bing Zhao for giving the first age estimates for the ceramic sherds, Ali Aghanjazadeh for providing us with drone images and photographs of the rock-cut structures at Siraf and Hoda Moradi for acting as an intermediary. Finally, we should like to thank two anonymous reviewers for their constructive comments and suggestions. This work was supported by the Burgergemeinde Bern (grant numbers 2021-284 and 2022-736).