The E ff ect of Fire on Building Materials : The Case-Study of the Varnakova Monastery Cells in Central Greece

The evaluation of the fire impact on building materials is of great scientific and socio-economic importance since fire can result in materials’ chemical and mechanical alterations, which leads to structural stability problems of historical and/or modern construction. This highly increases the cost of rehabilitation interventions. The case study of the Byzantine Monastery of Panagia (Virgin Mary) Varnakova is an example of the fire effect on both historical and newer stone masonries. The Varnakova Monastery is a typical 19th century monastic complex and, during its long history, it has undergone multiple reconstructions after major catastrophic events that have taken place due to its strategic geographical position and its financial and spiritual significance for the region. The last big-scale renovation of the Monastery was conducted between the years 1992 to 2014. However, in January 2017, a devastating fire destroyed the largest part of the monastic cells’ quarter. In this work, a diagnostic study of the different construction phases’ materials comprising the masonries of the monastery cells in their present state is presented. The examination of a series of samples through analytical techniques, such as optical microscopy, X-ray diffraction, thermal analysis, and total immersion tests, along with the use of non-destructive techniques in situ, such as Infra Red Thermography, Digital Microscopy, and Schmidt Hammer Rebound tests, shed light on the preservation state and on the decay of the diverse building materials. In addition, the impact of the fire on their properties was investigated. The results reveal the diversity of the materials used in the historical masonries throughout the centuries, while the combination of analytical and non-destructive techniques demonstrates the damages induced by the fire.


Introduction
In recent years, more research has focused on the effect of high temperatures on building materials [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16].The development of high temperatures affects the various characteristics of a material.Petrographic, mineralogical, chemical, physical, and mechanical properties may alter, depending on the temperatures developed, the characteristics of the material, the timeframe of the high temperature event, and the manner of cooling.The assessment of the effect of high temperatures on the building materials of a structure, especially after a catastrophic event, such as a fire, is crucial in order to evaluate the safety level of its damaged state and plan appropriate repair measures [10].This assessment is even more important in the case of monumental structures, where the historic building materials are "precious" and should, if possible, be replaced to the minimum extent.
The effect of high temperature on a building material is a complex mechanism and various material properties must be examined in order to obtain a holistic view of a fire effect.Visual inspection provides useful information regarding the effect of a fire event, since many damages and decay patterns are macroscopically manifested, including cracking, surface crazing, deflection, delamination, color changes, and smoke damage [12,13,15,16].
Petrographic analysis assists not only in the characterization of a stone type, which reveals composition, texture, binder type, and micro-morphology, but in the evaluation of the effect of high temperature as well, by examining the alterations observed in these characteristics [2,[4][5][6][7]10].A temperature increase induces inter-granular and intra-granular effects on a material while inter-granular effects are connected to the development of microcracks within the matrix of the material and are usually the result of different characteristics of the material's constituents.Intra-granular effects manifest through the development of microcracks within the grains themselves [1].Inherent anisotropy of materials is an example of degradation in the case of thermal loads.For example, inherent anisotropy of calcite grains, when heated, is considered to be the main agent for marble and limestones disintegration [11,13].Mineralogical analysis reveals the alteration of mineralogical compounds.Thus, the absence or decrease of a compound after the fire event is indicative that the fire reached a temperature at which the compound's structure irreversibly collapses and/or is transformed into an amorphous compound that is no longer detectable [2].Chemical analysis can reveal alterations in the composition of the material, which is also connected to transformations that take place during the fire effect.These alterations include oxidation, dehydration, de-hydroxylation, calcination, and other processes [6,14].These processes may infer matrix alterations of a building material and/or color changes, such as reddening (e.g., when ferrous minerals are included in the material).Thus, for example, the clay and iron oxides-hydroxides content within a stone or aggregates of a mortar may be a determinant for a series of transformations induced by heat [16].
Microstructural analysis is of paramount importance since the alteration of microstructural characteristics affects other properties, such as the behavior of a material under hygro-thermic loads and compressive strength [1][2][3][4][5][6][7]9]. Porosity usually increases when a material is subjected to high temperatures [1,3], while density decreases due to material loss and compound decomposition, dehydroxilation, and dehydration processes.Mechanical characteristics are crucial to structural stability.Compressive strength usually decreases due to the development of microcracks and/or the increase of porosity [8,9].
The effect of fire and the consequent alterations induced to a material's characteristics is clearly dependent on the material itself.In the case of stones, each lithotype presents a different behavior to fire-attack, depending on pertrographic characteristics, chemical composition, porosity, anisotropy of its components, etc.For example, granites are more prone to crack when thermally shocked, in comparison with other softer stones [5].In quartz-rich sandstones, due to the open porosity they exhibit, as well as due to their calcitic matrix (which undergoes a parallel calcining process), micro-strains due to quartz expansion (when it is transformed from α→β at ~575 • C), are absorbed by the matrix [1].Thus, knowledge of the type of stone and parallel evaluation of alterations studied in related research and practice can assist in predicting the alterations induced in a certain lithotype in the event of a fire [12].
In terms of physico-mechanical and structural stability of the monument, it is crucial to assess the impact of fire damage.In an extent to the above discussion, the indirect consequences to the whole masonry need to be taken under consideration, during a diagnostic study.Another important aspect to be explored is the variability of the fire impact parameters on the different lithotypes and parts of the masonry depending on the diverse temperatures, duration of the event, or other synergic factors (e.g., precedent defaults of a masonry block or an isolated stone).Mortars, depending on the mortar type, Heritage 2019, 2 1235 may be more or less resistant to a fire event.For example, concrete presents low thermal diffusivity and high incombustibility.However, the decrease in its load-bearing capability and its "explosive spalling" due to the fire action may compromise these assets, especially when the fire temperature exceeds 300 • C [15,16].Taking into account all the above, the fire impact needs to be addressed initially in terms of building materials.However, it aims to a holistic perspective by studying the structure as a whole.
Within the above framework, this study is an attempt to investigate the effect of the 2017 fire event on the Varnakova Monastery building materials and the masonries they comprise.Hereby, the preliminary results of a diagnostic study through an in situ non-destructive testing and an in-lab application of analytical techniques on selected samples are presented, which aim to understand the effect of the fire on the different lithotypes and mortars comprising the masonries of this historic structure.

The Varnakova Monastery
The Byzantine Monastery of Panagia (Virgin Mary) Varnakova is located on a mountainous landscape of Southwest Central Greece, at an altitude of 800 m (Figure 1a).Its general structure follows the typical 19th century of a monastic complex with an almost-rectangular courtyard and a church (catholicon) in the center (Figure 1b, topographic depiction: Figure 1c) [17].The evolution of the architectural phases of the catholicon until the 13th century is reflected in the Ch.Bouras drawing (Figure 1d) [18].
Heritage2019, 2 FOR PEER REVIEW 3 diffusivity and high incombustibility.However, the decrease in its load-bearing capability and its "explosive spalling" due to the fire action may compromise these assets, especially when the fire temperature exceeds 300°C [15,16].Taking into account all the above, the fire impact needs to be addressed initially in terms of building materials.However, it aims to a holistic perspective by studying the structure as a whole.Within the above framework, this study is an attempt to investigate the effect of the 2017 fire event on the Varnakova Monastery building materials and the masonries they comprise.Hereby, the preliminary results of a diagnostic study through an in situ non-destructive testing and an in-lab application of analytical techniques on selected samples are presented, which aim to understand the effect of the fire on the different lithotypes and mortars comprising the masonries of this historic structure.

The Varnakova Monastery
The Byzantine Monastery of Panagia (Virgin Mary) Varnakova is located on a mountainous landscape of Southwest Central Greece, at an altitude of 800 m (Figure 1a).Its general structure follows the typical 19 th century of a monastic complex with an almost-rectangular courtyard and a church (catholicon) in the center (Figure 1b, topographic depiction: Figure1c) [17].The evolution of the architectural phases of the catholicon until the 13 th century is reflected in the Ch.Bouras drawing (Figure 1d) [18].The first church was founded in 1077 AD by Saint Arsenios Varnakovitis.During the 11th and 12th century, it was decorated with wall paintings and on-floor marble mosaics, while the extended renovation of 1148-1151 was fostered by the Byzantine emperors of the Comnenian Dynasty, some of whom were buried beneath the monastery, as referred by A. Orlandos in his 1922 study [20].The church, as it was at the time of Orlandos's inspection, is referred to as a three-aisled basilica with a narthex and a main altar [21].
The monastery was almost completely destroyed in 1826, as it served as refuge and base during the Greek War of Independence (1821-1830) against the Ottoman Empire.The reconstruction works commenced soon after the liberation, in 1831, according to the plans made by the architect Andreas Gasparis Kalandros, an army lieutenant, and were completed by three Epirot masons by 1838.This is also the year of the construction of the wooden temple of the catholicon.A. Orlandos uses the term "hammered limestones" to describe the chosen building material used in this construction phase [17,21].
Between the years 1992-2014, the monastery was extensively renovated.On 29 January 2017, a devastating fire started due to a boiler explosion destroyed the largest part of the monastic cells' quarter [22].Thus today, the monastery cells are in a state of collapse and in need of major restoration and rebuilding (Figure 2).
Heritage2019, 2 FOR PEER REVIEW 4 renovation of 1148-1151 was fostered by the Byzantine emperors of the Comnenian Dynasty, some of whom were buried beneath the monastery, as referred by A. Orlandos in his 1922 study [20].The church, as it was at the time of Orlandos's inspection, is referred to as a three-aisled basilica with a narthex and a main altar [21].
The monastery was almost completely destroyed in 1826, as it served as refuge and base during the Greek War of Independence (1821-1830) against the Ottoman Empire.The reconstruction works commenced soon after the liberation, in 1831, according to the plans made by the architect Andreas Gasparis Kalandros, an army lieutenant, and were completed by three Epirot masons by 1838.This is also the year of the construction of the wooden temple of the catholicon.A. Orlandos uses the term "hammered limestones" to describe the chosen building material used in this construction phase [17,21].
Between the years 1992-2014, the monastery was extensively renovated.On 29 January 2017, a devastating fire started due to a boiler explosion destroyed the largest part of the monastic cells' quarter [22].Thus today, the monastery cells are in a state of collapse and in need of major restoration and rebuilding (Figure2).

