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International Journal of Humanities and Social Science Invention
ISSN (Online): 2319 – 7722, ISSN (Print): 2319 – 7714
www.ijhssi.org ||Volume 5 Issue 7 ||July. 2016 || PP.24-30
www.ijhssi.org 24 | Page
Asarkale on the Upper Aisepos Valley
Ayşe Çaylak Türker1
1
History of Art Department, Çanakkale Onsekiz Mart University
ABSTRACT: One of the important routes providing the transportation between the Hellespont and the
Kapıdağ Peninsula in the Byzantine period followed the Scamander and Aisepos Valleys. These valleys
constitute one of the areas we study to determine the military geography and defensive structures of the
Hellespont and its vicinity in the Byzantine period. In this manuscript, it was aimed to evaluate the
archaeological data we detected at Asarkale on the upper Aisepos Valley. It was predicted that the data to be
obtained with this evaluation would first of all contribute to the settlement of the problems of dating the
structure. Asartepe is approximately 310 m in length in the north-east - south-west direction. The highest
altitude of the hill is measured as around 798 m. First of all, a plan of the castle was drawn up by following the
walls of the castle in our study. The castle displays a long and narrow plan in the north-east - south-west
direction, in agreement with the topography of the hill. The defensive wall covering the north-west of the hill
approximately extends from the altitude of 783 m to the altitude of 795 m in the north-east - south-west
direction.
Keywords: Asarkale, Byzantine, Castle, Çanakkale, Hamdibey
I. Introduction
One of the important routes providing the transportation between the Hellespont and the Kapıdağ
Peninsula (Cyzicus) in the Byzantine period followed the Scamander and Aisepos Valleys [1]. These valleys
constitute one of the areas we study to determine the military geography and defensive structures of the
Hellespont and its vicinity in the Byzantine period. In this manuscript, it was aimed to evaluate the
archaeological data we detected at Asarkale on the upper Aisepos Valley [2] (Fig. 1). It was predicted that the
data to be obtained with this evaluation would first of all contribute to the settlement of the problems of dating
the structure.
II. Place and importance of asarkale in the aisepos valley
Aisepos originates by being nourished by more than one source in the Kaz Mountains. It is a valley
which extends for about 55 km in the north-east - south-west direction between the Kapıdağ Peninsula and the
Gulf of Edremit [3]. It has two different geographical characteristics. Its upper section has a connection with the
Scamander Valley. Therefore, it constitutes a natural road which originates from Cyzicus [4] – the metropolis of
Hellespontus – and provides access to the Aegean ports via the Hellespont. Given that the point this natural road
reached also provided access to the Black Sea and Mediterranean markets at the long distance and to the
Marmara and Aegean markets at the short distance, it is understood that such resources as the mines and wood
in the Kaz Mountains and in their close vicinity gained an economic value through these valleys [5].
Asarkale is located at one of the points qualifying as an intersection on the upper Aisepos Valley. With
its location at an altitude of 780 m, the castle controls the roads intersecting on the northern side of the Upper
Aisepos Valley. Of these roads, the first one follows the northern bank of Scamander, arrives in upper Aisepos
via Karaköy, and reaches around Asarkale [6]. The second road follows the north-eastern side of Mt. Katran in
the southern part of Aisepos from Karaköy in the west and arrives in the Aşağı Çavuş Village, whence it
progresses eastwards, passes to the northern side of Aisepos around Kalkım, and reaches around Asarkale. The
third road comes from the Gulf of Edremit in the south, follows the mountain roads, and reaches around the
Çamhisar Castle in Karaaydın, whence it crosses Aisepos in the north and arrives around Asarkale. The fourth
road comes from Pazarköy and Balya in the south-east and reaches around Çırpılar Kaletepesi. Another road
coming from the Gulf of Edremit also joins this point. Crossing Aisepos at this point and progressing to the
north-west, the road reaches around Asarkale. The fifth road originates from the Kapıdağ Peninsula, passes to
the northern side of Aisepos around Gönen, and reaches around Asarkale in the west.
Reaching around Asarkale, these roads follow the natural roads passing from the north-western margin
of Asarkale in the north. After Asarkale, this road progresses northwards first and then north-eastwards and
reaches Yenice. The middle and upper sections of the strait can easily be accessed through these byroads. The
defensive structures and surface finds we detected in these areas indicate that these road routes were used
throughout the Byzantine period. This road network, which we detected during our archaeological surveys in the
region, is new for the Byzantine studies.
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 25 | Page
Figure 1 Location of Asarkale and plan of the castle (Drawing by Türker Türker)
III. History of research
The remains on Asartepe, where the castle was located, were localized as Palaiskepsis by Kiepert [7].
