ArticlePDF Available

Characterization and Source of Sedimentary Rocks of the Alexandria Lighthouse Archaeological Objects, Egypt

Authors:

Abstract

The present study was aimed to present a detailed study concerning the nature and characterization of stones constituting some of the Alexandria Lighthouse monumental objects that are made of sedimentary rocks, as well as indicating their corresponding ancient quarries. A field inspection of the objects that were salvaged from the seabed and are presently displayed or stored at different locations in Alexandria city is conducted and a series of samples from objects that are still underwater are collected and studied. Petrographic studies, XRD, XRF/ ICP-AES and δ13C and δ180 isotopes analyses were carried to characterize the different rock types in terms of their petrographic types of stone and chemical properties. The studies revealed that these archaeological objects (stone blocks, columns, part of columns, statues and obelisks) are constructed from different igneous, metamorphic and sedimentary rocks. The archeological objects made of sedimentary rocks are formed of quartzitic sandstones (orthoquartzite), greywacke (siltstone and sandstone) and limestone (lime-mudstone and sandy dolomite/dolomite sandstone). The source area of each type of stone constituting the archaeological samples is performed, including delimitation of the corresponding ancient quarries when possible. Wadi Hammamat and Gebel Ahmar quarries were the provenance areas of the greywacke and quartzitic sandstones used in the Alexandria Lighthouse objects, respectively. Moreover, results and the data derived expand the knowledge concerning Egyptian monumental stones and provide inspiration for future investigations and studies.
(
a)
215 µ
(
b)
215 µ
215 µ
(
a)
140 µ
(
b)
140 µ
215 µ
(
a)
(
b)
140 µ
140 µ
(
c)
(
d)
140 µ
(
a)
215 µ
(
b)
215 µ
(
a)
215 µ
(
b)
215 µ
... The Egyptians translated these warnings into structures to guide ships (Adams 1870;Steveson 2013). The first lighthouse is the Alexandria Lighthouse on Faros Island in Alexandria, built by the Egyptians between 290 and 270 BC (Akarish and Dessandier 2011;Stevenson 2013). Previously, the lighthouses, which marked the port entrances, increased in number with the increase in world maritime trade. ...
Conference Paper
Full-text available
In the early days, people lit fires at the seaside or on the hills near the coast, sending warnings about rocks and navigational safety to ships approaching land. Lighthouses, one of the most important navigational aids of ships, is the main theme of this study. The aim of this study is to emphasize the importance of lighthouses in terms of both Black Sea history and to touch on the past of the Black Sea lighthouses, which are the silent and unknown witnesses of history. The fact that lighthouses continue to be one of the most important navigation aids even today, where technology has made great progress, proves the importance of these structures. For this reason, lighthouses are silently fulfilling their duties right next to us today as structures that need to be protected, illuminating not only the seas but also the field of maritime science and urban history.
... The 2nd type of stone (Sandy dolostone) used in the fortress foundation is ne grains of quartz cemented by dolomitic cement. According to [52], it is characterized by the yellowish to brownish colors and the presence of (30-70% Ca content) and (60-70 to 20-30% Qz content measured 60-120 µm). By comparing the different analytical data, the lithological features presented by [53] could be a rmed that this type's provenance does not belong to various limestone quarries (Mokattam, Minia, or Drunka, etc.). ...
Preprint
Full-text available
This paper investigates the seismic actions that affect Qait Bey Fortress in Alexandria- Egypt. It presents the results of scientific studies and examinations to evaluate the deterioration conditions, which affected archaeological buildings in the marine environment . In Alexandria, many monumental sites and stone buildings have suffered from many aggressive factors of deterioration (mechanical, chemical, and biological), which have caused great harmful appearances and threatened to eradicate them. These effects include the chemical actions resulting from seawater and marine aerosol and mechanical actions of water waves. ( Qait Bey Fortress ), as a case study, was periodically investigated by many scientific techniques through 5 years to check their decay conditions and to define the most suitable conservation approaches and non-destructive methods for preservation. Different techniques and examinations were performed to evaluate the current deterioration state of the fortress. For example, XRD analysis and PM investigation were used to study the mineralogical compositions, lithotype, and petrographic characteristics of the stone samples. SEM was used to investigate the morphological features of the same samples. AAS was also used for studying the chemical constitutes of seawater samples. In addition, microbiological investigations were conducted to evaluate the colored hard crusts that affected the stone surfaces in the fortress. Our results proved that severe deterioration factors highly influenced the fortress by collaborating with chemical, mechanical and biological mechanisms. These mechanisms caused several manifestations, such as abrasion and attrition, crystallizing of salt species, mortar desegregation, pitting and minerals’ honeycomb (Alveolar), color changes, in addition to the accumulation of black and colored biogenic hard crusts.