Visual Inspection
The external (Figure 2, Figure 3a) and the intermediate masonry (Figure 2, Figure 3d, and Figure 3e) of the cells' quarter belong to the 1831-1838 construction phase, referred to as historic masonries.It should be noted that, during the aforementioned construction phase, the intermediate masonry was, in fact, the masonry surrounding the internal courtyard and directly facing the Church.The historical masonries of this phase were constructed using two main lithotypes: a) a grey-beige limestone, which occasionally appears with black veins and b) sandstones of greenish to brownish shade.In some areas, a black compact stone has also been sporadically used.At certain areas of the intermediate masonry, relatively recent repointing seems to have taken place.
The internal masonry (Figure 2, Figure 3c, and Figure 3f), which faces the courtyard and the church today, was added during the major reconstruction that took place after 1992.This aims to improve residential functionality.This new restoration masonry, which is referred to as new masonry, was raised on an already existing base (19 th century construction phase).The building stone used for the construction of the interior masonry was a freshly-quarried grey-beige limestone, which greatly resembles the limestone used in the 19 th century construction phase masonries.

Visual Inspection
The external (Figure 2, Figure 3a) and the intermediate masonry (Figure 2, Figure 3d,e) of the cells' quarter belong to the 1831-1838 construction phase, referred to as historic masonries.It should be noted that, during the aforementioned construction phase, the intermediate masonry was, in fact, the masonry surrounding the internal courtyard and directly facing the Church.The historical masonries of this phase were constructed using two main lithotypes: a) a grey-beige limestone, which occasionally appears with black veins and b) sandstones of greenish to brownish shade.In some areas, a black compact stone has also been sporadically used.At certain areas of the intermediate masonry, relatively recent repointing seems to have taken place.
Heritage 2019, 2 1237 and Figure 3e).Its building materials present several damages and stone decay patterns such as color change, spalling, and flaking (Figure 4a).The western façade of this masonry (interior of domestic cells) was covered in plaster including remnants that still remain.iii) Finally, the new masonry was strongly affected by the fire on its western façade (the one facing the cells corridor).However, its eastern façade (the one facing the courtyard) seems to be unaffected (Figure 3f, Figure 4b).The internal masonry (Figure 2, Figure 3c,f), which faces the courtyard and the church today, was added during the major reconstruction that took place after 1992.This aims to improve residential functionality.This new restoration masonry, which is referred to as new masonry, was raised on an already existing base (19th century construction phase).The building stone used for the construction of the interior masonry was a freshly-quarried grey-beige limestone, which greatly resembles the limestone used in the 19th century construction phase masonries.
The visual inspection of the fire-exposed masonries allowed for the following observations: i.
The exterior façade of the external masonry (Figure 3a), which faces to the west, does not present any apparent damage from the fire.The interior plastered facade (Figure 3b) has clearly been affected, which displays blackened areas from the smoke produced during the fire, while partial plaster detachments can be noticed.Unfortunately, the total destruction of the wooden floors restricted access to these areas during this preliminary study.ii.
The historic intermediate masonry seems to have been severely affected by the fire (Figure 3d,e).Its building materials present several damages and stone decay patterns such as color change, spalling, and flaking (Figure 4a).The western façade of this masonry (interior of domestic cells) was covered in plaster including remnants that still remain.iii.
Finally, the new masonry was strongly affected by the fire on its western façade (the one facing the cells corridor).However, its eastern façade (the one facing the courtyard) seems to be unaffected (Figure 3f, Figure 4b).

Investigation Techniques and Methodology
A variety of techniques were used in the current study, which aim to evaluate the preservation state of the masonries and their building materials comprising them, after the effect of fire.Due to the different exposure of the building materials to the fire event, it was possible to select samples with a varying degree of fire damage, which is affected and not affected.This facilitated the evaluation of the fire effect on the examined building materials.
Analytical techniques were applied in the lab after sampling and were used in order to characterize the building materials and diagnose their decay due to the fire effect.Optical microscopy (OM) was employed for the petrographic characterization of the stone samples, using a ZEISS-AXIOSKOP 40 microscope, while a ProgRes-C14PLUS camera and ProgRes Capture Pro2.1 software were used for taking and editing microphotographs of the samples.Digital Microscopy (DM, i-scope, Moritex) was applied to examine the morphology and texture of the mortars under investigation.X-Ray Diffraction (XRD), using an Advanced D8 Diffractometer by Bruker, was applied for the identification of the crystalline compounds of selected stone and mortar samples, which aim to ascertain the mineralogical transformations due to the fire.Simultaneous Differential Thermal and Thermogravimetric Analysis (DTA/TG, Regulus 2500, Netzsch) was implemented on selected stone and mortar samples for the qualitative and quantitative determination of their compounds.The analyses were carried out at 30-1000 • C temperature range with a heating rate of 10 • C/min in a nitrogen atmosphere.Selected stone and mortar samples also underwent total water immersion tests [23], which aim to estimate the porosity accessible to water by total immersion for each sample, their water absorption capacity and apparent density, and, consequently, the alterations of these characteristics due to the fire effect.
In addition to the analytical techniques, non destructive techniques (NDTs) were applied in situ.In particular, Schmidt hammer rebound tests (SHR) were conducted on several building stones from various areas of the cell masonries in order to evaluate surface hardness of the various lithotypes [24][25][26] as well as its modification due to the fire effect.A Proceq N-type hammer (impact energy: 2.207 N m) was used, which followed the operation guidelines [27].An average of 10 impacts was performed on each of the examined building elements.All tests were performed with the hammer held perpendicular to the examined surface.For the statistical elaboration of the results, both the mean value (Rm) and the median value (RM) were calculated, while, in order to compare the dispersion of the measurements, the coefficient of variation (COV) was also estimated.
Infra-Red Thermography (IRT, B200, FLIR) was used to evaluate the preservation state of the masonry as a whole, by investigating representative areas [28][29][30].The passive approach implemented aimed to reveal any temperature gradations of the different building materials consisting of the masonry after the fire effect.
Heritage 2019, 2 1239 The methodological approach followed in this study is schematically represented in Figure 5.The evaluation was conducted on two levels: building elements scale and masonry scale.The evaluation on material level is necessary in order to succeed in the evaluation on the masonry level, since the individual materials comprise and, therefore, affect the overall performance of the masonry.
Heritage2019, 2 FOR PEER REVIEW 7 in its current condition (fire-affected).The evaluation on building material scale assists in the interpretation of the IRT results and, consequently, in the assessment of the overall preservation state of the masonry as a whole.
Figure 5. Diagram summarizing the methodological approach followed in this study.

Investigation of the Building Stones
The stone samples selected for in-lab examination are described in the following table (Table 1).The stone samples were collected from fire affected and seemingly unaffected areas of the masonry.The evaluation on building materials scale was conducted both in lab and in situ.The in lab evaluation aimed to reveal petrography and texture characteristics of the various building materials, their mineralogical and chemical composition, and physical characteristics, such as porosity, bulk density, and water uptake.In the present study, OM, DM, XRD, TG/DTA, and total water immersion tests were conducted in lab for the previously mentioned purposes.The in situ evaluation on building materials scale, aimed to estimate their surface hardness, using SHR.All the above measurements were applied on both fire-affected and seemingly unaffected stone elements in order to achieve a comparison of their properties' modification because of the fire event.In situ non destructive testing by IRT was used as a tool in order to evaluate the preservation state of the masonry (masonry scale) in its current condition (fire-affected).The evaluation on building material scale assists in the interpretation of the IRT results and, consequently, in the assessment of the overall preservation state of the masonry as a whole.

Investigation of the Building Stones
The stone samples selected for in-lab examination are described in the following table (Table 1).The stone samples were collected from fire affected and seemingly unaffected areas of the masonry.Grey-beige limestone from the new masonry (internal wall), which is a seemingly unaffected by the fire area.V7 Grey-beige limestone from the historic intermediate masonry, affected by the fire.V8 Grey-beige limestone from the new masonry (internal wall), affected by the fire.

V9
Limestone, with two distinct zones, one black and one grey-beige, the later similar to V7, unaffected by the fire (based on visual inspection).V10 Limestone, with two distinct zones (beige-gray and black), severely affected by fire.