A plan of these remains was published by Mordtmann [8]. According to the description by Mordtmann, on the
hill are remains of the walls, towers, aqueducts, and temple of the city of Palaiskepsis (Fig. 2). The walls were
built with large blocks of stones. The walls of the acropolis are 6 feet in thickness and made of black porphyry
marble. The towers were placed at irregular intervals, and there are four towers on the right-hand side of the
entrance. He expressed that the temple had probably been located in the north, in the area somewhat outside the
walls; however, he also stated that no trace had remained. He dated the visible building remains to the Classical
period. It is understood that Kiepert also accepted these findings.
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 26 | Page
Figure 2 Plan of the Asarkale Figure 3 Asartepe
(Mordtmann 1851)
Nevertheless, Wiegand dated the remains on Asartepe to the Byzantine period. He stated that the castle
in this area measured about 150m by 50m and had walls which were approximately 1.5 m thick. He said that the
castle had had two entrances and that the tower and cistern remains could be seen [9]. In his book, Hasluck
mentioned the remains in this area when conveying the discussions on the localization of Skepsis and
Palaiskepsis; however, he did not make any comment but stated that he had focused on Argiza in this region
[10]. When discussing the problem of localization of Palaiskepsis in his study in the region, Leaf stated that the
remains on Asartepe had belonged to the Byzantine period and that the ancient city must have been a little bit
further in the west [11]. When discussing Palaiskepsis and the relevant place names, Kahrstedt made a reference
to Asarkale but did not make any evaluation for the castle [12]. In the book entitled “the Byzantine Castles” and
prepared by Foss and Winfield, Asarkale is present with a panoramic photograph of its and it is dated to the
period of Byzantium which is called the dark ages [13].
Evaluations on Asarkale are also available in the reports on the surveys carried out in the region
recently. In the first one, a building described as Hadrian’s hunting lodge and located on one of the summits of
the mountains in the south of the district center of Yenice is mentioned without providing any information on
the location [14]. However, the photograph provided is from Asarkale. The second study contains a plan of
Asarkale, which is evaluated with the Alacaoluk Castle in Gönen, and both castles are dated to the 5th century
by making a reference to the political atmosphere experienced in this period by the empire [15]. As understood
from these data, there are different views about the quality and period of the building remains on Asartepe.
IV. Architecture Of Asarkale
Asartepe is approximately 310 m in length in the north-east - south-west direction (Fig. 3). The highest
altitude of the hill is measured as around 798 m [16]. First of all, a plan of the castle was drawn up by following
the walls of the castle in our study. The castle displays a long and narrow plan in the north-east - south-west
direction, in agreement with the topography of the hill (Fig. 1). The defensive wall covering the north-west of
the hill approximately extends from the altitude of 783 m to the altitude of 795 m in the north-east - south-west
direction. On the northern margin of this wall is the north-eastern entrance of the castle. A quadrilateral tower
was placed on both sides of the entrance. The covering of the walls belonging to Tower No. 1 in the south of the
entrance has been shed substantially (Fig. 4). The masonry built with irregular-sized unhewn stones is seen on
the preserved sections. The core is composed of white lime mortar and large unhewn stones. It is understood
that reused blocks were used as binders between the core and the masonry. One of the reused materials is a
double colonette at the eastern corner of the tower (Fig. 5). The wall covering of Tower No. 2 in the north of the
entrance has been shed substantially (Fig. 6). The rubble core is composed of white lime mortar and large
unhewn stones.
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 27 | Page
Figure 4 Asarkale, tower 1 Figure 5 Asarkele, east corner of the tower 1
Five towers can be detected on the defensive wall which covers the north of the castle. On the western
margin of this wall is the second entrance of the castle. It is understood that a quadrilateral tower was present on
both sides of this entrance. However, the walls of the tower were placed on the rocks, and it is hard to determine
the type and measurements of the towers due to the walls which are collapsed today. The wall covering of
Tower No. 3 on the northern defensive wall of the castle has been preserved, and large blocks of stones with
smoothly-shaped front faces were used on the masonry (Fig. 7). The stones were stacked in thin and thick rows.
Figure 6 Asarkale tower 2 Figure 7 Asarkale, tower 3
The mortared rubble core of Towers No. 4 and 5 has been preserved. The core is composed of large
unhewn stones and white lime mortar. On the upper section of Tower No. 4 is a lintel fragment which was
horizontally placed in the rubble core (Fig. 8). The covering of the wall between Towers No. 5 and 6 has been
preserved. The surface of the wall made of smoothly-shaped stones is covered with moss. The masonry of
Tower No. 6 has been preserved partially (Fig.9).
