heritage
Article
The Chiaravalle Cross: Results of a Multidisciplinary Study
Daniela Di Martino 1 , Giulia Benati 2 , Roberto Alberti 3 , Sandro Baroni 4 , Carlo Bertelli 5 ,
Franco Blumer 6 , Letizia Caselli 7 , Roberta Cattaneo 1 , Costanza Cucini 8 , Fabio D’Amico 9 ,
Tommaso Frizzi 3 , Elisabetta Gagetti 10 , Michele Gironda 3 , Lisa Greggio 9 , Lorenzo Lazzarini 11 ,
Maya Musa 9 , Enrico Perelli Cippo 12 , Maria Pia Riccardi 13,14, * and Giuseppe Gorini 1
1
2
3
4
5
6
7
8
9
10
11
12
13
14
*
Dipartimento di Fisica “G. Occhialini”, Università degli Studi di Milano-Bicocca, 20126 Milan, Italy
Veneranda Fabbrica del Duomo di Milano, 20122 Milan, Italy
XGLab S.R.L.—Bruker Nano Analytics, 20134 Milan, Italy
Fondazione Maimeri, 20144 Milan, Italy
Faculty of Art, University of Lausanne, 1015 Lausanne, Switzerland
Franco Blumer Restauro Metalli, 24020 Bergamo, Italy
Ateneo Veneto di Scienze, Lettere e Arti, Classe di Lettere e Arti, 30124 Venice, Italy
Laboratoire “Métallurgies et Cultures”, CNRS, IRAMAT Université de Technologie Belfort Montbéliard,
90010 Belfort, France
Gulf Institute of Gemology, Al Khuwair 133, Muscat, Oman
Independent Researcher, 20900 Monza, Italy
LAMA, Università IUAV, 30135 Venice, Italy
Istituto di Fisica del Plasma “P. Caldirola”, Consiglio Nazionale delle Ricerche, 20125 Milan, Italy
Dipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, 27100 Pavia, Italy
Arvedi Laboratorio, Università degli Studi di Pavia, 27100 Pavia, Italy
Correspondence: mariapia.riccardi@unipv.it
Received: 30 July 2019; Accepted: 28 August 2019; Published: 30 August 2019
Abstract: The Chiaravalle Cross, a masterpiece of Mediaeval goldsmithery, went under restoration in
2016. This was a unique opportunity to undertake an in-depth multidisciplinary study. Several issues
were addressed, as for example the chronology of the Cross, lacking any official document about it.
The scientific investigations included in situ and laboratory measurements, and the analyses, part of
a multidisciplinary protocol, completely characterized the gemstones adorning the Cross, the cameos,
the gold, silver, jasper and glass parts, to derive indications on their provenance, authenticity and
dating issues. All the results were shared with the whole collaboration of experts, which included art
historians, a restorer, a conservator, a scholar in ancient glyptic, gemologists, archaeometallurgists,
physicists and scientists in a very fruitful exchange of knowledge. This work is an example of a real
multidisciplinary research, gathering good practices in the study of a complex piece of art.
Keywords: Chiaravalle Cross; multidisciplinary protocol; gemstones characterization; 14 C dating;
SEM measurements; Raman Spectroscopy; XRF analyses; cameos study
1. Introduction
The Chiaravalle Cross, a mediaeval jewelry masterpiece, is a processional cross made of silver
and gold laminas, combined to filigrees, gemstones, cameos and red jasper plates. This piece from the
Museo del Duomo’s collection was restored during “Restituzioni 2016” [1]. Ancient documents on
the Chiaravalle Cross are rare,1 inaccurate and contradictory. In the late 19th century other scholars
1
The Cross has been mentioned in a Braidense manuscript [2], in the works of Count Giulini [3] and in the pages of
Longobardic Antiquities [4], chapter VIII.
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www.mdpi.com/journal/heritage
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added different conflicting interpretations.2 Finally, in the twentieth century, having cleared the field
of erroneous attributions to earlier times, the Cross was recognized as a work of Venetian art that
could be inserted into a large group of masterpieces of goldsmithery, dated to the end of the 13th
century. In particular, the Chiaravalle Cross is acknowledged as a work of art executed in Venice at
the end of the 13th century [6], likely commissioned by the archbishop of Milan Ottone Visconti (who
died in 1295). However, some decorations (like one angel statue and some gems) seem to have been
produced after this period.
The chronological attribution was one of the important research aspects, but the rich decoration and
complex iconography of this piece of art deserved further insights. The production and manufacturing
techniques of a complex piece of art like the Chiaravalle Cross involve much expertise, and in order to
derive a comprehensive knowledge many different multidisciplinary skills are required. Metalworking
and decoration techniques used in the production of jewelry can, for example, give indications on the
period of fabrication, while the choice for different materials suggests information on the provenance
of an ancient object of unknown origin. Several scientific investigations were applied during the
restoration of the Cross, including in situ and laboratory measurements, addressing different materials.
The analyses, part of a multidisciplinary protocol, completely characterized the gemstones adorning
the Cross, the cameos, the gold, silver, jasper plates and glass parts, to derive indications on materials
provenance, conservation status and authenticity issues [7].