Petrographic Examination of the Lithotypes
The petrographic examination was performed on selected samples from different areas of the historic and new masonries.Samples were collected from fire affected and non-affected masonry areas based on visual inspection, which aim to trace the heating impact on the mineralogical and micro-structural characteristics of the different lithotypes.
One of the main building stones used in the historic masonries of 1831 (second most abundant stone type used in the monument) is a clastic calcite sandstone consisting of crystalline and lithic fragments.The sandstone sample V1 was not affected by the fire, based on the visual inspection (Figure 6a).According to the petrographic examination (Figure 6b), the crystalline fragments include quartz SiO 2 , feldspars [albite (NaAlSi 3 O 8 ), and microcline (KAlSi 3 O 8 )], calcite CaCO 3 , muscovite folia [indicative formula: KAl 2 (AlSi 3 O 10 )(F,OH) 2 ], and grains of iron and zirconium oxides/hydroxides.The lithic fraction consists of quartzite, limestone, slate, serpentine, and sub-volcanic rock fragments.The cementing material of the clasts is of sparitic calcite nature.V2 is a sandstone sample of a fire-affected area of the historic masonry (Figure 6c).The petrographic results depict oxidation phenomena of iron-containing minerals.This is macroscopically manifested by the reddening of the sample.

Heritage2019, 2 FOR PEER REVIEW 8
The petrographic examination was performed on selected samples from different areas of the historic and new masonries.Samples were collected from fire affected and non-affected masonry areas based on visual inspection, which aim to trace the heating impact on the mineralogical and micro-structural characteristics of the different lithotypes.
One of the main building stones used in the historic masonries of 1831 (second most abundant stone type used in the monument) is a clastic calcite sandstone consisting of crystalline and lithic fragments.The sandstone sample V1 was not affected by the fire, based on the visual inspection (Figure6a).According to the petrographic examination (Figure 6b), the crystalline fragments include quartz SiO2, feldspars [albite (NaAlSi3O8), and microcline (KAlSi3O8)], calcite CaCO3, muscovite folia [indicative formula: KAl2(AlSi3O10)(F,OH)2], and grains of iron and zirconium oxides/hydroxides.The lithic fraction consists of quartzite, limestone, slate, serpentine, and sub-volcanic rock fragments.The cementing material of the clasts is of sparitic calcite nature.V2 is a sandstone sample of a fire-affected area of the historic masonry (Figure 6c).The petrographic results depict oxidation phenomena of iron-containing minerals.This is macroscopically manifested by the reddening of the sample.A compact black stone detected on some areas of the historic masonry is a chert (Figure7a, sample V5).This stone type is sporadically detected in the historic masonries.It was collected from a severely fire-affected area of the intermediate masonry.The stone consists of several zones.In Figure7b, three zones are discerned downwards: a) the upper fossiliferous limestone comprising sparitic fossils (mostly foraminiferal species) bound to a micritic mass, b) the intermediate zone of large rhomboid dolomite [CaMg(CO3)2] crystals,and c) the chert zone consisting of amorphous siliceous material and scattered dolomite crystals.Likewise, in Figure 7c, there is an additional zone where intense diffusion of iron hydroxides is distinguished (dark brown area, Figure 7c).This A compact black stone detected on some areas of the historic masonry is a chert (Figure 7a, sample V5).This stone type is sporadically detected in the historic masonries.It was collected from a severely fire-affected area of the intermediate masonry.The stone consists of several zones.In Figure 7b, three zones are discerned downwards: a) the upper fossiliferous limestone comprising sparitic fossils (mostly foraminiferal species) bound to a micritic mass, b) the intermediate zone of large rhomboid dolomite [CaMg(CO 3 ) 2 ] crystals, and c) the chert zone consisting of amorphous siliceous material and scattered dolomite crystals.Likewise, in Figure 7c, there is an additional zone where intense diffusion of iron hydroxides is distinguished (dark brown area, Figure 7c).This phenomenon is evident in the fossiliferous limestone zone (Figure 7f).The chert zone is depicted in Figure 7d-e where joints filled with carbonate material and super fine-grained iron pyrite crystals are observed.The limestone used in the new masonry (internal wall, 1992 reconstruction) is a grey-beige biomicritic limestone (sample V6, visually fire non-affected, Figure 8a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 8b).The new masonry is comprised solely of the grey-beige biomicritic limestone (V6).Sample V8 was also collected from the new masonry from an area highly affected by the fire (Figure 9a), as indicated, not only from the location of the sample, but from its pinkish hue as well.This is confirmed by optical microscopy, as V8 presents similar characteristics to sample V6 (Figure 9b).However, the effect of the fire is evident through the widening and rupture of the joints filled with secondary The limestone used in the new masonry (internal wall, 1992 reconstruction) is a grey-beige biomicritic limestone (sample V6, visually fire non-affected, Figure 8a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 8b).The limestone used in the new masonry (internal wall, 1992 reconstruction) is a grey-beige biomicritic limestone (sample V6, visually fire non-affected, Figure 8a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 8b).The new masonry is comprised solely of the grey-beige biomicritic limestone (V6).Sample V8 was also collected from the new masonry from an area highly affected by the fire (Figure 9a), as indicated, not only from the location of the sample, but from its pinkish hue as well.This is confirmed by optical microscopy, as V8 presents similar characteristics to sample V6 (Figure 9b).However, the effect of the fire is evident through the widening and rupture of the joints filled with secondary The new masonry is comprised solely of the grey-beige biomicritic limestone (V6).Sample V8 was also collected from the new masonry from an area highly affected by the fire (Figure 9a), as indicated, not only from the location of the sample, but from its pinkish hue as well.This is confirmed by optical microscopy, as V8 presents similar characteristics to sample V6 (Figure 9b).However, the effect of the fire is evident through the widening and rupture of the joints filled with secondary calcite, which is an effect commonly observed in limestones when exposed to extreme temperatures (Figure 9c).
Heritage2019, 2 FOR PEER REVIEW 10 calcite, which is an effect commonly observed in limestones when exposed to extreme temperatures (Figure 9c).One of the main construction materials of the historic masonry is a grey-beige micritic fossiliferous limestone.Sample V7 was collected from a severely damaged area of the intermediate masonry, which was clearly affected by the fire (Figure 10a).This damaged historical stone, as expected, presents similar petrographic characteristics to the damaged limestone collected from the new masonry (V8), which confirms macroscopic observations.Joint ruptures are also evident.However, they present a larger width, ranging from 35μm to 65μm (Figure 10b, Figure 10c).In both fire-affected samples of the grey-beige fossiliferous limestone (V8 from new masonry, V7 from historic masonry), stylolites are detected, while iron hydroxides and clay minerals seem to have intruded into their mass.In parallel, as previously mentioned, both samples present a distinct pinkish color.The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figure 9b, Figure 10b, and Figure 10c).Generally, the reddening of limestones due to the oxidation of iron compounds begins at 250-300 °C, but may not be evident before the 400 °C when the color change becomes more intense [10,31].This discoloration serves as an indication of the minimum temperature range reached during the fire in this area.
Sample V9 was collected from the historic intermediate masonry, and visual inspection indicated that it was not affected by the fire.Macroscopically, the lithotype presents two distinct zones of different coloration (black and grey-beige, Figure11a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 11b).The grey- One of the main construction materials of the historic masonry is a grey-beige micritic fossiliferous limestone.Sample V7 was collected from a severely damaged area of the intermediate masonry, which was clearly affected by the fire (Figure 10a).This damaged historical stone, as expected, presents similar petrographic characteristics to the damaged limestone collected from the new masonry (V8), which confirms macroscopic observations.Joint ruptures are also evident.However, they present a larger width, ranging from 35 µm to 65 µm (Figure 10b,c).
Heritage2019, 2 FOR PEER REVIEW 10 calcite, which is an effect commonly observed in limestones when exposed to extreme temperatures (Figure 9c).One of the main construction materials of the historic masonry is a grey-beige micritic fossiliferous limestone.Sample V7 was collected from a severely damaged area of the intermediate masonry, which was clearly affected by the fire (Figure 10a).This damaged historical stone, as expected, presents similar petrographic characteristics to the damaged limestone collected from the new masonry (V8), which confirms macroscopic observations.Joint ruptures are also evident.However, they present a larger width, ranging from 35μm to 65μm (Figure 10b, Figure 10c).In both fire-affected samples of the grey-beige fossiliferous limestone (V8 from new masonry, V7 from historic masonry), stylolites are detected, while iron hydroxides and clay minerals seem to have intruded into their mass.In parallel, as previously mentioned, both samples present a distinct pinkish color.The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figure 9b, Figure 10b, and Figure 10c).Generally, the reddening of limestones due to the oxidation of iron compounds begins at 250-300 °C, but may not be evident before the 400 °C when the color change becomes more intense [10,31].This discoloration serves as an indication of the minimum temperature range reached during the fire in this area.
Sample V9 was collected from the historic intermediate masonry, and visual inspection indicated that it was not affected by the fire.Macroscopically, the lithotype presents two distinct zones of different coloration (black and grey-beige, Figure11a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 11b).The grey- In both fire-affected samples of the grey-beige fossiliferous limestone (V8 from new masonry, V7 from historic masonry), stylolites are detected, while iron hydroxides and clay minerals seem to have intruded into their mass.In parallel, as previously mentioned, both samples present a distinct pinkish color.The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figure 9b, Figure 10b,c).Generally, the reddening of limestones due to the oxidation of iron compounds begins at 250-300 • C, but may not be evident before the 400 • C when the color change becomes more intense [10,31].This discoloration serves as an indication of the minimum temperature range reached during the fire in this area.
Heritage 2019, 2 1243 Sample V9 was collected from the historic intermediate masonry, and visual inspection indicated that it was not affected by the fire.Macroscopically, the lithotype presents two distinct zones of different coloration (black and grey-beige, Figure 11a).The matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (Figure 11b).The grey-beige biomicritic limestone is accompanied by laminae of a black-grey fossiliferous limestone comprising foraminiferal species of sparitic texture bound to a micritic mass.Oxidized grains of ferrous minerals are, also, detected (Figure 11c).
Heritage2019, 2 FOR PEER REVIEW 11 comprising foraminiferal species of sparitic texture bound to a micritic mass.Oxidized grains of ferrous minerals are, also, detected (Figure 11c).Based on visual inspection, a fire-affected sample of the above-described lithotype from the historic intermediate masonry was, also, examined (Figure 12, Sample V10).The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figures12 a, 12b, and 12c), as also noticed in samples V8 and V7.The capillary rupture observed in the stone mass constitutes a microstructural change, as an additional result of the fire impact on the beige-grey limestone zone.The black-grey limestone zone does not present any significant difference from the V9 sample, which was not affected by the fire.