Smoothly-shaped large blocks of stones were stacked to form thin and thick rows on the preserved
section. The wall between Towers No. 6 and 7 can be followed in fragments. The covering of this wall has been
shed too; however, the mortared rubble core is in good condition. It can be discovered that bricks were also used
in the wall core which was made of large unhewn stones and white lime mortar. The stones used as binders
between the core and the surface covering have been preserved in this wall as well. Tower No. 7 has also
survived up to the present time together with its mortared rubble core. (Fig. 10).
The core composed of large unhewn stones and white lime mortar contains large blocks of stones
which were used as binders. This area is rocky; the walls sit on these rocks; and the rock surfaces were
sometimes used as part of the wall. The same material and the same building technique are also followed on the
walls extending from this tower to the south-western entrance of the castle. The dense vegetation in the south-
west of this area does not allow making an examination. Nevertheless, according to the traces on the surface, it
may be predicted that there used to be architectural units connected with the castle in this area.
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 28 | Page
Figure 8 Asarkale, tower 4 Figure 9 Asarkale, tower 6
The wall extending in the north-west - south-east direction and covering the south-west of the hill
extends at an altitude of about 788 m. On this defensive wall is Tower No. 8, whose mortared rubble core has
been preserved (Fig. 11).
The wall which covers the south-east of the hill extends between the altitudes of 784 and 794 m in the
south-west - north-east direction. Traces of seven towers are detected on this defensive wall. The eastern and
southern walls of Tower No. 9 have been preserved (Fig. 12). Having survived up to the present time together
with their mortared rubble core, these walls sit on the local rocks. The south-eastern corner of Tower No. 10 has
been preserved (Fig. 13).
Figure 10 Asarkale, tower 7 Figure 11 Asarkale tower 8
Large horizontal blocks used as binders can be detected in the core that was composed of large unhewn
stones and white lime mortar. The wall covering of Tower No. 11 has been preserved partially (Fig. 14).
Smoothly-shaped thin and thick blocks were used on the two preserved rows of stones. The mortared rubble
core contains few broken bricks. The wall covering of Tower No. 12 has been preserved partially. The preserved
sections indicate that different-sized and smoothly-shaped stones were used in the wall covering. Besides large
unhewn stones, few broken brick fragments can be detected in the mortared rubble core (Fig. 15). Towers No.
13, 14 and 15 have also been preserved with their rubble core (Fig. 16-17). The core contains few broken brick
fragments. Large blocks of stones used as binders between the core and the wall surface can be detected at these
towers too.
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 29 | Page
Figure 12 Asarkale, tower 9 Figure 13 Asarkale, tower 10
Figure 14 Asarkale, tower 11 Figure 15 Asarkale tower 12
The archaeological traces of building inside the castle are concentrated in three sections. They have
been marked with Letters A, B, and C in the plan. There is a cistern in the area corresponding to the south of
Tower No. 3 and marked with A (Fig. 18). Bricks were used in the masonry of the cistern. The bricks are 31 cm
in length and 3.5 to 4 cm in thickness on average. The mortar between the bricks is the white lime mortar with
dense and large broken bricks. On the other hand, the plaster covering the wall surface has only been preserved
in the lower section of the walls. Wall fragments are found in the rocky areas marked with B and C; however, no
plan can be followed. Fragments of ground stones (Fig. 19), pottery and terracotta construction materials are
available in dispersed condition on the surface inside the castle. The terracotta roof covering materials include a
fragment of the late Roman period as well as edge and body fragments of cover and flat tiles dated to the
Byzantine period.
Figure 16 Asarkale, tower 13 Figure 17 Asarkale, tower 15
Asarkale on the Upper Aisepos Valley
www.ijhssi.org 30 | Page
Figure 18 Cistern Figure 19 Fragments of ground stones
V. Conclusion
In conclusion, the castle displays a long and narrow plan in the north-east - south-west direction, in
agreement with the topography of the hill. It has two entrances in the north-east and south-west. Both entrances
are understood to have been fortified with quadrilateral towers. Even though it is hard to determine the types and
measurements of the towers owing to the collapsed wall sections and the shed wall coverings, it is understood
that the walls of the castle were fortified with a total of 17 towers. The towers have a quadrilateral plan. The
majority of the walls belonging to the castle, which carries the overall character of the Byzantine defensive
structures with these qualities, have survived up to the present time together with their mortared rubble core.