The Cross was under restoration at Franco Blumer laboratory (Bergamo, Italy): this was an
invaluable circumstance to undertake selected and focused scientific analyses. A multidisciplinary study
was carried out, including neutron and nuclear analysis, gemological analysis, Raman characterization,
X-ray fluorescence (XRF) and scanning electron microscope (SEM) measurements, whose main results
will be discussed below.
This project gathered many different experts and all the contributors shared their findings in a
very fruitful collaboration, resulting in an in-depth knowledge of the masterpiece in order to clarify
several open questions as stated above.
2. Materials and Methods
The Cross is a precious jewelry masterpiece of rather complex construction, as can be seen from
the pictures (see Figure 1). The core of the Cross is a walnut wooden structure covered on the front
with 12 plates of red jasper, on which the main figures of the crucified Christ, of the Virgin and of
Saint John the Evangelist were applied, all made of lost wax-cast silver, finely chiselled, gilded with
mercury amalgam. The filigree in gilded silver entirely surrounds the outline and it is adorned with
jeweled settings (cameos, transparent and opaque colored gemstones). The perimeter thickness of
the Cross is entirely covered by a smooth and shiny silver sheet made in a single segment, fixed by
nails. On the back there are embossed, chiselled and gilded silver laminae, covered with natural quartz
lenses, ialine variety (commonly known as “rock crystal”). Many other details, visible before and after
the restoration, are available in [1] as well as the restoration report by F. Blumer (see contributions by
F. Blumer in [1], and [7], pp. 237–271).
The restorer had access to the inner part of the artefact, since a few parts were dismounted to
perform a better cleaning. In some cases, few fragments were available for the analysis. The use
of non-destructive and non-invasive analysis was very important for the whole study. However,
for dating analyses some very small fragments were used. We will focus on three different types of
analysis: (a) radiocarbon dating, (b) gemological study and (c) SEM measurements. Further analyses
were carried out, mainly neutron-based techniques, whose details can be found elsewhere [8,9].
Concerning the golden filigree, this deserves a particular attention, since the materials used and the
2
See for example [5], p. 54. Many other interpretations on the origin of the Cross followed, as described by the historic-artistic
notes in [1].
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techniques of fabrication were very peculiar. Therefore, an in-depth study performed both by SEM
and particle-induced X- and gamma-ray emission (PIXE and PIGE) is still ongoing and it will be the
subject of a presentation at the forthcoming IBA2019 congress (Antibes, October 2019 [10]).
(a)
(b)
Figure 1. The Chiaravalle Cross: (a) front; (b) rear. High-resolution images, before and after the
restoration, are available in [1]. The codes are relevant mainly for the identification of different
gems placements.
2.1. Radiocarbon Dating
14 C-AMS
(radiocarbon accelerator mass spectrometry) dating was performed at the CIRCE
laboratory (Caserta, Italy). Three samples were made available for the analysis: two pieces of wood
(few grams, from two different locations on the Cross) and some stucco coming from the rear of a
gem setting. In particular, we coded samples from the wood as RC442 (coming from the node of the
Cross, at its bottom part, FZ region-see Figure 1a,b) and RC443 (coming from the central part of the
Cross), while RC439 specimen was the stucco one (taken from the rear of jasper in R1, see Figure 1b).
The samples were prepared in the CUDAM laboratory (University of Milano-Bicocca).
The measurements have derived the ratios C14/C12 and C13/ C12 for carbon isotopes, extracted
by chemical and physical treatments from the specimens. From these data, the percentage of modern
carbon (pMC) has been derived, and the conventional age (tRC) calculated. This age has been calibrated
from OxCal v.4, calibration curve INTCAL04 [11] to obtain the calendar age.
2.2. Gemological Study
To identify and characterize all the gemstones set in the Chiaravalle Cross, we used the standard
gemological tools [12]. The gems dimensions, when possible, have been measured using a digital
dimensiometer, Presidium model, with a tolerance of ±0.01 mm. The setting prevented the direct
detection of gemstones weights by the scale method. The estimated carat weights were obtained on
the basis of the dimensions and known average density. On the unremovable stones, the observations
have been performed by the achromatic aplanatic 10× triplet gemological loop; while the partially
unset stones allowed the dark field microscope analysis. We used a Leica S6E optical microscope with
16× ocular and 0.63–4.0× magnification.
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The species and the variety identification were obtained crossing the refractometer analysis,
where applicable, with the optical observation. The standard gemological tests were completed by
fluorescence analysis exciting the gemstones with long wave (365 nm) and short wave (354 nm)
light sources.
For the main 17 gemstones set in the front of Chiaravalle Cross, the limitations imposed by the
mounting in the characterization performed by the standard methods were undertaken by applying a
portable spectrometer of new generation: XRAMAN, made by XGlab company [13]. This instrument
is able to perform in situ, fast and non-contact combined elemental and molecular analyses, by the
complementary EDXRF (energy-dispersive X-ray fluorescence) and Raman techniques. The XRF
system is fully integrated into a compact detection head and is equipped with a 20 mm2 fast silicon
drift detector (SDD) and digital readout electronics. The exciting source is a high-efficiency and
compact 50 kV X-ray tube, 200 µA (max 10 W) with Rh anode. The X-ray tube is coupled with three
automatically software-selectable different collimators between 0.5 mm and 2 mm and a set of X-ray
filters to improve low detection limit capability in special applications. Usual measuring conditions for
XRF were the following: X-ray tube 50 kV, 80 µA current, and acquisition time 30 s. Regarding the
Raman system, the instrument is equipped with a cooled CCD detector with 6–7 cm−1 of resolution
and 100–4000 cm−1 analytical range. The excitation source is a compact 785 nm stabilized laser source
with output power regulable from 0 to 500 mW. Common measuring conditions were power 400 mW
and acquisition time 180 s. However, the length of the measurements (for both XRF and Raman spectra)
could be different in order to acquire a good statistic.