Mineralogical Examination of the lithotypes through X-ray Diffraction
Mineralogical examination was conducted only on samples of the main building stones of historic and new masonries, sandstone samples V1, V2, and limestone samples V6, V7, and V8.The lithotypes were pulverized and studied through X-ray diffraction.The results are summarized in Table 2.
Regarding the green sandstone, both unaffected and affected samples (V1 and V2, respectively) present similar mineralogical composition, with quartz as the principal mineralogical component and calcite, albite, muscovite, and chlorite as accessory mineralogical components.However, in sample V1, microcline is detected, while, in sample V2, it is not detected.This is in accordance to other studies that have demonstrated that microcline does decrease as the temperature of the stone increases [32].
Regarding the beige-grey limestone, the only lithotype used in the new masonry and the most Based on visual inspection, a fire-affected sample of the above-described lithotype from the historic intermediate masonry was, also, examined (Figure 12, Sample V10).The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figure 12a-c), as also noticed in samples V8 and V7.The capillary rupture observed in the stone mass constitutes a micro-structural change, as an additional result of the fire impact on the beige-grey limestone zone.The black-grey limestone zone does not present any significant difference from the V9 sample, which was not affected by the fire.
Heritage2019, 2 FOR PEER REVIEW 11 comprising foraminiferal species of sparitic texture bound to a micritic mass.Oxidized grains of ferrous minerals are, also, detected (Figure 11c).Based on visual inspection, a fire-affected sample of the above-described lithotype from the historic intermediate masonry was, also, examined (Figure 12, Sample V10).The visual reddening of the stone is attributed to the oxidation of ferrous minerals and the diffusion of iron hydroxides due to the high temperatures developed during the burning event (Figures12 a, 12b, and 12c), as also noticed in samples V8 and V7.The capillary rupture observed in the stone mass constitutes a microstructural change, as an additional result of the fire impact on the beige-grey limestone zone.The black-grey limestone zone does not present any significant difference from the V9 sample, which was not affected by the fire.

Mineralogical Examination of the lithotypes through X-ray Diffraction
Mineralogical examination was conducted only on samples of the main building stones of historic and new masonries, sandstone samples V1, V2, and limestone samples V6, V7, and V8.The lithotypes were pulverized and studied through X-ray diffraction.The results are summarized in Table 2.
Regarding the green sandstone, both unaffected and affected samples (V1 and V2, respectively) present similar mineralogical composition, with quartz as the principal mineralogical component and calcite, albite, muscovite, and chlorite as accessory mineralogical components.However, in sample V1, microcline is detected, while, in sample V2, it is not detected.This is in accordance to other studies that have demonstrated that microcline does decrease as the temperature of the stone increases [32].
Regarding the beige-grey limestone, the only lithotype used in the new masonry and the most dominant in the historic ones, no alterations are noticed in relation to mineralogical composition

Mineralogical Examination of the lithotypes through X-ray Diffraction
Mineralogical examination was conducted only on samples of the main building stones of historic and new masonries, sandstone samples V1, V2, and limestone samples V6, V7, and V8.The lithotypes were pulverized and studied through X-ray diffraction.The results are summarized in Table 2.
Regarding the green sandstone, both unaffected and affected samples (V1 and V2, respectively) present similar mineralogical composition, with quartz as the principal mineralogical component and calcite, albite, muscovite, and chlorite as accessory mineralogical components.However, in sample V1, microcline is detected, while, in sample V2, it is not detected.This is in accordance to other studies that have demonstrated that microcline does decrease as the temperature of the stone increases [32].Regarding the beige-grey limestone, the only lithotype used in the new masonry and the most dominant in the historic ones, no alterations are noticed in relation to mineralogical composition between the unaffected (V6) and the affected by the fire samples, from both the new (V8) and the historic masonry (V7).Thus, the beige-gray limestone presents calcite as its principal mineralogical component and quartz as an accessory.

Compositional analysis of stone samples through simultaneous thermal analysis (TG/DTA)
The previously mentioned stone samples (V1, V2, V6-V8) were also examined through simultaneous thermal analysis, which aim to reveal modifications in their chemical composition due to the fire.The results are presented in Table 3, which report the mass loss (%) measured in specific temperature ranges.The unaffected sandstone sample V1 presents distinct differences in relation to the affected ones by the fire sandstone sample V2.In particular, sample V2 presents a higher amount of physically bound water in comparison to V1 (increased mass loss in temperature range 30-120 • C), which indicates a modification in the microstructure that increases water uptake from the environment after the effect of the fire.In addition, the mass loss above 600 • C, which is connected to the decomposition of carbonate compounds, is also distinctly different.The affected sample V2 presents a much lower carbonate content indicating that the calcite binding material of the matrix of the sandstone was reduced due to the fire, which confirms OM observations.It should be noted that, in the DTA curve, the distinct endothermic peak connected to quartz transition from α→β is noticed at ~575 • C.Although the carbonate compounds' decomposition endothermic peak is clear in the unaffected sample (~770 • C), it is not discernable in the fire-affected sample V2.
The beige-grey limestone of the historic and new masonries (V6-V8) seems to be unaffected by the fire in relation to its chemical composition.All samples present similar mass losses in all temperature ranges, which is independent of the fire effect.This confirms XRD results as well.The decomposition temperature of the carbonate compounds was detected above 800 • C.

Total Immersion Results on Stone Lithotypes
Total immersion was conducted on the stone samples, which aim to evaluate their porosity (%) accessible to water through total immersion.Water Absorption Capacity (WAC%) was calculated, Heritage 2019, 2 1245 while the apparent density of the samples was calculated as well.The results are summarized in Table 4.The characteristics of the unaffected and fire-affected sandstone samples display diverse values, which confirm a visual inspection observation regarding their state.In particular, the affected sample, V2, presented a higher porosity (~6% in relation to 3.7%), which indicates the creation of pores and micro-cracks.This alteration is consistent with the different mass loss values demonstrated by TG measurements in temperatures above 600 • C. Bulk density is slightly decreased from 2.4 g/cm 3 to 2.2 g/cm 3 due to the porosity increase and transformation, which take place on a mineralogical and chemical level.The water absorption capacity of the sandstone increases after the fire-event, as expected.The later statement is also evident through the higher mass loss detected for the affected stone through TG attributed to physically bound water (mass loss <120 • C).
The beige-grey limestone, on the other hand, seems not to be affected in relation to its physical characteristics, which is also noticed in the mineralogical and thermal analysis results.Porosity of the unaffected limestone (V6) and the fire-affected one (V8), from the new masonry, is very close (2.6% and 2.1%, respectively).Bulk density values are identical (2.3 g/cm 3 ), while water absorption capacity of the affected and non-affected samples are also extremely close (1.1%, 0.9%).The fire-affected limestone sample from the historic intermediate masonry (V7) also presents similar values to the previously mentioned samples, as expected since they are of the same lithotype.Its slightly higher porosity (2.9%) could be attributed to ageing processes in addition to the fire effect.The same is true for the slightly lower bulk density that it exhibits (2.1 g/cm 3 ) in relation to the new masonry fire-affected limestone V8 (2.3 g/cm 3 ), as well as the slightly higher water absorption capacity it presents (1.4% in relation to 0.9%).

Investigation of the Mortars
Mortar samples were collected from both the historic intermediate masonry and the new masonry.The mortar samples' description, along with characteristic digital microscopy images depicting their surface texture, are presented in Table 5.
Table 5. Description of the selected mortar samples from the cells' quarter.

Vm1
Structural soft mortar of clay texture and light-orange hue with blackened external surface due to the smoke deposition-upper part of the historical intermediate masonry (above 2 m).
for the slightly lower bulk density that it exhibits (2.1 g/cm ) in relation to the new masonry fireaffected limestone V8 (2.3g/cm 3 ), as well as the slightly higher water absorption capacity it presents (1.4% in relation to 0.9%).