... The limestone of these quarries is light-coloured, and their deposits belong to the Pleistocene Alexandria Formation. Ancient and recent quarries are observed on the Alexandria-Marsa Matrouh Road in a 21 km area [51,52]. ...
Article
Full-text available
The only example and reference of Ptolemaic Alexandrian tombs, with clear integrations of Egyptian-style scenes and decorations, is considered an endangered archaeological site due to different coastal environmental risks in Alexandria and the absence of maintenance. Anfushi's Ne-cropolis is located near the western harbour (Island of Pharos) and dates back to the 2nd century BC. Sea level rises, earthquakes, flooding, storminess, variations in temperature, rainfall, and wind are the factors that have the largest effect on the destruction and decay of Anfushi's Necropolis building materials. This paper's main objectives were to characterize this necropolis's building materials and assess its durability problems and risks regarding the coastal environment. Additionally, the vector mapping of its architectural and structural elements was applied for documentation and recording purposes for the necropolis. To achieve these aims, field (recording and photographs), desk (engineering drawing and mapping), and laboratory works (X-ray diffraction, X-ray fluores-cence, binocular microscopy, polarizing microscopy, and scanning electron microscopy) were carried out. The results confirmed the probabilistic risk of sea level rises and its impact on the sub-mergence of Anfushi's Necropolis. The structural deficiencies of the tombs were caused by the effect of earthquake tremors along with anthropogenic factors. In addition, chemical and microscopic investigations showed that salt weathering (halite and gypsum) induced the decay of the building materials.
... Statistical counting of components and evaluation of grain roundness are commonly applied in the field of sedimentary petrography [23] to undertake sedimentary provenance studies (identification of sediment sources and transport distances) but this represents a provenance marker for the sedimentary rock itself only in very particular cases. A much more effective provenance marker for a clastic rock would be a particular feature of the cement formed during the lithification process such as authigenic overgrowths [24]. ...
Article
Full-text available
The present study deals with a particular clastic rock from the Montjuïc hill exploited since Roman times in Barcino (present-day Barcelona (NE Spain)). Polarized and cathodoluminescence microscopies have been used to describe the main petrographic features of Montjuïc sandstones. Several characteristic provenance markers have been identified; among them the most specifically restricted to Montjuïc sandstone are the K-feldspar clasts with authigenic overgrowths. A petrographic survey oriented to the detection of such markers has been fruitfully applied to sculptures, architectural elements, mosaics, and pottery. The petrographic approach has demonstrated that some Roman heritage materials had been erroneously assigned to Montjuïc sandstone and the revision of all the pieces macroscopically assigned to this provenance is advised. The use of Montjuïc sandstone in Roman tesserae has been reported for the first time with interesting implications on previously unreported evidence of Roman extraction at the bottom part of the Montjuïc cliff. Finally, Montjuïc crushed sandstone used as pottery temper has been also reported in the productions of a medieval (12th-13th century) workshop in Barcelona. This encourages the study of the distribution of pottery with this particular temper.
... The intensity of degradation can infer its maturity, distance travelled from provenance. These and other such chemical processes are preserved and ultimately transferred to sedimentary records which gives a tenable signature for evaluating the original composition maturity and following weathering conditions (Akarish and Dessandier, 2011). ...