Thanks to the XRAMAN alignment system, made by a couple of lasers (axial and focal) and a
micro-camera, able to observe a 2 × 2 cm2 area at 10× magnification, the tests were performed at 1 cm
distance, without any direct contact between the gemstones and the instrument. The analyzed area
corresponds to about 1 mm diameter with perfect coincidence for both techniques.
2.3. Scanning Electron Microscope (SEM) Measurements
A scanning electron microscope (SEM) equipped with an energy-dispersion (EDS) detector was
used in a non-invasive approach, i.e., without any treatment of the artifact, to study some elements of
the Cross (like glass, filigrees, collets, embossed sheet and figures in relief). Their sizes, though large,
could be easily housed in the sample chamber.
The instrument used is a TESCAN Mira XMU series, coupled with an EDAX system in EDS, and the
operating conditions for the collection of images and microanalysis were as follows: beam acceleration
voltage: 20 KV; beam current: 40 mA; working distance: 15.8 mm; counting for microanalysis: 100 s;
correction factor for microanalysis: ZAF; analysis area 100 × 100 µm2 .
The study has returned images in high resolution, both in secondary electrons (SE) and
in back-scattered electrons (BSE) of the surfaces, of the texture of the material, of the relations
(microstructures) between the different metal alloys and crystalline and/or amorphous phases.
EDS measurements, when conducted on morphological surfaces, should be considered purely
indicative of the chemical composition of the sample, since it is possible that, during the measurement,
a direct proportionality between the signal output from the sample and the counts to the detector is
not guaranteed, due to the lack of flatness of the surface.
3. Results
3.1. Radiocarbon Dating Results
The following results were obtained for the pMC and conventional dates, with relative errors and
ranges of the probable dates within 1σ and 2σ (between 68% or 95% confidence level).
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Code
RC439
RC442
RC443
pMC
97.10 ± 0.36
90.28 ± 0.34
89.51 ± 0.34
tRC (years BP)
236 ± 30
822 ± 30
890 ± 30
Calibrated Date
σ (±1σ)
1645–1800 AD
1190–1260 AD
1050–1205 AD
Calibrated Date
σ (±2σ)
1530–present
1165–1265 AD
1040–1220 AD
A better visualization of the results is displayed in Figure 2. As reported in the previous section
we coded samples from the wooden core as RC442 (node of the Cross) and RC443 (central part of
the Cross), while RC439 specimen was the stucco one (R1 gem position, see Figure 1b).
Figure 2. Scheme for the results of
different specimens.
14 C
dating, displaying the probability for the dates of the
We can thus underline from the age of the wooden part that the central part of the Cross was
not fabricated before 1040 AD (considering the wider probability range of dates: 1040–1220 AD) and
the node of the Cross was not fabricated before 1165 AD (considering the wider probability range of
dates: 165–1265 AD). If we consider the node and the central part of the Cross fabricated at the same
time, the chronological attribution of the Cross should be in the shortest range, that is 1165–1265 AD.
We stress that these dates represent a lower limit: indeed, the wood could have been cut at those dates,
but we do not know the exact date of fabrication of the Cross. We know that the piece of art has been
produced later than the cut of the wooden part (later than 1165–1265 AD), while the age obtained for
the stucco sample is a modern age.
3.2. Gemstones Characterization
On the Chiaravalle Cross are set a total of 985 gemstones, assigned 533 on the front and 452 on the
rear. On the basis of the dimensions it was possible to classify this large number of stones as reported
in Table 1.
Table 1. Overview of front and rear distribution of central and lateral gemstones on the Chiaravalle
Cross. In this table, the average of the estimated carat weights ranges are also reported.
Front
Rear
1)
420 lateral gemstones (0.40–0.60 ct
96 central gemstones (1.00–3.00 ct 1 )
1
420 lateral gemstones (0.40–0.60 ct 1 )
15 central gemstones (0.80–3.00 ct 1 )
Due to the limitations imposed by the mounting, the carat weight ranges are estimated.
As displayed in Figure 3, we could summarize the gemological items shown in Figure 1: the main
gemstones are the 34 stones, 10 cameos included, set as centre of the round motif; the central gemstones
are the 111 stones set as centre of the half-moon motif plus the stones surrounding the Christ icon on
the front; the lateral term refers to the smaller gemstones decorating the circular and the half-moon
motif as well. The lateral and the central gemstones are all oval cabochon or irregular oval cabochon,
while the main gemstones present more variety in shape and cutting style.
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Figure 3. The terms used to describe the stones are clarified in this image, corresponding to the right arm
magnification and reporting several examples: in purple circle, green circles and blue circles are reported
the position of one main gemstone, two central gemstones and two lateral gemstones, respectively.