Investigation of the Mortars
Mortar samples were collected from both the historic intermediate masonry and the new masonry.The mortar samples' description, along with characteristic digital microscopy images depicting their surface texture, are presented in Table5.

Vm1
Structural soft mortar of clay texture and light-orange hue with blackened external surface due to the smoke deposition-upper part of the historical intermediate masonry (above 2m).

Vm2
Joint mortar of cementitious texture from a severely fire-affected area from the middle part of the new masonry (~1.5m).

Vm2
Joint mortar of cementitious texture from a severely fire-affected area from the middle part of the new masonry (~1.5 m).

Vm6
In-depth mortar of mixed cementitious and clay texture from a severely fire-affected area at the lower part of the historical intermediate masonry (<1m).

Vm6
In-depth mortar of mixed cementitious and clay texture from a severely fire-affected area at the lower part of the historical intermediate masonry (<1 m).mass loss observed in the <120 • C temperature range is due to the loss of physically bound water (H 2 O PBW ), (ii) the mass loss detected in the range 120-200 • C is attributed to the loss of the crystalline water of salts (e.g., gypsum), (iii) the mass loss observed in the temperature range 200-600 • C is attributed to chemically-bound water (H 2 0 SWB ) (e.g., dehydroxylation of clay minerals, dehydration of aluminosilicates, or calcium aluminosilicate phases etc.), (iv) the mass loss detected in the range >600 • C is attributed to the decomposition of carbonates and consequent CO 2 loss [33].The inverse hydraulicity index is calculated as the ratio CO 2 /H 2 0 SWB and is widely used in order to evaluate the hydraulicity of a mortar (lower inverse hydraulicity indexes are indicative of more hydraulic mortars) [34].All samples present mass losses attributed to physically bound water between 1% and 1.5%, except for the cementitious textured mortar Vm2, which presents 0.54%.They also present low mass losses in the temperature range of 120 to 200 • C, which indicates extremely low percentages of crystalline water bound to hygroscopic salts.Chemically bound water presents dispersion among the mortar samples ranging from 1.49% to 3.11% for the cementitious-textured mortars, and 2.84% to 4.32% for the clayey textured mortars.Sample Vm6, which is of a mixed texture, presents a water percentage higher than the cementitious-textured mortars and within the range of the clayey textured mortars.All cementitious-textured mortars present relatively high mass losses attributed to the loss of CO 2 due to the decomposition of carbonate materials (ranging from 18.57% to 20.93%), while all clayey textured mortars present lower mass losses in the previously mentioned range (ranging from 6.62% to 8.41%).Sample Vm6, of a mixed texture, presents a CO 2 mass loss value intermediate of the cementitious and clayey textured mortars.The mass loss values attributed to CO 2 loss also indicate the siliceous and mixed carbonate and siliceous nature of the aggregates of all mortars investigated.However, the CO 2 /H 2 O CBW ratio is used to determine whether a mortar is of hydraulic nature.In the present study, it is used, in addition to the mass loss attributed to the decomposition of carbonates above 600 • C, to discriminate clay mortars from cement mortars aimed to ascertain their nature (Figure 13).It is clear that the "clayey" mortars (Vm1, Vm3, Vm4, Vm5 and Vm8) are all grouped in a very tight area, while the "cement textured" mortars are also grouped, but with a wider distribution.The mixed-textured sample, Vm6, falls between the two groups, in closer vicinity to the cement textured mortars.The thermal analysis results indicate that there are two types of mortar in the masonry, namely clay mortars and cement-based mortars.The thermal analysis results, in combination with the mineralogical analysis, indicate relatively high carbonation of the cement-based mortars, especially in the case of Vm2, which was located in the middle part of the new masonry.

Total Immersion Results on Mortar Samples
Total water immersion tests were conducted on selected mortar samples.Since it was not possible to conduct these measurements on all mortar samples, due to their poor state of preservation and consequent dissolution in water, measurements were only conducted on samples Vm2, Vm9 (cement-based mortars), and sample Vm4 (clay mortar).The results are summarized in the following table (Table 8).The clay mortar (V4) presents the highest porosity accessible to water (31.18%), as expected for a mortar of this category.The cement mortars present relatively high porosity values of 17% and 22% for samples Vm2 and Vm9, respectively.However, this is distinctly lower than the clay mortar.Their porosity values, in addition to thermal analysis results, confirm a high level of carbonation, which is probably due to the fire effect and the consequent microstructure alteration.The water absorption capacity of the clay mortar is the highest among the examined samples (25.38%), while the cement mortars present similar values (14.33% and 17.15%).Regarding bulk density, the cement mortars Vm2 and Vm9 present values very low for cement mortars, which is clearly due to their poor state of preservation (1.45 g/cm 3 and 1.34 g/cm 3 ) because of the fire effect.This result can also be attributed to a mixed cement-lime composition of the cement-based mortars (which present lower bulk densities than cement mortars) without diminishing the destructive role of the fire event.Vm 4, which is the clay mortar examined, presents a bulk density of 1.63g/cm 3 .This is an intermediate value for historic mortars.

Total Immersion Results on Mortar Samples
Total water immersion tests were conducted on selected mortar samples.Since it was not possible to conduct these measurements on all mortar samples, due to their poor state of preservation and consequent dissolution in water, measurements were only conducted on samples Vm2, Vm9 (cement-based mortars), and sample Vm4 (clay mortar).The results are summarized in the following table (Table 8).The clay mortar (V4) presents the highest porosity accessible to water (31.18%), as expected for a mortar of this category.The cement mortars present relatively high porosity values of 17% and 22% for samples Vm2 and Vm9, respectively.However, this is distinctly lower than the clay mortar.Their porosity values, in addition to thermal analysis results, confirm a high level of carbonation, which is probably due to the fire effect and the consequent microstructure alteration.The water absorption capacity of the clay mortar is the highest among the examined samples (25.38%), while the cement mortars present similar values (14.33% and 17.15%).Regarding bulk density, the cement mortars Vm2 and Vm9 present values very low for cement mortars, which is clearly due to their poor state of preservation (1.45 g/cm 3 and 1.34 g/cm 3 ) because of the fire effect.This result can also be attributed to a mixed cement-lime composition of the cement-based mortars (which present lower bulk densities than cement mortars) without diminishing the destructive role of the fire event.Vm 4, which is the clay mortar examined, presents a bulk density of 1.63g/cm 3 .This is an intermediate value for historic mortars.

SHR Results
AREA 1 (Figure 14) is the area left of the entrance to the Monastery and is mainly comprised of the beige-grey limestone and the sandstone.The results from the SHR measurements are presented in Table 9.As already mentioned, this part of the masonry belongs to the historical phase of 1831-1838 and is seemingly unaffected by the fire.The highest Rebound value corresponds to the black chert, which is found as an inclusion inside the limestone in this area.The grey-beige limestone presents higher surface hardness index values than the sandstone examined.

SHR Results
AREA 1 (Figure 14) is the area left of the entrance to the Monastery and is mainly comprised of the beige-grey limestone and the sandstone.The results from the SHR measurements are presented in Table 9.As already mentioned, this part of the masonry belongs to the historical phase of 1831-1838 and is seemingly unaffected by the fire.The highest Rebound value corresponds to the black chert, which is found as an inclusion inside the limestone in this area.The grey-beige limestone presents higher surface hardness index values than the sandstone examined.15a and 15b).This area was completely affected by the fire burning and presents the most intense deterioration patterns, such as extreme scaling of the beige-grey limestone and exfoliation of the sandstones.The black chert was also examined (Figure 15a, sub-area 2).This latter type of stone seems macroscopically less affected by the fire, but presents a SHR value decrease close to 50% compared to the value from the fire unaffected masonry (Figure 14-AREA 1, sub-area 3).In both zones, the beige-grey limestone presents the lower Rebound values compared to the green sandstone, which indicates a higher deterioration level due to the fire event (Table 10).The eastern façade of the intermediate historic masonry (AREA 2) was investigated after being divided per height in two areas: below 50 cm and above 1 m (Figures 15a and 15b).This area was completely affected by the fire burning and presents the most intense deterioration patterns, such as extreme scaling of the beige-grey limestone and exfoliation of the sandstones.The black chert was also examined (Figure 15a, sub-area 2).This latter type of stone seems macroscopically less affected by the fire, but presents a SHR value decrease close to 50% compared to the value from the fire unaffected masonry (Figure 14-AREA 1, sub-area 3).In both zones, the beige-grey limestone presents the lower Rebound values compared to the green sandstone, which indicates a higher deterioration level due to the fire event (Table 10)..17In order to further estimate the fire impact on the grey compact limestone, a wall pillar from the new masonry (northern façade, from interior to exterior) was examined (Figure 2 and Figure 3f).This part of the masonry was constructed between the years 1992 to 2014.The 2017's fire event left intact the exterior façade of the masonry (eastern façade, the one facing the courtyard) while intense fire effects are observed at the interior (western) façade, such as discoloration, scaling, and detachments.The area under examination, depicted in Figure 17, was divided into zones for the SHR measurements to be carried out.a) a fire-affected zone (FAZ), according to visual inspection with a total length of approximately 8 cm, where a burnt front, facing west (interior façade), and a burnt zone, facing north, are evident.b) A potentially fire unaffected zone (FUZ), which was further examined both in the middle and in the outer side of each stone block, and c) an in-between zone of ~10 cm length.The total width of the wall is 51 cm, while the SHR measurements were conducted in a height of six stone arrays (total height around 60 cm).The results are presented in Table 12.A progressive decline in the Rebound values is observed.The most affected area i.e. the FAZ burnt front presents an approximate loss of SHR hardness value of 52%-58% compared to the macroscopically perceived sound zones.The SHR values of the beige-grey limestone, which are visually perceived as fire unaffected zones, are similar to the ones received from the fire unaffected AREA 1 (Figure 14, Table 9).In order to further estimate the fire impact on the grey compact limestone, a wall pillar from the new masonry (northern façade, from interior to exterior) was examined (Figures 2 and 3f).
This part of the masonry was constructed between the years 1992 to 2014.The 2017's fire event left intact the exterior façade of the masonry (eastern façade, the one facing the courtyard) while intense fire effects are observed at the interior (western) façade, such as discoloration, scaling, and detachments.The area under examination, depicted in Figure 17, was divided into zones for the SHR measurements to be carried out.a) a fire-affected zone (FAZ), according to visual inspection with a total length of approximately 8 cm, where a burnt front, facing west (interior façade), and a burnt zone, facing north, are evident.b) A potentially fire unaffected zone (FUZ), which was further examined both in the middle and in the outer side of each stone block, and c) an in-between zone of ~10 cm length.The total width of the wall is 51 cm, while the SHR measurements were conducted in a height of six stone arrays (total height around 60 cm).The results are presented in Table 12.A progressive decline in the Rebound values is observed.The most affected area i.e. the FAZ burnt front presents an approximate loss of SHR hardness value of 52%-58% compared to the macroscopically perceived sound zones.The SHR values of the beige-grey limestone, which are visually perceived as fire unaffected zones, are similar to the ones received from the fire unaffected AREA 1 (Figure 14, Table 9).