The core is composed of dense lime mortar, large unhewn stones, and broken brick fragments. The reused
fragments preserved in the rubble core are understood to have been used to function as a binder between the
core and the masonry. Besides reused stones, regularly-shaped large stones were used on the wall covering on
the front and back sides of the core. These stones were placed to form a thin row and a thick row in the masonry
each. The fragment with the latest date that can be detected among the reused materials is a coupled column
which is dated to the 5th-6th century. The use of reused fragments to function as a binder between the core and
the masonry was a common application particularly in the Byzantine defensive structures constructed during the
Arab raids in the 7th and 8th centuries [17]. Similar applications were also documented at Hala Hisar [18], Bolu,
in Asarlık, Yırca [19], at Fındıklı Kale, Kuşadası [20], and in Altıntaş, Kütahya [21] that were dated to the same
period. With these qualities of its, Asarkale may be evaluated among the defensive structures of the 7th & 8th
centuries.
References
[1]. For the archaeological data on the Scamander Valley, see A. Çaylak Türker, Bizans Döneminde Çanakkale Boğazı ve Yerleşim
Modelleri: Skamander Vadisi. Anadolu ve Çevresinde Ortaçağ, 4, 2010, 53-94.
[2]. Today Asarkale is located in Hamdibey, Yenice, Çanakkale. It is known as Hamdibey-Asarkale or Koyuneli-Asarkale – the ancient
name of Hamdibey. Today the castle is accessed via the Namazgah Village.
[3]. For Aisepos Valley see, A. Ç. Türker, Archaeological survey of early Christian – Byzantine period on the valleys that reached the
Hellespont: 2012 research. 31. Araştırma Sonuçları Toplantısı 1. Muğla 2014, 192-196.
[4]. The Anatolian shore of the Hellespont is called the Hellespontus region. This region was established in some part of ancient Mysia
and Phrygia Minor. According to the 36th Canon of the Trullan Synod in 692, the metropolis of Hellespontus is Cyzicus. See J. E.
T. Wiltsch, Handbuch der kirhlichen Geographie und Statistik. Berlin 1846, 414-415, 312-313.
[5]. Munro, who arrived in Troas in the late 19th century, stated that the trees cut from Mt. Ida had been brought to the sea via the
Aisepos and Scamander Rivers and sent as far as Alexandria from this point. Furthermore, he wrote that the estuary of Aisepos had
turned into a dark color due to the tree barks. See A. Munro, Gleanings from Mysia. Journal of Hellenic Studies 21, 1901, 235.
[6]. This intersection, where the roads intersect, is around the ancient Karabey Village in the south of Asarkale.
[7]. Kiepert, H. Specialkarte vom westlichen Kleinasien nach seinen eigenen Reisen und nach andern grösstenteils noch
unveröffentlichten Routenaufnahmen. Berlin 1892.
[8]. F. Babinger, Anatolien Skizzen und Reisebriefe aus Kleinasien (1850-1859) von A. D. Mordtmann D. Ä. Osnabrück, 1972, 285-348.
[9]. Th. Wiegand, Reisen in Mysien. Mitteilungen des Kaiserich Deotschen Archäologischen Instituts Athenische Abteilung, XXIX,
1904, 274.
[10]. F. W. Hasluck, Cyzicus. Cambridge 1910, 110-111.
[11]. W. Leaf, Strabo on Troad. London 1923, 211.
[12]. U. Kahrstedt, Palaiskepsis und verwandte Ortsnamen. Historia: Zeitschrift für Alte Geschichte. 3, 1955, 293-294.
[13]. C. Foss - D. Winfield, Byzantine Fortifications:An Introduction. Pretoria, 1986, 140-141, fig.17.
[14]. C. Başaran, - A.Y. Tavukçu, - V. Keleş, – E. Küçükefe - Z. A. Tavukçu, Kuzey Troas-Parion Araştırmaları 2002. 21. Araştırma
Sonuçları Toplantısı 1, Ankara 2004: 187, res. 9. 5-192.
[15]. C. B. Rose – R. Körpe, (). The Granicus River Valley Survey Project, 2007. 26. Araştırma Sonuçları Toplantısı 2. Ankara 2009,
347-348, fig 11.
[16]. Topcon GPT3007N total station was used in the measurements at the castle.
[17]. C. Foss - D. Winfield, Byzantine Fortifications: An Introduction, Pretoria 1986, 162.
[18]. L. Robert, A travers l’Asie Mineure, Paris 1980, 136; W. Von Diest, Von Pergamon über den Dindymos zum Pontus. Petermanns
Mitteilungen Ergänzungsheft, 94, 1889, 61.
[19]. L. Robert, Villes d’Asie Mineure. Paris 1962, 435.
[20]. W. Müller-Weiner, Die Stadtmauer von İzmir, Sığacık und Çandarlı. Istanbuler Mitteilungen,12, 1961, 62-65.
[21]. C. Foss, Survey of Medieval Castles of Anatolia, 1: Kütahya, Oxford 1985, 96-98.