On the basis of the data reported in Table 1, it is possible to observe a difference in the distribution
between the front and the rear of the Cross. The higher number of the front central stones is ascribable
to the line motif surrounding the Christ icon, not present on the rear where the bas relief are surrounded
by the filigree.
Due to the large number of central and lateral gems, these gemstones have been also classified on
the basis of their species and their colors (Table 2).
Table 2. This table reports the distribution of the lateral and central stones set in the front (a) and in the
rear (b) of the Chiaravalle Cross, in relation to the main color categories.
(a) FRONT
Red
Blue
Green–Yellow–Other
LATERAL
mainly garnets and
spinels; rare rubies
CENTRAL
mainly rubies
mainly sapphires; rare iolite and
moonstones 1 , artificial glass
sapphires, few lapis, rare
artificial glass
beryls, few emeralds included,
tiger eye quartz 1 , artificial glass
artificial glass, amethysts and
chalcedonies
(b) REAR
Red
Blue
Green–Yellow–Other
LATERAL
mainly garnets and
spinels; rare rubies
mainly sapphires; rear iolite and
moonstones 1 artificial glass
CENTRAL
rubies and spinels
sapphires and artificial glass
green beryls and few emeralds,
tiger eye quartz 1 , artificial glass
artificial glass, amethysts and
moonstones1
1
Gem with optical phenomena.
The characterization data of the 34 main gemstones are reported in Table 3. To match the correct
position of the gemstones set on the Chiaravalle Cross, Table 3 reports the codes used to identify the
stones in Figure 1.
Table 3. Identification of the main 34 gemstones set in the Chiaravalle Cross. Due to the limitation
imposed by the mounting, the dimensions have been rounded off and “Not Applicable (NA)” has been
indicated when it was not possible to carry out the identification.
Code
Dimensions
(mm)
Shape and Cut
Transparency
Color
Identification
F1
35.7 × 29.3 × 2.8
oval cameo
translucent
brown and
white
chalcedony,
sardonyx variety
FDD1
32.4 × 23.5 × 2.4
hexagonal
tablet
translucent
blue and white
trapiche sapphire
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Table 3. Cont.
Code
Dimensions
(mm)
Shape and Cut
Transparency
Color
Identification
FDE1
15.8 × 12.4 × 2.7
irregular
cabochon
translucent
green
artificial glass
FDF1
30.5 × 21.7 × 2.8
hexagonal
tablet
translucent
blue and white
trapiche sapphire
FDL1
33.1 × 25.6 × NA
oval cameo
opaque
brown and
white
chalcedony,
sardonyx variety
FDP1
20.6 × 16.7 × NA
cushion cameo
translucent
brownish green
artificial glass
FDQ1
17.0 × 15.8 × 2.3
oval tablet
opaque
orangy brown
Artificial mixture
FDR1
NA
square cameo
translucent
greenish blue
chalcedony
FDV1
27.6 × 24.0 × NA
cameo
translucent
brown and
white
chalcedony,
sardonyx variety
FSV1
36.6 × 30.0 × 4.4
cameo
translucent
brown and
white
chalcedony,
sardonyx variety
FSR1
22.8 × 14.8 × 3.4
oval cameo
translucent
green
artificial glass
FSQ1
15.4 × 13.7 × NA
oval tablet
opaque
blue
lapis simulant
FSP1
NA
oval cameo
translucent
brownish green
artificial glass
FSL1
NA
cameo
opaque
bluish green
artificial glass
FSF1
NA
hexagonal
tablet
translucent
blue and white
trapiche sapphire
FSE1
15.0 × 11.5 × 2.5
irregular
cabochon
translucent
green
artificial glass
FSD1
31.9 × 23.3 × 2.7
hexagonal
tablet
translucent
blue and white
trapiche sapphire
R1
32.8 × 27.4 × 2.1
oval tablet
opaque
red
jasper
RDD1
29.3 × 18.6 × 7.2
irregular
cabochon
translucent
white
chalcedony,
agata variety
RDE1
13.4 × 11.1 × 4.3
irregular tablet
opaque
orangy brown
jasper
RDF1
26.0 × 23.7 × 3.0
irregular
cabochon
transparent
green
artificial glass
RDL1
19.2 × 17.2 × 4.0
cushion cameo
translucent
green and
brown
artificial glass plus
greek tar
RDP1
24.6 × 17.8 × 4.2
oval cabochon
transparent
green
artificial glass
RDQ1
17.3 × 14.1 × 4.8
tumbled
opaque
green and
white
chalcedony,
plasma variety
RDR1
19.9 × 14.7 × 3.3
irregular
cabochon
translucent
orangy white
chalcedony
RDV1
27.8 × 23.3 × 4.1
rectangular
cabochon
opaque
brownish red
jasper
RSV1
33.7 × 25.0 × 5.0
oval tablet
opaque
red
jasper
RSR1
13.0 × 12.5 × 3.5
oval tablet
opaque
brown and
white
chalcedony/jasper
RSQ1
14.8 × 13.3 × 4.1
round tablet
opaque
brown
jasper
RSP1
24.7 × 20.4 × 6.4
cushion
cabochon
opaque
green and
brown
jasper
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Table 3. Cont.