IRT Inspection
IRT investigation took place on several parts of the new and the historical masonry, and some characteristic results are presented below.
The higher masonry part of the new masonry (above 1m) presents lower temperature readings compared to the lower masonry part, as well as an intermediate temperature distribution width of 3 °C (from 23 °C to 27 °C), (Figure 18a-18d).Regarding the lower masonry part, the lower stone zone presents higher temperatures (Figures 18c and 18d, zone under the dotted line) compared to the upper zone (Figure 18c, 18d, zone above the dotted line), as well as a tighter temperature distribution width of 2 °C (from 26 °C to 28 °C), whereas the upper zone displays a temperature distribution width of 4 °C (from 23.5 °C to 27.5°C ).
It can be assumed by the 2 IRT images' co-evaluation that the new masonry presents different temperature zones height-wise.In particular, lower masonry parts display higher temperature readings compared to the upper masonry parts.This indicates a difference of the fire effect on the new masonry stone blocks, according to their height and position, even though a precise pattern is not demonstrated.

IRT Inspection
IRT investigation took place on several parts of the new and the historical masonry, and some characteristic results are presented below.
The higher masonry part of the new masonry (above 1m) presents lower temperature readings compared to the lower masonry part, as well as an intermediate temperature distribution width of 3 • C (from 23 • C to 27 • C), (Figure 18a-d).Regarding the lower masonry part, the lower stone zone presents higher temperatures (Figure 18c,d    The application of IRT at higher historic masonry parts (above 2m) display lower temperature readings compared to the lower masonry parts (Figure 20).The wooden element in the middle of the IRT image presents temperatures up to 25.5°C , while the masonry parts above and below it reach up to 26.8 °C .The temperature distribution width of the masonry, except the wooden element, is about 4.5 °C .Thus, it is demonstrated that the historic masonry holds a similar pattern with the new one, as far as it concerns temperature distribution.The upper masonry parts display lower temperatures when compared to the lower parts.It can be assumed by the 2 IRT images' co-evaluation that the new masonry presents different temperature zones height-wise.In particular, lower masonry parts display higher temperature readings compared to the upper masonry parts.This indicates a difference of the fire effect on the new masonry stone blocks, according to their height and position, even though a precise pattern is not demonstrated.
IRT investigation of the intermediate historical masonry shows temperature variations among the different stone types examined (Figure 19a  IRT investigation of the intermediate historical masonry shows temperature variations among the different stone types examined (Figures 19a and 19b), which are attributed to the different degree of the surface detachment/scaling due to the fire effect.The intermediate historical masonry presents a wide temperature distribution width of 4.5 °C (from 22.5 °C to 27 °C ).The application of IRT at higher historic masonry parts (above 2m) display lower temperature readings compared to the lower masonry parts (Figure 20).The wooden element in the middle of the IRT image presents temperatures up to 25.5°C , while the masonry parts above and below it reach up to 26.8 °C .The temperature distribution width of the masonry, except the wooden element, is about 4.5 °C .Thus, it is demonstrated that the historic masonry holds a similar pattern with the new one, The application of IRT at higher historic masonry parts (above 2 m) display lower temperature readings compared to the lower masonry parts (Figure 20).The wooden element in the middle of the IRT image presents temperatures up to 25.5 • C, while the masonry parts above and below it reach up to 26.8 • C. The temperature distribution width of the masonry, except the wooden element, is about 4.5 • C. Thus, it is demonstrated that the historic masonry holds a similar pattern with the new one, as far as it concerns temperature distribution.The upper masonry parts display lower temperatures when compared to the lower parts.

Conclusions
During this preliminary study, the characterization of the different lithotypes and mortars used in the different architectural phases of Varnakova Monastery took place.The petrographic examination proved to be an indispensable tool for characterization and the fire impact assessment on the different lithotypes of the historic structure.The main building stones of the historic masonries are a beige-grey fosilliferrous biomicritic limestone, as well as a clastic calcite sandstone, consisting of crystalline and lithic fragments.Other stones are also sporadically detected, such as a black chert and a black fossiliferous limestone, which appears as laminae of the beige-grey fosilliferrous biomicritic limestone.
Regarding the main building stones, the petrographic examination of the fire-affected sandstone shows oxidation phenomena of iron-containing minerals due to the fire, which is macroscopically

Conclusions
During this preliminary study, the characterization of the different lithotypes and mortars used in the different architectural phases of Varnakova Monastery took place.The petrographic examination proved to be an indispensable tool for characterization and the fire impact assessment on the different lithotypes of the historic structure.The main building stones of the historic masonries are a beige-grey fosilliferrous biomicritic limestone, as well as a clastic calcite sandstone, consisting of crystalline and lithic fragments.Other stones are also sporadically detected, such as a black chert and a black fossiliferous limestone, which appears as laminae of the beige-grey fosilliferrous biomicritic limestone.
Regarding the main building stones, the petrographic examination of the fire-affected sandstone shows oxidation phenomena of iron-containing minerals due to the fire, which is macroscopically

Conclusions
During this preliminary study, the characterization of the different lithotypes and mortars used in the different architectural phases of Varnakova Monastery took place.The petrographic examination proved to be an indispensable tool for characterization and the fire impact assessment on the different lithotypes of the historic structure.The main building stones of the historic masonries are a beige-grey fosilliferrous biomicritic limestone, as well as a clastic calcite sandstone, consisting of crystalline and lithic fragments.Other stones are also sporadically detected, such as a black chert and a black fossiliferous limestone, which appears as laminae of the beige-grey fosilliferrous biomicritic limestone.
Regarding the main building stones, the petrographic examination of the fire-affected sandstone shows oxidation phenomena of iron-containing minerals due to the fire, which is macroscopically manifested by the reddening of the sample.While the fire-affected beige-grey limestone presents a pinkish hue macroscopically, due to the effect of the fire, the fire-effect is also evident through the widening and rupture of the joints filled with secondary calcite.The latter is more intense in the case of the limestone collected from the historical masonry.
Both XRD and thermal analysis measurements indicated distinct alterations of the sandstone due to the effect of fire.The microcline peak detected in the unaffected sample is not discerned in the fire-affected sample, while the calcite content also decreased.Physical properties of the sandstone are also altered.The effect of fire has increased porosity, decreased bulk density, and increased water absorption capacity.SHR values conducted in situ on a large number of sandstone building elements, both affected and unaffected, showed a decrease of surface hardness, as expected, in accordance with the degree of the fire exposure.
On the other hand, the limestone samples do not present distinct differences in their mineralogical, chemical, or physical properties due to the fire effect.However, the SHR evaluation reveals that, although relatively stable in the terms mentioned above, the effect of fire and the rupturing of the limestone's joints filled with secondary calcite are quantitatively evident in the decreased SHR values and, therefore, the decreased surface hardness.Further research is necessary in order to ascertain whether the mechanical strength values and especially compressive strength has also decreased, as expected.This highlights the need for further sampling to obtain samples of adequate geometry and dimensions in order to accomplish mechanical strength measurements.Such a sampling campaign requires further authorization, as the Monastery is a listed historical monument and is under a strict sampling legislation.
The mortars selected from the new masonry are classified as cement-based mortars, a fact which is anticipated in a recently constructed masonry.The thermal analysis and microstructure evaluation results demonstrate that these mortars are highly carbonated due to the fire effect.The mortars selected from the intermediate historical masonry belong to two categories: clay mortars and cement-based mortars.All structural mortars belong to the clay mortars category, while the final joint mortars belong to the cement-based category, which demonstrate that recent repointing had taken place using a cement-based mortar, prior to the fire event.Digital microscopy observations regarding the texture of the mortars proved to be a useful tool for an initial classification.
IRT inspection of the masonries as a whole, demonstrates that the historic masonry presents relatively high temperature variations, due to the presence of diverse lithotypes, as well as the different degree of the fire effect.Similar fluctuation of temperatures is observed for the new masonry as well, despite the fact that it is entirely built from one lithotype (namely the grey-beige limestone) and can be attributed to the fire event.
Both historical and new masonries present different temperature zones with their upper parts being cooler than the lower ones.This is an indication of the different effect of the fire per height.However, even though the fire effect seems to depend on position, height, and lithotype, no clear pattern is displayed.
Blackened surfaces, in both the historical and new masonries, present higher temperatures, which indicate differences in the thermo-hygric behavior of the masonry in these areas, due to soot accumulation from the fire, as well as a possible stronger fire damaging effect.
It is evident from the IRT results that the historical masonry presents wider temperature distribution width in comparison to the new masonry.However, the recorded temperature readings of the historical masonry are lower in comparison to the ones of the new masonry.These differences are attributed to the differentiated development of the fire event, as well as to the fire's different effect on the historical masonry, due to the variety of building materials comprising it.