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Asarkale on the Upper Aisepos Valley

  • 1. International Journal of Humanities and Social Science Invention ISSN (Online): 2319 – 7722, ISSN (Print): 2319 – 7714 www.ijhssi.org ||Volume 5 Issue 7 ||July. 2016 || PP.24-30 www.ijhssi.org 24 | Page Asarkale on the Upper Aisepos Valley Ayşe Çaylak Türker1 1 History of Art Department, Çanakkale Onsekiz Mart University ABSTRACT: One of the important routes providing the transportation between the Hellespont and the Kapıdağ Peninsula in the Byzantine period followed the Scamander and Aisepos Valleys. These valleys constitute one of the areas we study to determine the military geography and defensive structures of the Hellespont and its vicinity in the Byzantine period. In this manuscript, it was aimed to evaluate the archaeological data we detected at Asarkale on the upper Aisepos Valley. It was predicted that the data to be obtained with this evaluation would first of all contribute to the settlement of the problems of dating the structure. Asartepe is approximately 310 m in length in the north-east - south-west direction. The highest altitude of the hill is measured as around 798 m. First of all, a plan of the castle was drawn up by following the walls of the castle in our study. The castle displays a long and narrow plan in the north-east - south-west direction, in agreement with the topography of the hill. The defensive wall covering the north-west of the hill approximately extends from the altitude of 783 m to the altitude of 795 m in the north-east - south-west direction. Keywords: Asarkale, Byzantine, Castle, Çanakkale, Hamdibey I. Introduction One of the important routes providing the transportation between the Hellespont and the Kapıdağ Peninsula (Cyzicus) in the Byzantine period followed the Scamander and Aisepos Valleys [1]. These valleys constitute one of the areas we study to determine the military geography and defensive structures of the Hellespont and its vicinity in the Byzantine period. In this manuscript, it was aimed to evaluate the archaeological data we detected at Asarkale on the upper Aisepos Valley [2] (Fig. 1). It was predicted that the data to be obtained with this evaluation would first of all contribute to the settlement of the problems of dating the structure. II. Place and importance of asarkale in the aisepos valley Aisepos originates by being nourished by more than one source in the Kaz Mountains. It is a valley which extends for about 55 km in the north-east - south-west direction between the Kapıdağ Peninsula and the Gulf of Edremit [3]. It has two different geographical characteristics. Its upper section has a connection with the Scamander Valley. Therefore, it constitutes a natural road which originates from Cyzicus [4] – the metropolis of Hellespontus – and provides access to the Aegean ports via the Hellespont. Given that the point this natural road reached also provided access to the Black Sea and Mediterranean markets at the long distance and to the Marmara and Aegean markets at the short distance, it is understood that such resources as the mines and wood in the Kaz Mountains and in their close vicinity gained an economic value through these valleys [5]. Asarkale is located at one of the points qualifying as an intersection on the upper Aisepos Valley. With its location at an altitude of 780 m, the castle controls the roads intersecting on the northern side of the Upper Aisepos Valley. Of these roads, the first one follows the northern bank of Scamander, arrives in upper Aisepos via Karaköy, and reaches around Asarkale [6]. The second road follows the north-eastern side of Mt. Katran in the southern part of Aisepos from Karaköy in the west and arrives in the Aşağı Çavuş Village, whence it progresses eastwards, passes to the northern side of Aisepos around Kalkım, and reaches around Asarkale. The third road comes from the Gulf of Edremit in the south, follows the mountain roads, and reaches around the Çamhisar Castle in Karaaydın, whence it crosses Aisepos in the north and arrives around Asarkale. The fourth road comes from Pazarköy and Balya in the south-east and reaches around Çırpılar Kaletepesi. Another road coming from the Gulf of Edremit also joins this point. Crossing Aisepos at this point and progressing to the north-west, the road reaches around Asarkale. The fifth road originates from the Kapıdağ Peninsula, passes to the northern side of Aisepos around Gönen, and reaches around Asarkale in the west. Reaching around Asarkale, these roads follow the natural roads passing from the north-western margin of Asarkale in the north. After Asarkale, this road progresses northwards first and then north-eastwards and reaches Yenice. The middle and upper sections of the strait can easily be accessed through these byroads. The defensive structures and surface finds we detected in these areas indicate that these road routes were used throughout the Byzantine period. This road network, which we detected during our archaeological surveys in the region, is new for the Byzantine studies.