Code
Dimensions
(mm)
Shape and Cut
Transparency
Color
Identification
RSL1
20.9 × 17.3 × 6.2
irregular
triangular
cabochon
opaque
brownish green
chalcedony-jasper
RSF1
25.2 × 23.5 × 4.3
oval tablet
opaque
brown
chalcedony-jasper
RSE1
13.0 × 11.5 × 4.2
irregular tablet
opaque
orangy brown
jasper
RSD1
22.1 × 14.4 × 6.3
irregular
cabochon
translucent
white
chalcedony, agata
variety
As already observed for lateral and central stones, the front and the rear of the Cross result
different for quality and preciousness of the gem materials set, favoring the front. Considering for
example the cameos distribution, 9 are set on the front while only one on the rear.
Where the standard gemological tests were not enough to complete the identification of the main
gemstones, the XRAMAN instrument was used, in order to complete the characterization by the
chemical and Raman data.
When the laser source of the XRAMAN instrument was focused on the surface of one of the
four sardonyx cameos reported in Figure 4a–d, a Raman spectrum as reported in Figure 4e was
recorded, showing bands at 208, 350, strong 466 with a second weak peak at 500 cm−1 , consistent with
chalcedony—crypto-crystalline quartz—mineral phase [14]. These cameos are different from the other
six, one in bluish-green chalcedony (FDR1) and the other five in artificial glass.
Figure 4. The four sardonyx cameos ((a) F1, (b) FDL1, (c) FDV1, (d) FSV1) and the corresponding
Raman spectrum (e), showing the bands consistent with the chalcedony mineral phase. High-resolution
images can be seen in [1].
−
−
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The same technique was applied to confirm the identification of the FSQ1 gemstone as lapis
simulant (Figure 5). The Raman spectrum acquired on the FSQ1 gemstone did not display any
band at 544 cm−1 (usually considered diagnostic for lazurite mineral phase [15]), or calcite bands or
other typically lapis minerals bands. The band at 1316 cm−1 is the only Raman feature visible in the
spectrum of the FSQ1 gemstone and this band, especially when it is present without the 544 cm−1
band, corresponds to the Raman feature of the synthetic ultramarine pigment [16]. On the other hand,
the XRF spectrum has recorded barium and zirconium traces, not reported for the natural lapis-lazuli
chemical composition [17]. For better clarity, we report that in the XRF spectrum the presence of the
Au peaks (at ~9.7 and 11.4 keV) and the broad Rh Compton (~19 keV) peak are visible.
Figure 5. (a) lapis simulant FSQ1, (b) the chemical composition X-ray fluorescence (XRF) spectrum,
and (c) the Raman spectrum. Note the presence of barium and zirconium, commonly found in the
mixtures, and the absence of the lazurite and calcite bands in the Raman spectrum.
Due to their relative rarity, one of the most important gemological observation regards the
presence of four magnificent trapiche sapphires, set in the front and characterized by hexagonal shape
tablet cut. In Figure 6, sapphires detailed images are reported with the corresponding Raman and
−
XRF spectra. The Raman bands at 416 cm−1 and
749 cm−1− are ascribable to the corundum mineral
− are correlated to the vibrational modes of the blue
phase [15] and the bands at 185 and 246 cm−1
chromophore group in sapphire variety [18]. Moreover, by the XRF analyses it was possible to detect
aluminum, iron, small trace of titanium and gallium as the mainly elements of the gemstones’ chemical
composition [19]. The inclusions responsible for the “white star” visible on the surface of the trapiche
sapphires, have been characterized as feldspar group minerals [20].
Among the gemstones, 10 are carved in relief (cameos). They can be divided into two groups.
The first consists of six specimens (Figure 1: FSL1, FSP1, FSR1, FDR1, FDP1, RDL1). The group
can be dated to the mid-Byzantine period (dynasty of the Komnenoi; late 11th century), owing to
peculiar iconographies, (Christ Pantokrator, the Virgin Hagiosoritissa—two specimens—Christ in the
well dated iconography of the Akra Tapeinosis, saint Peter and, possibly, saint Paul; its upper half is
missing), styles and inscriptions (mostly the cameo with saint Peter, showing the typical 11th-century
remake of the epigraphic “uncial BR” style). All of the six cameos are in monochrome glass, except
for one, in bluish chalcedony. The second group consists of four cameos, all in two-layered sardonyx
(Figure 1: F1, FSV1, FDV1, FDL1; Figure 3). They can be ascribed to the atelier working at the Norman
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court of the Hautevilles in Palermo (second half of the 11th century), owing to comparisons with
artifacts in different media, regarding the rendering of the lion head; the ordering of the feathers on the
eagle’s body; details in the pose, draperies, nimbus of the Pantokrator. During the 12th century at the
court of the Hautevilles, in fact, a multi-ethnic atelier was active in the arts of luxury: among these,
glyptic flourished again in the West, after a span of at least four centuries, merging the skillfulness
of gemstone carvers from Fatimid Egypt and iconographic models from Byzantium, with no traces
of cultural conflicts (see an extended discussion and wide literature on both groups in Gagetti, E.,
“Minute imagini scolpite nelle pietre”. L’ornato glittico della Croce di Chiaravalle, in [7], pp. 123–183).