Article
Full-text available
Attempts have been made to classify the sediment on their degree of maturity. Compositional maturity is a reflection of intensity of weathering and a function of labile grains, unstable/stable rock fragments and stable quartz arenites. The main aim of this study is to investigate maturity and area of deposition and attempt to shed light on source area paleo-weathering conditions. Twenty one samples of shales and sandstones units were collected from a depth precisely between 1160 to 11,480m at a well in western Niger Delta, grinded, pulverized and sieved with less than 75μm. About 10g was packed and sent to Acme analytical Laboratory LTD., Vancouver, Canada. From the results, various plots and indexes inferring maturity and area of deposition were utilized. Using the A-K-F ternary plots of Englund and Jørgensen (1973), the depositional environment is transition zone. The silicate weathering indexes CIA, CIW and PIA values ranges from 45-65, on average indicates low to moderate weathering in the source area with extreme weathering of some sand fraction. Various calculated values of the weathering indices: Chemical Index of Alteration (CIA), Plagioclase Index of Alteration (PIA), Chemical Index of Weathering (CIW) and scatter plots of formulated ratios of Al/Na, K/Na, and Rb/K vs chemical index of alteration (CIA) were plotted. The moderate values below average suggest low to moderate weathering conditions in the source area or during transportation. This also inferred their recycling processes are insignificant. The clay content is low and feldspars are averagely high implying immaturity. The calculated ZTR index for the sand ranges from 36.4-75.0 from with an average mode of 55.5% implying almost all contain mineralogically immature sediments. The calculated Zircon- Tourmaline-Rutile (ZTR) index shows that majority of the sample depths have >43% ZTR index but below 75% which corresponds to generally immature sediments.
... In the case of building materials used in antiquity, a large body of stable isotope data has been compiled for historic quarry sites and the geochemistry of the quarried rock (Attanasio et al., 2006;Brilli et al., 2010;Galan et al., 1999;Gorgoni et al., 2002;Herz and Dean, 1986;Lapuente et al., 2000). These baseline data provide the foundation for comparison between an historical structure and potential source quarries or regions (Akarish and Dessandier, 2011;Antonelli et al., 2003;Attanasio et al., 2008;Brilli et al., 2011;De Vito et al., 2004;Pinter et al., 2004). In addition to structural materials, the comparison of stable isotope measurements and databases has also been used to understand the region of origin of jewelry (Hull et al., 2008) and glass artifacts (Henderson et al., 2005;Silverstri et al., 2010), which is discussed in more detail in Chapter 14.14. ...
Article
Stable isotope analysis has a lengthy application history in the fields of biology, ecology, and geology but its application in forensic investigations is relatively new. A recent report by the National Research Council on the strength of the forensic sciences in the United States highlighted areas of weakness, including the lack of a tested scientific foundation for many of the analytical techniques used in examinations. Stable isotope analysis has a strong scientific foundation developed in the academic community and could thus play a major role in the forensic community as a powerful tool in the investigator's toolbox.This chapter presents a framework for applying the stable isotope analysis techniques commonly employed by isotope geochemists in forensics settings. The utility of this framework lies in its ability to address a range of questions from relatively simple sample comparisons to more complex region or origin predictions. The forensic application of stable isotope analysis within this framework is discussed at both a nonspatial and spatial scale, examples of applications include the analysis of nonorganic and organic materials. The chapter concludes with a discussion detailing how the stable isotope analysis techniques developed in scientific settings can be extremely useful in legal settings as well.
Conference Paper
Full-text available
ZET İlk zamanlarda insanlar deniz kenarlarında veya sahillere yakın tepelerde ateşler yakarak karaya yaklaşan gemilere kayalıklar ve seyir emniyeti ile ilgili uyarılar göndermiştir. Gemilerin en önemli seyir yardımcılarından biri olan deniz fenerleri bu çalışmanın ana temasıdır. Kıyılarda sessizce gemilerin emniyetli seyretmelerine yardımcı olan deniz fenerleri üzerine çok az araştırma yapılmış, denizcilik açısından bakıldığında önemli bir yere sahip olan Gazimağusa Kuzeybatı Karakol Deniz Feneri ile ilgili ise hiç çalışma yapılmamıştır. Bu çalışmanın amacı hem Kıbrıs tarihi açısından fenerlerin önemini vurgulamak ve tarihin sessiz ve çok bilinmeyen tanığı olan Gazimağusa Kuzeybatı Karakol Deniz Feneri'nin geçmişine değinmektir. Teknolojinin büyük bir ilerleme gösterdiği bugün bile deniz fenerlerinin en önemli seyir yardımcılarından biri olma özelliğini sürdürüyor olması bu yapıların önemlerini kanıtlamaktadır. Bu nedenle fenerler sadece denizleri değil, aynı zamanda denizcilik bilimi ve kent tarihi alanını da aydınlatan, korunması gereken yapılar olarak sessizce görevlerini yerine getirmektedir. Çalışmamız aynı zamanda bu yapılar üzerindeki farkındalığı da artırmaya adaydır.