  • 2. Asarkale on the Upper Aisepos Valley www.ijhssi.org 25 | Page Figure 1 Location of Asarkale and plan of the castle (Drawing by Türker Türker) III. History of research The remains on Asartepe, where the castle was located, were localized as Palaiskepsis by Kiepert [7]. A plan of these remains was published by Mordtmann [8]. According to the description by Mordtmann, on the hill are remains of the walls, towers, aqueducts, and temple of the city of Palaiskepsis (Fig. 2). The walls were built with large blocks of stones. The walls of the acropolis are 6 feet in thickness and made of black porphyry marble. The towers were placed at irregular intervals, and there are four towers on the right-hand side of the entrance. He expressed that the temple had probably been located in the north, in the area somewhat outside the walls; however, he also stated that no trace had remained. He dated the visible building remains to the Classical period. It is understood that Kiepert also accepted these findings.
  • 3. Asarkale on the Upper Aisepos Valley www.ijhssi.org 26 | Page Figure 2 Plan of the Asarkale Figure 3 Asartepe (Mordtmann 1851) Nevertheless, Wiegand dated the remains on Asartepe to the Byzantine period. He stated that the castle in this area measured about 150m by 50m and had walls which were approximately 1.5 m thick. He said that the castle had had two entrances and that the tower and cistern remains could be seen [9]. In his book, Hasluck mentioned the remains in this area when conveying the discussions on the localization of Skepsis and Palaiskepsis; however, he did not make any comment but stated that he had focused on Argiza in this region [10]. When discussing the problem of localization of Palaiskepsis in his study in the region, Leaf stated that the remains on Asartepe had belonged to the Byzantine period and that the ancient city must have been a little bit further in the west [11]. When discussing Palaiskepsis and the relevant place names, Kahrstedt made a reference to Asarkale but did not make any evaluation for the castle [12]. In the book entitled “the Byzantine Castles” and prepared by Foss and Winfield, Asarkale is present with a panoramic photograph of its and it is dated to the period of Byzantium which is called the dark ages [13]. Evaluations on Asarkale are also available in the reports on the surveys carried out in the region recently. In the first one, a building described as Hadrian’s hunting lodge and located on one of the summits of the mountains in the south of the district center of Yenice is mentioned without providing any information on the location [14]. However, the photograph provided is from Asarkale. The second study contains a plan of Asarkale, which is evaluated with the Alacaoluk Castle in Gönen, and both castles are dated to the 5th century by making a reference to the political atmosphere experienced in this period by the empire [15]. As understood from these data, there are different views about the quality and period of the building remains on Asartepe. IV. Architecture Of Asarkale Asartepe is approximately 310 m in length in the north-east - south-west direction (Fig. 3). The highest altitude of the hill is measured as around 798 m [16]. First of all, a plan of the castle was drawn up by following the walls of the castle in our study. The castle displays a long and narrow plan in the north-east - south-west direction, in agreement with the topography of the hill (Fig. 1). The defensive wall covering the north-west of the hill approximately extends from the altitude of 783 m to the altitude of 795 m in the north-east - south-west direction. On the northern margin of this wall is the north-eastern entrance of the castle. A quadrilateral tower was placed on both sides of the entrance. The covering of the walls belonging to Tower No. 1 in the south of the entrance has been shed substantially (Fig. 4). The masonry built with irregular-sized unhewn stones is seen on the preserved sections. The core is composed of white lime mortar and large unhewn stones. It is understood that reused blocks were used as binders between the core and the masonry. One of the reused materials is a double colonette at the eastern corner of the tower (Fig. 5). The wall covering of Tower No. 2 in the north of the entrance has been shed substantially (Fig. 6). The rubble core is composed of white lime mortar and large unhewn stones.
  • 4. Asarkale on the Upper Aisepos Valley www.ijhssi.org 27 | Page Figure 4 Asarkale, tower 1 Figure 5 Asarkele, east corner of the tower 1 Five towers can be detected on the defensive wall which covers the north of the castle. On the western margin of this wall is the second entrance of the castle. It is understood that a quadrilateral tower was present on both sides of this entrance. However, the walls of the tower were placed on the rocks, and it is hard to determine the type and measurements of the towers due to the walls which are collapsed today. The wall covering of Tower No. 3 on the northern defensive wall of the castle has been preserved, and large blocks of stones with smoothly-shaped front faces were used on the masonry (Fig. 7). The stones were stacked in thin and thick rows. Figure 6 Asarkale tower 2 Figure 7 Asarkale, tower 3 The mortared rubble core of Towers No. 4 and 5 has been preserved. The core is composed of large unhewn stones and white lime mortar. On the upper section of Tower No. 4 is a lintel fragment which was horizontally placed in the rubble core (Fig. 8). The covering of the wall between Towers No. 5 and 6 has been preserved. The surface of the wall made of smoothly-shaped stones is covered with moss. The masonry of Tower No. 6 has been preserved partially (Fig.9). Smoothly-shaped large blocks of stones were stacked to form thin and thick rows on the preserved section. The wall between Towers No. 6 and 7 can be followed in fragments. The covering of this wall has been shed too; however, the mortared rubble core is in good condition. It can be discovered that bricks were also used in the wall core which was made of large unhewn stones and white lime mortar. The stones used as binders between the core and the surface covering have been preserved in this wall as well. Tower No. 7 has also survived up to the present time together with its mortared rubble core. (Fig. 10). The core composed of large unhewn stones and white lime mortar contains large blocks of stones which were used as binders. This area is rocky; the walls sit on these rocks; and the rock surfaces were sometimes used as part of the wall. The same material and the same building technique are also followed on the walls extending from this tower to the south-western entrance of the castle. The dense vegetation in the south- west of this area does not allow making an examination. Nevertheless, according to the traces on the surface, it may be predicted that there used to be architectural units connected with the castle in this area.