Figure 6. The marvelous four trapiche sapphires ((a) FSD1, (b) FSF1, (c) FDD1, (d) FDF1) and the
corresponding Raman (e) and XRF (f) spectra.
Finally, the XRAMAN instrument was focused on the red platelets constituting the background
of the front, recording a spectrum with a double bands at 466 cm−1 and 504 cm−1 , ascribable to
jasper—crypto-crystalline quartz—mineral phase [14], while the bands at 227, 294, 407 and 610 cm−1
are typical for the hematite phase [21], responsible for the jasper red color [19].
3.3. SEM Results
The analysed glass-gems belong to the plate coded RDD1 (Figure 7A) and seem to be original.
Figure 7B shows the BSE image of gem-glass 3. The collet is intact and shows no sign of deformation,
as reported by the restorer. Moreover, in the southern portion of the collet it is possible to observe the
presence of a boilish material, inserted between the glass and the collet, which can be interpreted as
the glue used for fixing the gem. The observations reported for collet 3 can also be extended to the
other collets.
−
−
−
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Figure 7. The gem-glass in the plate RDD1. (A) RDD1 plate with the positions of the gem-glass
analyzed (Table 4); (B) BSE image of collet 3; (C) back-scattered electrons (BSE) image of the surface of
gem-glass 3.
The glass shows limited surface alterations. This is testified by the tiny flakes that detach from the
surface of the glass, indicating a beginning of degradation (Figure 7C). The presence of this thin layer
of alteration has not allowed to obtain compositional data completely adherent to the composition of
the intact glass, but they represent an average between the composition of the intact glass and the layer
of alteration. Therefore, the data obtained and reported in Table 4 are to be considered as indicative of
the composition of the glass.
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Table 4. Chemical composition (semi-quantitative analysis) of gem-glass in RDD1 plate.
Colourless 3
Yellow 2
Yellow 1
Na2 O
1.4
1.3
1.5
MgO
3.4
3.3
3.9
Al2 O3
0.8
0.6
0.6
SiO2
64.7
64.9
64.0
P2 O 5
0.7
0.9
1.2
PbO
17.7
18.6
19.2
Cl2 O
0.7
0.6
0.6
K2 O
6.1
6.1
5.8
CaO
3.2
2.9
2.5
MnO
0.2
0.1
0.0
FeO
0.6
0.4
0.2
CuO
0.6
0.4
0.4
The values shown in Table 4 represent the average of 5 measurements, carried out on the same
decorative element, on areas of 20 × 20 µm2 . The gem-glass is a silicates glass. The flux used seems to
be a mixed-alkali flux, containing both sodium (Na2 O) and potassium (K2 O), while the stabilizer has a
Ca-rich composition. The stabilizing component (CaO) as well as Na2 O are deficient compared to the
optimal formula for glass production, but the lack of these components is undoubtedly to be attributed
to surface leaching effects (Figure 7C). Magnesium (MgO) is present in percentages equal to 3–4 wt %.
This component can be related both to the composition of the flux, probably ash, and to the stabilizer
(use of mixed carbonates CaO/MgO).
The glass colorants are Fe (FeO in Table 4) and probably Cu (CuO in Table 4), even if the
measured values of Cu are at the limit of the sensitivity of the instrument. The presence of small
amounts of chlorine (Cl2 O) and phosphorus (P2 O5 ) can be justified by the presence of dust deposits.
The measurements also indicate important values for Pb (PbO).
The metal was analyzed in portable XRF and at SEM–EDS in order to obtain a mapping of the
chemical compositions of the alloys in relationship with the type of decoration and the moulding
technique. The main objects under investigation are located on the front of the Cross: the cherub, the
two angels, the Christ, the foils and collets, and the filigrees (Figure 8A,B); 46 analyses have been
collected. The measurements obtained express the average composition between the composition of
the surface gilding and that of the silver. Although we are aware that these data could be strongly
conditioned by the thickness of the gilding, which may not be constant on the different elements
analyzed, the representation of the ratio between the three main components of the metal alloys,
shown in the ternary diagram in Figure 8, indicates different ratios Au/Ag depending on the analyzed
decorative element. For each type, the compositions are quite homogeneous. The copper (Cu) content
rarely exceeds 10 wt %.
The embossed sheet, observed at SEM in secondary electrons (SE), shows on the surface the
presence of a thin homogeneous layer (see Figure 9), which is distinguished as weaving from the
underlying metal of the foil. This is an evidence of the presence of a gold leaf. The table in Figure 9
shows the measurements carried out on the individual grains of the alloy. The main metal is silver (Ag),
with the presence of gold (Au) in values between 3 and 5 wt %. Minor elements are tin (Sn), iron (Fe),
zinc (Zn) and copper (Cu). The presence of abundant mercury (Hg) indicates how the gold leaf was
installed on the foil. However, the observation at SEM is not diagnostic to identify the technique
followed for gilding because the leaf can be “amalgamated” or applied directly to the surface where the
mercury has been brushed (see [22] and Cucini, C. “Note di tecnologia sulla fabbricazione della filigrana
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veneziana del Duecento” in [7], pp. 185–203), cold or hot. Full-surface observations of the plate show
no signs of junction or overlapping of gold leaves (see Blumer, F. “Il restauro” in [7], pp. 237–271),
but it is also possible, for the gilding on silver, that the workpiece has been heated after polishing the
surface, in order to obtain a better adhesion of the leaf to the substrate (see [22] and Cucini, C. “Note di
tecnologia sulla fabbricazione della filigrana veneziana del Duecento” in [7], pp. 185–203).