Article
Full-text available
Thermal treatments constitute the core in the success for most structural treatments, such as consolidation, treating planar deformations, reinforcing degraded support and others. Among the wide range of devices for thermal treatments of paintings proposed in scientific and technical literature, flexible heaters appear to be the most promising technology, especially for working with large painting or in situ. The present study provides a comprehensive review of flexible mild heater systems devised for structural conservation of paintings in the last decades, bringing forward the issues related to the instrumentation used for thermal treatments, stressing the importance of accurate control and the inadequateness of available devices. By highlighting the actual limitations of existing devices, a different approach, which employs Carbon Nanotubes-based flexible heaters is then proposed in its conceptual form. The design of such device, called IMAT (Intelligent Mobile Accurate Thermo-electrical device) is supported by the European Community in the context of the EC-FP7 Environment Theme (ENV-NMP.2011.2.2-5) into a three-year project started on November 2011. © 2012 Asian Network for Scientific Information.
Article
Full-text available
Ancient Egyptian limestone quarries in the Nile Valley occur in six geological formations of Palaeogene age. Samples were collected from 23 of the 48 known quarries, and analysed by thin-section petrography and X-ray fluorescence spectrometry. Results of the analyses show that the geological formations can be identified from rock texture and allochem types, and a plot of SiO2/Al2O3 versus CaO/[CaO + MgO]. The application of these petrographic and geochemical parameters make it possible to determine the geographic provenance of limestone used in ancient Egyptian sculptures and monuments.
Article
Ooids are a major constituent of the Pleistocene carbonates along the northwestern coastal zone of Egypt. The Mersa Matruh area was selected for a detailed diagenetic study of these rocks. δ18O, δ13C and Sr values were determined on whole-rock samples on manually separated ooids and calcite cements. Plerographic examination shows that these rocks are partly consolidated ooid grainstones with low-Mg calcite cement in granular voids.Oxygen isotopic and Sr values for the whole rock (+ 0.5% vs. PDB and 9300 ppm, respectively) are consistent with data on limestones of the same age. In contrast, oxygen isotopic values for ooids (ave. +0.5% vs. PDB) are heavier relative to values for low-Mg calcite cements (ave. −1.4% vs. PDB), and Sr contents are higher for ooids (10,000 ppm). In addition, δ13C-values are identical for the whole rock and ooids (ave. +4.5% vs. PDB), and heavier relative to δ13C-values of the calcite cements (ranging from +1.4 to +3.8% vs. PDB). These data may suggest that calcite cements are formed in non-diluted pore water under relatively high rock/water ratios.
Article
Greywackes and siltstones from the Neoproterozoic Hammamat Group in the Wadi Hammamat and Wadi Bali areas, Eastern Desert of Egypt, were analyzed for major and trace elements. The sedimentary rocks are characterized by , a wide range of both and plus a chemical index of alteration between 60 and 44. These data suggest that the Hammamat sedimentary rocks are chemically immature and that there was minimal chemical weathering involved in their erosion and deposition. The sedimentary units show two broad compositional groupings in the two studied areas. The Wadi Bali sedimentary rocks are characterized by low MgO, Cr, Ni, V, Ba, Nb, Y and Zr and high Na2O, CaO, and Sr relative to the Wadi Hammamat sedimentary rocks. These geochemical differences suggest contrasting provenance for the sedimentary rocks in the two areas. The Wadi Hammamat sedimentary rocks were derived from 30% mafic rocks, 25% granodiorite, 25% intermediate volcanics and 20% felsic volcanics, whereas those of the Wadi Bali area were derived from a relatively homogeneous source of 90% intermediate volcanics and 10% felsic volcanics. The Wadi Hammamat sedimentary rocks were deposited in an intra-arc basin that developed as a result of the creation of considerable topographic and structural relief after development of a continental arc. The source rocks were continental arc volcanics (Dokhan Volcanics) and the uplifted older oceanic tholeiites and island arc assemblages. The Wadi Bali sedimentary rocks were formed by the same scenario as the Wadi Hammamat sedimentary rocks, but the absence of rock fragments older than the Dokhan Volcanics indicates a closed intra-arc basin where the Dokhan Volcanics were the main source of clasts.
The pharos of Alexandria, A concentration of geometry
  • Hairy I.