  • 5. Asarkale on the Upper Aisepos Valley www.ijhssi.org 28 | Page Figure 8 Asarkale, tower 4 Figure 9 Asarkale, tower 6 The wall extending in the north-west - south-east direction and covering the south-west of the hill extends at an altitude of about 788 m. On this defensive wall is Tower No. 8, whose mortared rubble core has been preserved (Fig. 11). The wall which covers the south-east of the hill extends between the altitudes of 784 and 794 m in the south-west - north-east direction. Traces of seven towers are detected on this defensive wall. The eastern and southern walls of Tower No. 9 have been preserved (Fig. 12). Having survived up to the present time together with their mortared rubble core, these walls sit on the local rocks. The south-eastern corner of Tower No. 10 has been preserved (Fig. 13). Figure 10 Asarkale, tower 7 Figure 11 Asarkale tower 8 Large horizontal blocks used as binders can be detected in the core that was composed of large unhewn stones and white lime mortar. The wall covering of Tower No. 11 has been preserved partially (Fig. 14). Smoothly-shaped thin and thick blocks were used on the two preserved rows of stones. The mortared rubble core contains few broken bricks. The wall covering of Tower No. 12 has been preserved partially. The preserved sections indicate that different-sized and smoothly-shaped stones were used in the wall covering. Besides large unhewn stones, few broken brick fragments can be detected in the mortared rubble core (Fig. 15). Towers No. 13, 14 and 15 have also been preserved with their rubble core (Fig. 16-17). The core contains few broken brick fragments. Large blocks of stones used as binders between the core and the wall surface can be detected at these towers too.
  • 6. Asarkale on the Upper Aisepos Valley www.ijhssi.org 29 | Page Figure 12 Asarkale, tower 9 Figure 13 Asarkale, tower 10 Figure 14 Asarkale, tower 11 Figure 15 Asarkale tower 12 The archaeological traces of building inside the castle are concentrated in three sections. They have been marked with Letters A, B, and C in the plan. There is a cistern in the area corresponding to the south of Tower No. 3 and marked with A (Fig. 18). Bricks were used in the masonry of the cistern. The bricks are 31 cm in length and 3.5 to 4 cm in thickness on average. The mortar between the bricks is the white lime mortar with dense and large broken bricks. On the other hand, the plaster covering the wall surface has only been preserved in the lower section of the walls. Wall fragments are found in the rocky areas marked with B and C; however, no plan can be followed. Fragments of ground stones (Fig. 19), pottery and terracotta construction materials are available in dispersed condition on the surface inside the castle. The terracotta roof covering materials include a fragment of the late Roman period as well as edge and body fragments of cover and flat tiles dated to the Byzantine period. Figure 16 Asarkale, tower 13 Figure 17 Asarkale, tower 15
  • 7. Asarkale on the Upper Aisepos Valley www.ijhssi.org 30 | Page Figure 18 Cistern Figure 19 Fragments of ground stones V. Conclusion In conclusion, the castle displays a long and narrow plan in the north-east - south-west direction, in agreement with the topography of the hill. It has two entrances in the north-east and south-west. Both entrances are understood to have been fortified with quadrilateral towers. Even though it is hard to determine the types and measurements of the towers owing to the collapsed wall sections and the shed wall coverings, it is understood that the walls of the castle were fortified with a total of 17 towers. The towers have a quadrilateral plan. The majority of the walls belonging to the castle, which carries the overall character of the Byzantine defensive structures with these qualities, have survived up to the present time together with their mortared rubble core. The core is composed of dense lime mortar, large unhewn stones, and broken brick fragments. The reused fragments preserved in the rubble core are understood to have been used to function as a binder