Figure 8. XRF measurements. (A,B) indication of the objects analyzed on the front (A) and on the back
of Cross; (C) ternary diagram Ag—Au—Cu.
Figure 9. Textures and chemical composition of alloys of embossed sheet. (A) secondary electron
images of sheet; (B) energy-dispersive X-ray spectroscopy (EDS) spectrum of gold leaf. The table shows
the microchemical data and average alloy.
The angels placed in the central part of the Cross clearly show two very different aspects, both
in style and size (Figure 1A). This raised doubts about their relative ages, also in connection to the
realization of the Cross. The measurements were therefore directed to understand their composition
but also to verify their affinities and differences in texture. Figure 10A,B highlight the differences of the
two objects: The left angel (1), the smallest, shows a finer grain (each grain is about 20 µm) and the
shape of the grains seems rather irregular so as their arrangement (Figure 10A), while the right angel
(2) has grains whose dimensions are included between 30 and 40 µm (Figure 10B), better formed and
with more regular dispositions. The observation at higher magnifications (Figure 10C,D) also puts in
evidence that the smallest angel (right (2)) has a greater porosity, with micrometric pores, while the
larger angel (left (1)) has a diffuse submicrometric porosity. The composition of the metal alloy is very
similar for both objects (see the table in Figure 10). The composition of the right angel is different from
that of the left angel. The major components of the metal alloy are silver (Ag) and gold (Au), but their
ratio varies from 0.85 for the left angel to 3.7 for the right angel. There are minor elements such as tin
(Sn), antimony (Sb), iron (Fe) and zinc (Zn). The presence of mercury (Hg) is undoubtedly linked to
the existence, on the surface, of gilding.
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Figure 10. Textures and chemical composition of alloys of central angels statues. (A,C) secondary
electron images of left (1) angel; (B,D) secondary electron images of right (2) angel. The table shows the
average alloy composition of each angel.
4. Discussion
The Chiaravalle Cross is a processional cross that came from the abbey of Chiaravalle (close to
Milan, Italy). Several non-destructive (or micro-invasive) techniques were used, tailored to this case
study. Wood, stucco, gems, cameos, and metals were deeply investigated and many interesting
considerations can be derived.
Lacking any indication on the date of the production of this artefact, since no documentation
has been found until now, we obtained by radiocarbon dating a date in agreement with the current
attribution of this masterpiece to the late 13th century, since for the wooden part of the Cross we
derived an age not earlier than 1165–1265 AD. Concerning the modern date of the stucco behind a
jasper gem, this could be related to a different chronological placement but also to a later restoration
improving the adhesion of the gem setting. Yet, two previous restorations were recorded: the first
in 1539 when the Cross was found again after having been stolen in 1521, and the second in the 17th
century [7] (p. 240). In addition, F. Blumer reported a recent restoration too, finding a small paper
with the inscription “Agostino Figini orafo—Milano, restaurò anno 1950” (literally meaning “Agostino
Figini goldsmith—Milan, did restore in 1950 AD”, see the restoration report in [1] and Blumer, F.
“Il restauro” in [7], pp. 239, 262–263).
Regarding the characterization of the gems on the Chiaravalle Cross, it is possible to focus the
attention on several discussion points. First of all, on the basis of the statistical data reported in
Tables 1–3 it has been possible to observe differences in the number, quality, dimensions and color of
the gemstones between the front and rear of the Cross. The dominant red color is the first sensation
observing the front of the Cross, hand in hand with the preciousness of the gem materials.
Considering all the differences found between the front and the rear, it is possible to deduce a
deep planning ability beyond this magnificent opera. The gemstones come from several parts of the
world, as it was known during the 13th century. Due to that the gemstones set could be considered as
a symbol of the commercial links existing from Italy, Venice particularly, to the Asian regions. A proof
for these facts is the presence of the four trapiche sapphires, probably from Burma or Ceylon.
The four trapiche sapphires open an interesting window regarding where are they from and
how old they are. In the modern market the trapiche corundum, rubies and especially sapphires,
are very rare gemstones. Regarding the geographic origin, the first trapiche rubies arrived on the
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market from MongHsu mines, Myanmar (Burma), around 1995 and subsequently from the Vietnam
mines, as described by Schmetzer, et al. [23,24] and Garnier, et al. [25]. About sapphires, the discovery
of the trapiche variety is a recent fact, too and the rare ones found are typically from modern and
magmatic geographic origin, such as Madagascar, Australia, Montana mines [20]. Due to that and
to the limitations imposed by the mounting, using only the gemological applicable methods it is not
possible to give a unique answer to these questions, but crossing all the other knowledge obtained
on the Chiaravalle Cross during this work, several hypotheses could be formulated. On the basis of
the data obtained analyzing the metal and particularly the settings, it is possible to define them as
original and untouched; however, since we could not date the fabrication age of all the decorative
parts, we cannot be sure about the chronological arrangement of the four trapiche sapphires. However,
the cut and the inclusion pattern observed on them suggest that the trapiche sapphire tablets could
have been cut from the same, big, hexagonal “barrel”-shaped rough stone. Therefore, considering the
edge and all the gemological characteristics, the four trapiche sapphires could come from only two
geographic areas: Burma or Ceylon, actually known as Myanmar and Sri Lanka, respectively.