Figure 1 .
Figure 1.(a)A general photo of the Varnakova Monastery before the 2017 fire.Arrows and dotted lines indicate the cells' section and the catholicon.(b) A general photo of the Varnakova Monastery after the fire -yellow dotted lines indicate the burnt cells' area.(c)A topographical depiction of the complex by Rural and Survey Engineer S. Zacharopoulos[19].(d)The ground plan of Ch.Bouras depicting the four architectural phases of the catholicon between the 11 th and 13 th centuries [18].

Figure 1 .
Figure 1.(a) A general photo of the Varnakova Monastery before the 2017 fire.Arrows and dotted lines indicate the cells' section and the catholicon.(b) A general photo of the Varnakova Monastery after the fire -yellow dotted lines indicate the burnt cells' area.(c) A topographical depiction of the complex by Rural and Survey Engineer S. Zacharopoulos [19].(d) The ground plan of Ch.Bouras depicting the four architectural phases of the catholicon between the 11th and 13th centuries [18].

Figure 2 .
Figure 2. Depiction of the Monastery cells in its present state after the fire, which indicates the external, the intermediate, and the internal masonry.The church, as indicated, is to the east.

Figure 2 .
Figure 2. Depiction of the Monastery cells in its present state after the fire, which indicates the external, the intermediate, and the internal masonry.The church, as indicated, is to the east.

Figure 3 .
Figure 3. Different areas of the cells quarter: (a) the exterior of the external wall (historic masonry), (b) the plastered interior façade of the external wall presenting severe damages from the fire (historic masonry), (c) the lower part of the internal wall facing the courtyard (new masonry raised on a historic base), (d) the historic intermediate masonry,(e) detail from the fire-affected intermediate masonry, and (f) the new masonry of the cells' quarter: its exterior façade seems intact after the fire, while its interior has suffered fire damage.

Figure 3 .
Figure 3. Different areas of the cells quarter: (a) the exterior of the external wall (historic masonry), (b) the plastered interior façade of the external wall presenting severe damages from the fire (historic masonry), (c) the lower part of the internal wall facing the courtyard (new masonry raised on a historic base), (d) the historic intermediate masonry, (e) detail from the fire-affected intermediate masonry, and (f) the new masonry of the cells' quarter: its exterior façade seems intact after the fire, while its interior has suffered fire damage.

Heritage 2019, 2 1238Figure 3 .
Figure 3. Different areas of the cells quarter: (a) the exterior of the external wall (historic masonry), (b) the plastered interior façade of the external wall presenting severe damages from the fire (historic masonry), (c) the lower part of the internal wall facing the courtyard (new masonry raised on a historic base), (d) the historic intermediate masonry,(e) detail from the fire-affected intermediate masonry, and (f) the new masonry of the cells' quarter: its exterior façade seems intact after the fire, while its interior has suffered fire damage.

Figure 4 .
Figure 4. (a) Collapse of building materials from the upper part of the intermediate masonry.(b) Discolorations and scaling of the beige-grey limestone on the interior (western) façade of the new masonry.

Figure 5 .
Figure 5. Diagram summarizing the methodological approach followed in this study.

Figure 6 .
Figure 6.(a) Photograph of sandstone sample V1.(b) The crystalline and lithic fragments of the sandstone are observed.The cementing material is of a sparitic calcite nature (crossed Nicols).(c) Photograph of sandstone sample V2.(d) Oxidation phenomena of iron compounds into the stone mass (crossed Nicols).

Figure 6 .
Figure 6.(a) Photograph of sandstone sample V1.(b) The crystalline and lithic fragments of the sandstone are observed.The cementing material is of a sparitic calcite nature (crossed Nicols).(c) Photograph of sandstone sample V2.(d) Oxidation phenomena of iron compounds into the stone mass (crossed Nicols).

Heritage2019, 2
Figure 7d-7e where joints filled with carbonate material and super fine-grained iron pyrite crystals are observed.

Figure 7 .
Figure 7. (a) Photograph of sample V5. (b,c) The stone constitutes of three to four zones (crossed Nicols).(d) The chert zone is traversed by joints filled with carbonate content, while super finegrained iron pyrite is, also, observed (crossed Nicols).(e) The chert zone consists of amorphous siliceous material and scattered iron pyrite crystals, (metallographic microscope, incident light).(f) The fossiliferous limestone zone.The orange hue is attributed to the diffusion of iron hydroxides (parallel Nicols).

Figure 8 .
Figure 8.(a) Photograph of limestone sample V6.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).

Figure 7 .
Figure 7. (a) Photograph of sample V5. (b,c) The stone constitutes of three to four zones (crossed Nicols).(d) The chert zone is traversed by joints filled with carbonate content, while super fine-grained iron pyrite is, also, observed (crossed Nicols).(e) The chert zone consists of amorphous siliceous material and scattered iron pyrite crystals, (metallographic microscope, incident light).(f) The fossiliferous limestone zone.The orange hue is attributed to the diffusion of iron hydroxides (parallel Nicols).

Heritage2019, 2
Figure 7d-7e where joints filled with carbonate material and super fine-grained iron pyrite crystals are observed.

Figure 7 .
Figure 7. (a) Photograph of sample V5. (b,c) The stone constitutes of three to four zones (crossed Nicols).(d) The chert zone is traversed by joints filled with carbonate content, while super finegrained iron pyrite is, also, observed (crossed Nicols).(e) The chert zone consists of amorphous siliceous material and scattered iron pyrite crystals, (metallographic microscope, incident light).(f) The fossiliferous limestone zone.The orange hue is attributed to the diffusion of iron hydroxides (parallel Nicols).

Figure 8 .
Figure 8.(a) Photograph of limestone sample V6.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).

Figure 8 .
Figure 8.(a) Photograph of limestone sample V6.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).

Figure 9 .
Figure 9. (a) Photograph of fire-effected limestone sample V8.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).(c) Joint rupture with a width range of 15-18μm (crossed Nicols).

Figure 10 .
Figure 10.(a) Photograph of fire-effected limestone sample V7.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (crossed Nicols).(c) Joint rupture with a width range of 35 to 65μm (crossed Nicols).

Figure 9 .
Figure 9. (a) Photograph of fire-effected limestone sample V8.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).(c) Joint rupture with a width range of 15-18 µm (crossed Nicols).

Figure 9 .
Figure 9. (a) Photograph of fire-effected limestone sample V8.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (parallel Nicols).(c) Joint rupture with a width range of 15-18μm (crossed Nicols).

Figure 10 .
Figure 10.(a) Photograph of fire-effected limestone sample V7.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (crossed Nicols).(c) Joint rupture with a width range of 35 to 65μm (crossed Nicols).

Figure 10 .
Figure 10.(a) Photograph of fire-effected limestone sample V7.(b) Grey-beige micritic fossiliferous limestone: the matrix of the stone is of micritic texture, while traces of fossils and sparitic foraminiferal species are detected inside the stone mass.A great number of joints, filled with secondary calcite, traverse the stone mass (crossed Nicols).(c) Joint rupture with a width range of 35 to 65 µm (crossed Nicols).

Figure 11 .
Figure 11.(a) Photograph of limestone sample V9 where two zones are distinct.(b) On the left, the grey-beige micritic fossiliferous limestone zone and, on the right, the grey-black fossiliferous limestone zone, (parallel Nicols).(c) Grains of iron oxides close to the interface of the two zones (parallel Nicols).

Figure 12 .
Figure 12.(a) Photograph of fire-affected limestone sample V10.(b) The capillary rupture of some μm width observed in the stone mass constitutes a micro-structural change.The orange hue is due to the diffusion of iron hydroxides and infers the visually observed reddening of the stone (parallel Nicols).(c) Oxidation of iron compounds due to the high temperature during the fire (parallel Nicols).