between the core and the masonry. Besides reused stones, regularly-shaped large stones were used on the wall covering on the front and back sides of the core. These stones were placed to form a thin row and a thick row in the masonry each. The fragment with the latest date that can be detected among the reused materials is a coupled column which is dated to the 5th-6th century. The use of reused fragments to function as a binder between the core and the masonry was a common application particularly in the Byzantine defensive structures constructed during the Arab raids in the 7th and 8th centuries [17]. Similar applications were also documented at Hala Hisar [18], Bolu, in Asarlık, Yırca [19], at Fındıklı Kale, Kuşadası [20], and in Altıntaş, Kütahya [21] that were dated to the same period. With these qualities of its, Asarkale may be evaluated among the defensive structures of the 7th & 8th centuries. References [1]. For the archaeological data on the Scamander Valley, see A. Çaylak Türker, Bizans Döneminde Çanakkale Boğazı ve Yerleşim Modelleri: Skamander Vadisi. Anadolu ve Çevresinde Ortaçağ, 4, 2010, 53-94. [2]. Today Asarkale is located in Hamdibey, Yenice, Çanakkale. It is known as Hamdibey-Asarkale or Koyuneli-Asarkale – the ancient name of Hamdibey. Today the castle is accessed via the Namazgah Village. [3]. For Aisepos Valley see, A. Ç. Türker, Archaeological survey of early Christian – Byzantine period on the valleys that reached the Hellespont: 2012 research. 31. Araştırma Sonuçları Toplantısı 1. Muğla 2014, 192-196. [4]. The Anatolian shore of the Hellespont is called the Hellespontus region. This region was established in some part of ancient Mysia and Phrygia Minor. According to the 36th Canon of the Trullan Synod in 692, the metropolis of Hellespontus is Cyzicus. See J. E. T. Wiltsch, Handbuch der kirhlichen Geographie und Statistik. Berlin 1846, 414-415, 312-313. [5]. Munro, who arrived in Troas in the late 19th century, stated that the trees cut from Mt. Ida had been brought to the sea via the Aisepos and Scamander Rivers and sent as far as Alexandria from this point. Furthermore, he wrote that the estuary of Aisepos had turned into a dark color due to the tree barks. See A. Munro, Gleanings from Mysia. Journal of Hellenic Studies 21, 1901, 235. [6]. This intersection, where the roads intersect, is around the ancient Karabey Village in the south of Asarkale. [7]. Kiepert, H. Specialkarte vom westlichen Kleinasien nach seinen eigenen Reisen und nach andern grösstenteils noch unveröffentlichten Routenaufnahmen. Berlin 1892. [8]. F. Babinger, Anatolien Skizzen und Reisebriefe aus Kleinasien (1850-1859) von A. D. Mordtmann D. Ä. Osnabrück, 1972, 285-348. [9]. Th. Wiegand, Reisen in Mysien. Mitteilungen des Kaiserich Deotschen Archäologischen Instituts Athenische Abteilung, XXIX, 1904, 274. [10]. F. W. Hasluck, Cyzicus. Cambridge 1910, 110-111. [11]. W. Leaf, Strabo on Troad. London 1923, 211. [12]. U. Kahrstedt, Palaiskepsis und verwandte Ortsnamen. Historia: Zeitschrift für Alte Geschichte. 3, 1955, 293-294. [13]. C. Foss - D. Winfield, Byzantine Fortifications:An Introduction. Pretoria, 1986, 140-141, fig.17. [14]. C. Başaran, - A.Y. Tavukçu, - V. Keleş, – E. Küçükefe - Z. A. Tavukçu, Kuzey Troas-Parion Araştırmaları 2002. 21. Araştırma Sonuçları Toplantısı 1, Ankara 2004: 187, res. 9. 5-192. [15]. C. B. Rose – R. Körpe, (). The Granicus River Valley Survey Project, 2007. 26. Araştırma Sonuçları Toplantısı 2. Ankara 2009, 347-348, fig 11. [16]. Topcon GPT3007N total station was used in the measurements at the castle. [17]. C. Foss - D. Winfield, Byzantine Fortifications: An Introduction, Pretoria 1986, 162. [18]. L. Robert, A travers l’Asie Mineure, Paris 1980, 136; W. Von Diest, Von Pergamon über den Dindymos zum Pontus. Petermanns Mitteilungen Ergänzungsheft, 94, 1889, 61. [19]. L. Robert, Villes d’Asie Mineure. Paris 1962, 435. [20]. W. Müller-Weiner, Die Stadtmauer von İzmir, Sığacık und Çandarlı. Istanbuler Mitteilungen,12, 1961, 62-65. [21]. C. Foss, Survey of Medieval Castles of Anatolia, 1: Kütahya, Oxford 1985, 96-98.