Regarding the cameos, on the basis of the gemological analyses, it is possible to identify three
type of materials: sardonyx, chalcedony and artificial glass, divided into two groups (see results).
Both groups are older than the creation of the Cross, and reused on it because felt as “ancient” and
then “precious”—a phenomenon well known since the Early Middle Ages3 —as demonstrated by the
fact that a cameo from group (a), lacking its upper half, has been nonetheless maintained on the Cross,
even if integrated with colophony, as stated after autoptical examination and experimental remake
by the conservator F. Blumer (see his report in [1]) and moved from the front to the rear side of the
precious artifact.
The natural untreated lapis-lazuli gemstone is a complex and variable mixture of minerals,
commonly constituted by lazurite and sodalite with minor amount of calcite, nosean, hauyna and
pyrite [28]. No bands corresponding to these typically associated mineral phases were observed in the
Raman analysis of FSQ1. Moreover, the chemical spectrum of FSQ1 presents barium and zirconium
traces not reported for natural lapis-lazuli chemicals [17]; a chemical composition as reported in
Figure 4b is compatible with a mixture used to create a gemstone imitation [29]. The presence of the
imitation of lapis on the Cross is not a surprise, because the use of lapis-lazuli simulants or dyed
are common and well known in the gemstones on the market, also from ancient ages [30]. Due to
that, the presence of lapis imitation is easily explicable thanks to the observations made on the metal
setting during the restauration process; indeed, Blumer [7] indicates a settings alteration corresponding
to FSQ1 and FDQ1 gemstones. The presence of this modern lapis could be compatible with the
restoration in 1950 documented by Blumer (see the restoration report in [1] and Blumer, F. “Il restauro”
in [7], pp. 239, 262–263).
The red jasper on which the crucifix has been fixed was macroscopically identified as likely coming
from Giuliana, province of Palermo, Sicily (see [7], pp. 207–209). This source of beautiful green, yellow
and red jaspers was known since the Hellenistic period and much exploited in Roman and Baroque
times when it was exported throughout the Italian peninsula [31]. This information, together with the
connection to the atelier working at the Norman court of the Hautevilles in Palermo (for some cameos
provenance) opens new scenarios for the Cross production, linking the acknowledged golden filigree
fabrication in Venice to some peculiar materials provenance from Sicily.
The analytical data collected on the transparent glass-gems, although only indicative of their
chemical composition, indicate the main components of the glass recipe: SiO2 as a vitrified, mixed-alkali
as a flux, CaO as a stabilizer. The yellow color of two of the three gems is due to the presence of FeO;
the colorless glass-gem has been obtained by adding manganese to the vitrifiable mixture [32].
3
For a large variety of objects (liturgical and not) reusing ancient cameos and intaglios see [26] For examples of glyptic reuse
still in the Late Middle Ages, see [27].
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We cannot forget that each ancient artefact is the testimony of a series of gestures and actions (chaine
operatoire), whose sequence often comes to us incomplete and devoid of operational details sometimes
fundamental to the success of the object. The ancient artefact also comes to us with the overprint of
its entire “life path”, including the use, ordinary maintenance and extraordinary maintenance [33].
The presence of lead (Table 4) found in the glass could be also attributed to the polishing phases of the
fake gemstone, as reported in technical cookbooks [34,35] certainly known in the early Middle Ages
and, therefore, may not be a component of the glass recipe.
Finally, concerning metal objects we observed, they are made of an alloy of silver, containing
copper and gold as minor elements. The proportions between these elements seem to show a correlation
with the technique of realization of the single decorative elements (Figure 8). A striking result followed
the observations and measurements on the two central angels’ statues, confirming the hypothesis
that the realization of the two artefacts could have taken place in different times and probably in
different workshops.
Other metallic processional crosses were characterized in the literature [36,37], but this is the first
really multidisciplinary study, addressing different materials and fabrication techniques, published as
a journal paper. The study of a complex masterpiece like the Chiaravalle Cross has taken advantage
from the exchange of knowledge and skills in the field of gemology, gliptic, restoration, art history,
physics, and archaeometallurgy.
Author Contributions: Conceptualization, D.D., G.B., M.P.R., E.P.C., F.B. and G.G.; historic analysis, C.B., and
L.C.; Raman and XRF investigations, R.A., T.F., and M.G.; gemological, cameos and jasper investigations, M.M.,
F.D., L.G., E.G., and L.L.; nuclear investigations, D.D., E.P.C., and R.C.; SEM investigations, S.B., C.C., and M.P.R.;
writing—original draft preparation, D.D., M.M., E.G., and M.P.R.; writing—review and editing, D.D. with the help
of all the coauthors.
Funding: This research received no external funding.
Acknowledgments: We thank Emanuela Daffra for her effort in the administrative issues for the loan of the
samples and for very valuable discussions.
Conflicts of Interest: The authors declare no conflict of interest.
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© 2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access
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