Figure 11 .
Figure 11.(a) Photograph of limestone sample V9 where two zones are distinct.(b) On the left, the grey-beige micritic fossiliferous limestone zone and, on the right, the grey-black fossiliferous limestone zone, (parallel Nicols).(c) Grains of iron oxides close to the interface of the two zones (parallel Nicols).

Figure 11 .
Figure 11.(a) Photograph of limestone sample V9 where two zones are distinct.(b) On the left, the grey-beige micritic fossiliferous limestone zone and, on the right, the grey-black fossiliferous limestone zone, (parallel Nicols).(c) Grains of iron oxides close to the interface of the two zones (parallel Nicols).

Figure 12 .
Figure 12.(a) Photograph of fire-affected limestone sample V10.(b) The capillary rupture of some μm width observed in the stone mass constitutes a micro-structural change.The orange hue is due to the diffusion of iron hydroxides and infers the visually observed reddening of the stone (parallel Nicols).(c) Oxidation of iron compounds due to the high temperature during the fire (parallel Nicols).

Figure 12 .
Figure 12.(a) Photograph of fire-affected limestone sample V10.(b) The capillary rupture of some µm width observed in the stone mass constitutes a micro-structural change.The orange hue is due to the diffusion of iron hydroxides and infers the visually observed reddening of the stone (parallel Nicols).(c) Oxidation of iron compounds due to the high temperature during the fire (parallel Nicols).

Heritage2019, 2
FOR PEER REVIEW 14 Vm3 Structural soft mortar of clay texture and dark-orange hue from the upper part of the historical intermediate masonry (above 2m).Vm4 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm5 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm6In-depth mortar of mixed cementitious and clay texture from a severely fire-affected area at the lower part of the historical intermediate masonry (<1m).Vm3Structural soft mortar of clay texture and dark-orange hue from the upper part of the historical intermediate masonry (above 2 m).

Heritage2019, 2
FOR PEER REVIEW 14 Vm3 Structural soft mortar of clay texture and dark-orange hue from the upper part of the historical intermediate masonry (above 2m).Vm4 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm5 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm6 In-depth mortar of mixed cementitious and clay texture from a severely fire-affected area at the lower part of the historical intermediate masonry (<1m).Vm4 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2 m).

Heritage2019, 2
FOR PEER REVIEW 14 Vm3 Structural soft mortar of clay texture and dark-orange hue from the upper part of the historical intermediate masonry (above 2m).Vm4 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm5 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm6 In-depth mortar of mixed cementitious and clay texture from a severely fire-affected area at the lower part of the historical intermediate masonry (<1m).Vm5 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2 m).Heritage2019, 2 FOR PEER REVIEW 14 Vm3 Structural soft mortar of clay texture and dark-orange hue from the upper part of the historical intermediate masonry (above 2m).Vm4 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm5 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).

Heritage2019, 2
FOR PEER REVIEW 15 Vm7 Joint mortar of cementitious texture from a severely fire-affected area with blackened external surface due to smoke deposition -lower part of the historical intermediate masonry (same sampling area with Vm6, <1m) Vm8 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).Vm7 Joint mortar of cementitious texture from a severely fire-affected area with blackened external surface due to smoke deposition -lower part of the historical intermediate masonry (same sampling area with Vm6, <1 m) Heritage2019, 2 FOR PEER REVIEW 15 Vm7 Joint mortar of cementitious texture from a severely fire-affected area with blackened external surface due to smoke deposition -lower part of the historical intermediate masonry (same sampling area with Vm6, <1m) Vm8 Structural soft mortar of clay texture and yellow hue from the upper part of the historical intermediate masonry (above 2m).

Figure 13 .
Figure 13.Correlation of CO2 and the CO2/H2OCBW ratio.The clay mortar group and cement-based mortar group are indicated.

Figure 13 .
Figure 13.Correlation of CO 2 and the CO 2 /H 2 O CBW ratio.The clay mortar group and cement-based mortar group are indicated.

Figure 14 .
Figure 14.AREA 1: The exterior of the external masonry, on the left of the entrance to the monastic cells quarter (historic masonry, western façade).Bullets and numbering indicate where the SHR measurements were performed.

Figure 14 .
Figure 14.AREA 1: The exterior of the external masonry, on the left of the entrance to the monastic cells quarter (historic masonry, western façade).Bullets and numbering indicate where the SHR measurements were performed.

Figure 16 .
Figure 16.AREA 3: South-Western façade of the intermediate masonry.The area was examined after the plaster's removal.(a) South façade of the intermediate masonry.(b) Western façade of the intermediate masonry.Numbering indicates the corner-stones examined by SHR from south to west.

Figure 16 .
Figure 16.AREA 3: South-Western façade of the intermediate masonry.The area was examined after the plaster's removal.(a) South façade of the intermediate masonry.(b) Western façade of the intermediate masonry.Numbering indicates the corner-stones examined by SHR from south to west.

Figure 17 .
Figure 17.AREA 4: New masonry (Northern façade).The pillar is built from the beige-grey limestone.The examined areas by SHR are labeled.

Figure 17 .
Figure 17.AREA 4: New masonry (Northern façade).The pillar is built from the beige-grey limestone.The examined areas by SHR are labeled.
, zone under the dotted line) compared to the upper zone (Figure 18c,d, zone above the dotted line), as well as a tighter temperature distribution width of 2 • C (from 26 • C to 28 • C), whereas the upper zone displays a temperature distribution width of 4 • C (from 23.5 • C to 27.5 • C).

Figure 18 .
Figure 18.(a) Photo of the examined area 1 on the new masonry (higher masonry part).(b) Thermography of area 1. (c) Photo of the examined area 2 on the new masonry (lower masonry partarea 2 is below area 1).(d) Thermography of area 2.
), which are attributed to the different degree of the surface detachment/scaling due to the fire effect.The intermediate historical masonry presents a wide temperature distribution width of 4.5 °C (from 22.5 °C to 27 °C ).

Figure 19 .
Figure 19.(a) Photo of the examined area 3 of the intermediate historical masonry.(b) Thermography of area 3.

Figure 18 .
Figure 18.(a) Photo of the examined area 1 on the new masonry (higher masonry part).(b) Thermography of area 1. (c) Photo of the examined area 2 on the new masonry (lower masonry part-area 2 is below area 1).(d) Thermography of area 2.
,b), which are attributed to the different degree of the surface detachment/scaling due to the fire effect.The intermediate historical masonry presents a wide temperature distribution width of 4.5 • C (from 22.5 • C to 27 • C).

Heritage2019, 2 Figure 18 .
Figure 18.(a) Photo of the examined area 1 on the new masonry (higher masonry part).(b) Thermography of area 1. (c) Photo of the examined area 2 on the new masonry (lower masonry partarea 2 is below area 1).(d) Thermography of area 2.

Figure 19 .
Figure 19.(a) Photo of the examined area 3 of the intermediate historical masonry.(b) Thermography of area 3.

Figure 19 .
Figure 19.(a) Photo of the examined area 3 of the intermediate historical masonry.(b) Thermography of area 3.

Heritage2019, 2 FOR PEER REVIEW 23 Figure 20 .
Figure 20.(a) Photo of the examined area 4 of the intermediate historical masonry.(b) Thermography of area 4.

Figure 21 .
Figure 21.(a) Photo of the examined area 5 of the intermediate historical masonry.(b)Thermography of area 5.

Figure 20 .
Figure 20.(a) Photo of the examined area 4 of the intermediate historical masonry.(b) Thermography of area 4. Furthermore, IRT investigation of the historical intermediate masonry surfaces that are blackened from the fire, records these areas with higher temperature readings (Figure 21); a result in accordance with the IRT examination of the respective areas of the new masonry.Temperature distribution width of the blackened surface is 2 • C (from 23.5 • C to 25.5 • C), whereas the rest of the masonry area under investigation holds a temperature distribution width of 3 • C (from 22 • C to 25 • C).

Heritage2019, 2 FOR PEER REVIEW 23 Figure 20 .
Figure 20.(a) Photo of the examined area 4 of the intermediate historical masonry.(b) Thermography of area 4.

Figure 21 .
Figure 21.(a) Photo of the examined area 5 of the intermediate historical masonry.(b)Thermography of area 5.

Figure 21 .
Figure 21.(a) Photo of the examined area 5 of the intermediate historical masonry.(b) Thermography of area 5.

Table 1 .
Description of the selected stone samples from the cells' quarter.Collected from intermediate historic masonry, which is seemingly unaffected by the fire area (based on visual inspection).Second most abundant stone type used in the monument.V2 Sandstone sample, collected from intermediate historic masonry, from a fire-affected area of the masonry.V5 Compact black stone collected from a severely fire-affected area of the intermediate masonry.V6

Table 2 .
XRD analysis of stone samples.

Table 3 .
TG results of stone samples.

Table 4 .
Total water immersion tests results -stones.

Table 5 .
Description of the selected mortar samples from the cells' quarter.

Table 7 .
TG results of mortars' samples.

Table 8 .
Total water immersion tests results -mortars.

Table 8 .
Total water immersion tests results -mortars.

Table 9 .
SHR values from the AREA 1 (see Figure14).The eastern façade of the intermediate historic masonry (AREA 2) was investigated after being divided per height in two areas: below 50 cm and above 1 meter (Figure